# muaggatt

muname:
Tecolote stony loam, 20 to 70 percent slopes


muname:
Tecolote stony loam, thick surface variant, 20 to 70 percent slopes


muname:
Tesajo gravelly sandy loam, 2 to 15 percent slopes


muname:
Trail loamy fine sand, 5 to 10 percent slopes


muname:
Turkeysprings stony loam, 20 to 50 percent slopes


muname:
Washoe cobbly loam, 9 to 25 percent slopes


muname:
Washoe gravelly loam, 1 to 9 percent slopes


muname:
Wilcoxson clay loam, 2 to 10 percent slopes


muname:
Wilcoxson loam, thick surface, 1 to 6 percent slopes


muname:
Wilcoxson stony loam, 5 to 20 percent slopes


muname:
Wilcoxson stony loam, 20 to 50 percent north slopes


muname:
Wilcoxson stony loam, 15 to 45 percent south slopes


muname:
Chenango gravelly silt loam, 3 to 8 percent slopes


muname:
Chenango gravelly silt loam, 8 to 15 percent slopes


muname:
Collamer silt loam, 3 to 8 percent slopes


muname:
Collamer silt loam, 8 to 15 percent slopes


muname:
Collamer silt loam, 15 to 25 percent slopes


muname:
Erie gravelly silt loam, 0 to 3 percent slopes


muname:
Erie gravelly silt loam, 3 to 8 percent slopes


muname:
Erie extremely stony soils, gently sloping


muname:
Hoosic gravelly sandy loam, 0 to 3 percent slopes


muname:
Hoosic gravelly sandy loam, 3 to 8 percent slopes


muname:
Hoosic gravelly sandy loam, 8 to 15 percent slopes


muname:
Hoosic gravelly sandy loam, 15 to 25 percent slopes


muname:
Lordstown channery silt loam, 3 to 8 percent slopes


muname:
Lordstown channery silt loam, 8 to 15 percent slopes


muname:
Mardin gravelly silt loam, 3 to 8 percent slopes


muname:
Mardin gravelly silt loam, 8 to 15 percent slopes


muname:
Mardin gravelly silt loam, 15 to 25 percent slopes


muname:
Nassau channery silt loam, 15 to 25 percent slopes


muname:
Oakville loamy fine sand, 0 to 3 percent slopes


muname:
Oakville loamy fine sand, 3 to 8 percent slopes


muname:
Otisville gravelly sandy loam, 0 to 8 percent slopes


muname:
Otisville gravelly sandy loam, 8 to 15 percent slopes


muname:
Otisville gravelly sandy loam, 15 to 25 percent slopes


muname:
Pittsfield gravelly loam, 3 to 8 percent slopes


muname:
Pittsfield gravelly loam, 8 to 15 percent slopes


muname:
Pittsfield gravelly loam, 15 to 25 percent slopes


muname:
Rhinebeck silt loam, 0 to 3 percent slopes


muname:
Rhinebeck silt loam, 3 to 8 percent slopes


muname:
Riverhead sandy loam, 0 to 3 percent slopes


muname:
Riverhead sandy loam, 3 to 8 percent slopes


muname:
Riverhead sandy loam, 8 to 15 percent slopes


muname:
Riverhead sandy loam, 15 to 25 percent slopes


muname:
Rock outcrop-Arnot complex, moderately steep


muname:
Rock outcrop-Hollis complex, moderately steep


muname:
Swartswood gravelly loam, 3 to 8 percent slopes


muname:
Swartswood gravelly loam, 8 to 15 percent slopes


muname:
Swartswood gravelly loam, 15 to 25 percent slopes


muname:
Swartswood and Mardin very stony soils, sloping


muname:
Swartswood and Mardin very stony soils, moderately stee p


muname:
Wurtsboro gravelly loam, 8 to 15 percent slopes


muname:
Bath-Nassau channery silt loams, 3 to 8 percent slopes


muname:
Bath-Nassau channery silt loams, 8 to 15 percent slopes


muname:
Castile gravelly silt loam, 0 to 3 percent slopes


muname:
Castile gravelly silt loam, 3 to 8 percent slopes


muname:
Charlton fine sandy loam, 3 to 8 percent slopes


muname:
Charlton fine sandy loam, 8 to 15 percent slopes


muname:
Charlton-Paxton complex, extremely stony, sloping


muname:
Charlton-Paxton complex, extremely stony, moderately st eep


muname:
Chenango gravelly silt loam, 0 to 3 percent slopes


muname:
Swartswood and Mardin very stony soils, very steep


muname:
Unadilla silt loam, 0 to 8 percent slopes


muname:
Unadilla silt loam, 8 to 15 percent slopes


muname:
Wurtsboro gravelly loam, 3 to 8 percent slopes


muname:
Alton gravelly sandy loam, 3 to 8 percent slopes


muname:
Appleton silt loam, 0 to 3 percent slopes


muname:
Appleton silt loam, 3 to 8 percent slopes


muname:
Arkport very fine sandy loam, 0 to 6 percent slopes


muname:
Arkport very fine sandy loam, 6 to 12 percent slopes


muname:
Arkport-Collamer complex, 6 to 20 percent slopes


muname:
Bombay fine sandy loam, 0 to 3 percent slopes


muname:
Bombay fine sandy loam, 3 to 8 percent slopes


muname:
Brockport silty clay loam, 0 to 2 percent slopes


muname:
Brockport silty clay loam, 2 to 6 percent slopes


muname:
Brockport silty clay loam, 6 to 12 percent slopes


muname:
Cazenovia silt loam, 0 to 3 percent slopes


muname:
Cazenovia silt loam, 3 to 8 percent slopes


muname:
Cazenovia gravelly silt loam, shale substratum, 0 to 3 percent slopes


muname:
Cazenovia gravelly silt loam, shale substratum, 3 to 8 percent slopes


muname:
Churchville silt loam, 0 to 2 percent slopes


muname:
Churchville silt loam, 2 to 6 percent slopes


muname:
Claverack loamy fine sand, 0 to 6 percent slopes


muname:
Collamer silt loam, 0 to 2 percent slopes


muname:
Collamer silt loam, 2 to 6 percent slopes


muname:
Collamer silt loam, 6 to 12 percent slopes, severely eroded


muname:
Colonie loamy fine sand, 0 to 6 percent slopes


muname:
Colonie loamy fine sand, 6 to 12 percent slopes


muname:
Elnora loamy fine sand, 0 to 6 percent slopes


muname:
Farmington silt loam, 0 to 8 percent slopes


muname:
Farmington silt loam, 8 to 15 percent slopes


muname:
Galen very fine sandy loam, 0 to 2 percent slopes


muname:
Galen very fine sandy loam, 2 to 6 percent slopes


muname:
Hilton loam, rock substratum, 0 to 3 percent slopes


muname:
Hilton loam, rock substratum, 3 to 8 percent slopes


muname:
Hilton-Cazenovia stony silt loams, 0 to 8 percent slopes


muname:
Howard gravelly loam, 3 to 8 percent slopes


muname:
Kendaia and Appleton silt loams, rock substratum, 0 to 3 percent slopes


muname:
Lairdsville silt loam, 0 to 6 percent slopes


muname:
Madrid fine sandy loam, 3 to 8 percent slopes


muname:
Madrid fine sandy loam, 8 to 15 percent slopes


muname:
Niagara silt loam, 0 to 2 percent slopes


muname:
Niagara silt loam, 2 to 6 percent slopes


muname:
Ontario stony loam, 3 to 8 percent slopes


muname:
Ontario very stony loam, 3 to 15 percent slopes


muname:
Ontario loam, rock substratum, 0 to 8 percent slopes slopes


muname:
Ovid silt loam, shale substratum, 0 to 4 percent slopes


muname:
Rhinebeck silt loam, 0 to 2 percent slopes


muname:
Rhinebeck silt loam, 2 to 6 percent slopes


muname:
Schoharie silt loam, 2 to 6 percent slopes


muname:
Wampsville gravelly loam, 3 to 8 percent slopes


muname:
Wassaic silt loam, 0 to 3 percent slopes


muname:
Wassaic silt loam, 3 to 8 percent slopes


muname:
Bridgehampton silt loam, 0 to 2 percent slopes


muname:
Bridgehampton silt loam, 2 to 6 percent slopes


muname:
Bridgehampton silt loam, till substratum, 2 to 6 percent slopes


muname:
Bridgehampton silt loam, till substratum, 6 to 12 percent slopes


muname:
Carver and Plymouth sands, 0 to 3 percent slopes


muname:
Carver and Plymouth sands, 3 to 15 percent slopes


muname:
Carver and Plymouth sands, 15 to 35 percent slopes


muname:
Montauk fine sandy loam, 0 to 3 percent slopes


muname:
Montauk fine sandy loam, 3 to 8 percent slopes


muname:
Montauk fine sandy loam, 8 to 15 percent slopes


muname:
Montauk silt loam, 0 to 3 percent slopes


muname:
Montauk silt loam, 3 to 8 percent slopes


muname:
Montauk silt loam, 8 to 15 percent slopes


muname:
Montauk soils, graded, 0 to 8 percent slopes


muname:
Montauk soils, graded, 8 to 15 percent slopes


muname:
Montauk loamy sand, sandy variant, 0 to 3 percent slopes


muname:
Montauk loamy sand, sandy variant, 3 to 8 percent slopes


muname:
Montauk loamy sand, sandy variant, 8 to 15 percent slopes


muname:
Montauk loamy sand, sandy variant, 15 to 35 percent slopes


muname:
Plymouth loamy sand, 0 to 3 percent slopes


muname:
Plymouth loamy sand, 3 to 8 percent slopes


muname:
Plymouth loamy sand, 8 to 15 percent slopes


muname:
Plymouth gravelly loamy sand, 3 to 8 percent slopes, eroded


muname:
Plymouth gravelly loamy sand, 8 to 15 percent slopes, eroded


muname:
Plymouth loamy sand, silty substratum, 0 to 3 percent slopes


muname:
Plymouth loamy sand, silty substratum, 3 to 8 percent slopes


muname:
Riverhead very stony sandy loam, 3 to 8 percent slopes


muname:
Riverhead very stony sandy loam, 8 to 15 percent slopes


muname:
Riverhead and Haven soils, graded, 0 to 8 percent slopes


muname:
Riverhead and Haven soils, graded, 8 to 15 percent slopes


muname:
Riverhead and Plymouth very bouldery soils, 15 to 35 percent slopes


muname:
Scio silt loam, till substratum, 2 to 6 percent slopes


muname:
Scio silt loam, sandy substratum, 0 to 2 percent slopes


muname:
Scio silt loam, sandy substratum, 2 to 6 percent slopes


muname:
Patent-Gullied land-Glendive complex, 1 to 9 percent slopes


muname:
Boxwell-Cabbart-Arikara complex, 9 to 50 percent slopes


muname:
Kirby-Arikara-Badland, outcrop complex, 15 to 70 percent slopes


muname:
Tinsley-Chanta complex, 6 to 35 percent slopes


muname:
Wolf Point silty clay loam, 0 to 1 percent slopes


muname:
Badland, outcrop-Cabbart complex, 6 to 70 percent slopes


muname:
Cabba-Sen-Chama silt loams, 15 to 70 percent slopes


muname:
Arikara-Shambo-Cabba loams, 9 to 70 percent slopes


muname:
Glendive fine sandy loam, 0 to 3 percent slopes, rarely flooded


muname:
Havre silt loam, 0 to 3 percent slopes, rarely flooded


muname:
Kremlin-Ethridge-Gerda complex, 1 to 6 percent slopes


muname:
Lambert-Slickspots-Rhoades complex, 1 to 9 percent slopes


muname:
Scairt-Maltese-Boxwell complex, 3 to 25 percent slopes


muname:
Cedarpan-Slickspots, stony-Farfeld complex, 3 to 35 percent slopes


muname:
Heil silt loam, low precipitation, 0 to 1 percent slopes


muname:
Harriet silt loam, low precipitation, 0 to 3 percent slopes


muname:
Pits, gravel and sand, low precipitation


muname:
Straw-Daglum complex, channeled, 0 to 2 percent slopes


muname:
Boxwell-Kremlin loams, 1 to 6 percent slopes


muname:
Boxwell-Kremlin loams, 6 to 15 percent slopes


muname:
Badland, outcrop-Arikara-Cabbart complex, 15 to 70 percent slopes


muname:
Harriet silt loam, 0 to 2 percent slopes


muname:
Rhame-Kremlin-Maltese complex, 1 to 15 percent slopes


muname:
Boxwell-Scairt-Maltese complex, 6 to 15 percent slopes


muname:
Rhame-Arikara-Fleak complex, 9 to 50 percent slopes


muname:
Patent-Gerda-Slickspots complex, 1 to 9 percent slopes


muname:
Lonna-Arikara-Cabbart complex, 9 to 70 percent slopes


muname:
Wolf Point silty clay loam, wooded, 0 to 1 percent slopes


muname:
Havre silt loam, wooded, 0 to 1 percent slopes


muname:
Haplustolls-Ustorthents complex, 0 to 6 percent slopes


muname:
Cozberg-Chanta loams, 1 to 6 percent slopes


muname:
Kremlin-Shibah loams, 9 to 50 percent slopes, very bouldery


muname:
Kremlin-Chanta loams, 1 to 6 percent slopes


muname:
Shibah-Rubbleland-Arikara complex, 15 to 70 percent slopes


muname:
Glendive fine sandy loam, wooded, 0 to 3 percent slopes


muname:
Hanly fine sandy loam, wooded, 0 to 6 percent slopes


muname:
Maltese-Lonna-Arikara complex, 3 to 50 percent slopes


muname:
Bulltop-Shibah loams, 1 to 9 percent slopes


muname:
Rhoades-Daglum complex, 0 to 6 percent slopes


muname:
Dogtooth-Janesburg silt loams, 0 to 6 percent slopes


muname:
Dogtooth-Janesburg complex, 6 to 15 percent slopes


muname:
Amor-Brandenburg complex, 3 to 25 percent slopes


muname:
Daglum-Rhoades complex, 0 to 6 percent slopes


muname:
Amor-Arnegard loams, 0 to 3 percent slopes


muname:
Amor-Shambo loams, 3 to 6 percent slopes


muname:
Amor-Cabba loams, 9 to 15 percent slopes


muname:
Manning-Schaller-Wabek complex, 6 to 25 percent slopes


muname:
Sen-Golva silt loams, 0 to 3 percent slopes


muname:
Chama-Sen-Cabba silt loams, 3 to 6 percent slopes


muname:
Chama-Cabba-Sen silt loams, 6 to 9 percent slopes


muname:
Cabba-Chama-Sen silt loams, 9 to 15 percent slopes


muname:
Parshall fine sandy loam, 0 to 6 percent slopes


muname:
Regent-Savage silty clay loams, 3 to 6 percent slopes


muname:
Janesburg fine sandy loam, 0 to 6 percent slopes


muname:
Lefor fine sandy loam, 0 to 6 percent slopes


muname:
Badland, outcrop-Lambert-Cabba complex, 6 to 50 percent slopes


muname:
Flasher-Rock outcrop-Vebar complex, 9 to 70 percent slopes


muname:
Vebar-Amor complex, 6 to 35 percent slopes, extremely stony


muname:
Sen-Janesburg silt loams, 0 to 6 percent slopes


muname:
Sen-Janesburg silt loams, 6 to 9 percent slopes


muname:
Flasher-Vebar-Parshall complex, 9 to 35 percent slopes


muname:
Ekalaka-Parshall-Desart fine sandy loams, 0 to 6 percent slopes


muname:
Farfeld-Cedarpan loams, 0 to 6 percent slopes


muname:
Wayden-Moreau silty clays, 3 to 9 percent slopes


muname:
Searing-Ringling loams, 0 to 6 percent slopes


muname:
Belfield-Grail silty clay loams, 0 to 2 percent slopes


muname:
Manning fine sandy loam, 0 to 6 percent slopes


muname:
Lihen-Parshall complex, 0 to 6 percent slopes


muname:
Savage silty clay loam, 0 to 2 percent slopes


muname:
Janesburg-Dogtooth silt loams, 0 to 6 percent slopes


muname:
Savage-Daglum silt loams, 0 to 6 percent slopes


muname:
Straw loam, channeled, 0 to 2 percent slopes


muname:
Straw-Rhoades-Daglum silt loams, 0 to 2 percent slopes


muname:
Savage silty clay loam, 2 to 6 percent slopes


muname:
Dogtooth-Janesburg-Brandenburg complex, 9 to 35 percent slopes


muname:
Dogtooth-Janesburg-Cabba complex, 6 to 30 percent slopes


muname:
Banks-Trembles fine sandy loams, channeled, 0 to 2 percent slopes


muname:
Evridge-Desart-Telfer fine sandy loams, 0 to 6 percent slopes


muname:
Cabbart-Badland, outcrop complex, 6 to 70 percent slopes


muname:
Patent-Badland, outcrop-Cabbart complex, 6 to 50 percent slopes


muname:
Maltese-Gerda complex, 0 to 6 percent slopes


muname:
Chinook-Rhame fine sandy loams, 1 to 6 percent slopes


muname:
Rhame-Chinook fine sandy loams, 6 to 15 percent slopes


muname:
Rhame-Fleak complex, 9 to 50 percent slopes


muname:
Gerda-Kirby complex, 1 to 15 percent slopes


muname:
Glendive and Havre soils, channeled, 0 to 3 percent slopes


muname:
Glendive fine sandy loam, 0 to 3 percent slopes


muname:
Hanly fine sandy loam, 0 to 6 percent slopes


muname:
Zeona loamy fine sand, 1 to 9 percent slopes


muname:
Ethridge silt loam, 1 to 3 percent slopes


muname:
Vebar-Parshall fine sandy loams, 0 to 6 percent slopes


muname:
Vebar-Tally fine sandy loams, 6 to 9 percent slopes


muname:
Vebar-Flasher-Tally complex, 9 to 15 percent slopes


muname:
Badland, outcrop-Patent complex, 6 to 25 percent slopes


muname:
Lonna-Cabbart silt loams, 6 to 35 percent slopes


muname:
Kirby-Badland, outcrop-Patent complex, 9 to 70 percent slopes


muname:
Littlemo-Chanta complex, 0 to 3 percent slopes


muname:
Lonna-Kirby-Cabbart complex, 3 to 50 percent slopes


muname:
AMOR-SHAMBO LOAMS, 3 TO 6 PERCENT SLOPES


muname:
WILLIAMS-ZAHL LOAMS, 6 TO 9 PERCENT SLOPES


muname:
ZAHL-WILLIAMS LOAMS, 9 TO 15 PERCENT SLOPES


muname:
ZAHL-WILLIAMS LOAMS, 15 TO 25 PERCENT SLOPES


muname:
MOREAU VARIANT CLAY LOAM, 1 TO 6 PERCENT SLOPES


muname:
REGENT SILTY CLAY LOAM, 1 TO 3 PERCENT SLOPES


muname:
REGENT SILTY CLAY LOAM, 3 TO 6 PERCENT SLOPES


muname:
REGENT SILTY CLAY LOAM, 6 TO 9 PERCENT SLOPES


muname:
REGENT-RHOADES SILTY CLAY LOAMS, 1 TO 6 PERCENT SLOPES


muname:
REGENT-RHOADES SILTY CLAY LOAMS, 6 TO 9 PERCENT SLOPES


muname:
RHOADES SILT LOAM, 1 TO 6 PERCENT SLOPES


muname:
RHOADES-CABBA LOAMS, 9 TO 15 PERCENT SLOPES


muname:
SAVAGE SILTY CLAY LOAM, 1 TO 3 PERCENT SLOPES


muname:
SAVAGE SILTY CLAY LOAM, 3 TO 6 PERCENT SLOPES


muname:
SAVAGE-RHOADES SILTY CLAY LOAMS, 1 TO 6 PERCENT SLOPES


muname:
CHERRY-VANDA COMPLEX, 3 TO 9 PERCENT SLOPES, GULLIED


muname:
VELVA FINE SANDY LOAM, 1 TO 3 PERCENT SLOPES


muname:
VEBAR-PARSHALL FINE SANDY LOAMS, 1 TO 6 PERCENT SLOPES


muname:
VEBAR-PARSHALL FINE SANDY LOAMS, 6 TO 9 PERCENT SLOPES


muname:
VEBAR FINE SANDY LOAMS, 9 TO 15 PERCENT SLOPES


muname:
VEBAR EXTREMELY STONY FINE SANDY LOAM, 3 TO 15 PERCENT SLOPES


muname:
BAAHISH FINE SANDY LOAM, 9 TO 50 PERCENT SLOPES


muname:
BRANDENBURG-CABBA LOAMS, 6 TO 50 PERCENT SLOPES


muname:
CABBA-CHAMA SILT LOAMS, 6 TO 9 PERCENT SLOPES


muname:
WILLIAMS EXTREMELY STONY LOAM, 1 TO 9 PERCENT SLOPES


muname:
WILLIAMS-NOONAN LOAMS, 3 TO 6 PERCENT SLOPES


muname:
WILLIAMS-NOONAN LOAMS, 6 TO 9 PERCENT SLOPES


muname:
CABBART-BADLAND COMPLEX, 15 TO 50 PERCENT SLOPES


muname:
BRANDENBURG-CABBART COMPLEX, 6 TO 50 PERCENT SLOPES


muname:
HANLY FINE SANDY LOAM, 0 TO 3 PERCENT SLOPES


muname:
WAYDEN SILTY CLAY, 9 TO 25 PERCENT SLOPES


muname:
AMOR-CABBA LOAMS, 9 TO 15 PERCENT SLOPES


muname:
EKALAKA FINE SANDY LOAM, 1 TO 6 PERCENT SLOPES


muname:
CABBA EXTREMELY STONY LOAM, 3 TO 25 PERCENT SLOPES


muname:
CABBA-BADLAND COMPLEX, 15 TO 120 PERCENT SLOPES


muname:
WABEK GRAVELLY LOAM, 1 TO 15 PERCENT SLOPES


muname:
BELFIELD-FARLAND SILT LOAMS, 1 TO 3 PERCENT SLOPES


muname:
BELFIELD-SAVAGE SILTY CLAY LOAMS, 1 TO 6 PERCENT SLOPES


muname:
BELFIELD-GRAIL SILTY CLAY LOAMS, 1 TO 3 PERCENT SLOPES


muname:
BELFIELD-MORTON SILT LOAMS, 1 TO 6 PERCENT SLOPES


muname:
CHERRY-CABBA COMPLEX, 9 TO 25 PERCENT SLOPES


muname:
BADLAND-CABBA-ARIKARA COMPLEX, 25 TO 120 PERCENT SLOPES


muname:
CHERRY SILTY CLAY LOAM, 1 TO 6 PERCENT SLOPES


muname:
CHERRY SILTY CLAY LOAM, 6 TO 9 PERCENT SLOPES


muname:
BAAHISH-ROCK OUTCROP COMPLEX, 15 TO 120 PERCENT SLOPES


muname:
FARLAND SILT LOAM, 1 TO 3 PERCENT SLOPES


muname:
FARLAND SILT LOAM, 3 TO 6 PERCENT SLOPES


muname:
FARLAND-RHOADES SILT LOAM, 1 TO 6 PERCENT SLOPES


muname:
COHAGEN-VEBAR FINE SANDY LOAMS, 9 TO 25 PERCENT SLOPES


muname:
COHAGEN-VEBAR-ROCK OUTCROP COMPLEX, 15 TO 40 PERCENT SLOPES


muname:
FLAXTON-WILLIAMS COMPLEX, 1 TO 6 PERCENT SLOPES


muname:
FLAXTON-WILLIAMS COMPLEX, 6 TO 9 PERCENT SLOPES


muname:
LAWTHER SILTY CLAY, 1 TO 3 PERCENT SLOPES


muname:
LAWTHER SILTY CLAY, 3 TO 6 PERCENT SLOPES


muname:
LEFOR FINE SANDY LOAM, 1 TO 6 PERCENT SLOPES


muname:
LEFOR FINE SANDY LOAM, 6 TO 9 PERCENT SLOPES


muname:
HAVRELON SILT LOAM, FAN, 1 TO 6 PERCENT SLOPES


muname:
LIHEN LOAMY FINE SAND, 1 TO 6 PERCENT SLOPES


muname:
LIHEN LOAMY FINE SAND, 6 TO 15 PERCENT SLOPES


muname:
MOREAU SILTY CLAY, 1 TO 3 PERCENT SLOPES


muname:
MOREAU SILTY CLAY, 3 TO 6 PERCENT SLOPES


muname:
MOREAU SILTY CLAY, 6 TO 9 PERCENT SLOPES


muname:
AMOR EXTREMELY STONY LOAM, 1 TO 9 PERCENT SLOPES


muname:
MORTON-RHOADES SILT LOAMS, 1 TO 6 PERCENT SLOPES


muname:
MORTON-RHOADES SILT LOAMS, 6 TO 9 PERCENT SLOPES


muname:
PARSHALL FINE SANDY LOAM, 1 TO 6 PERCENT SLOPES


muname:
BAAHISH-CABBART LOAMS, 6 TO 25 PERCENT SLOPES


muname:
CABBART-CHERRY SILT LOAMS, 9 TO 35 PERCENT SLOPES


muname:
CHAMA-CABBA SILT LOAMS, 3 TO 9 PERCENT SLOPES


muname:
FLASHER LOAMY SAND, 15 TO 45 PERCENT SLOPES


muname:
GRASSNA SILT LOAM, 1 TO 3 PERCENT SLOPES


muname:
GRAIL SILTY CLAY LOAM, 1 TO 3 PERCENT SLOPES


muname:
GLENDIVE FINE SANDY LOAM, 0 TO 3 PERCENT SLOPES


muname:
KORCHEA SILT LOAM, 0 TO 3 PERCENT SLOPES


muname:
MOREAU-WAYDEN-ABSHER COMPLEX, 3 TO 9 PERCENT SLOPES


muname:
PARSHALL FINE SANDY LOAM, 0 TO 3 PERCENT SLOPES


muname:
CABBART-ROCK OUTCROP COMPLEX, 15 TO 120 PERCENT SLOPES


muname:
BADLAND-CHERRY COMPLEX, 6 TO 75 PERCENT SLOPES


muname:
LAWTHER SILTY CLAY LOAM, 1 TO 3 PERCENT SLOPES


muname:
LAWTHER SILTY CLAY LOAM, 3 TO 6 PERCENT SLOPES


muname:
VEBAR FINE SANDY LOAM, 1 TO 6 PERCENT SLOPES


muname:
VEBAR FINE SANDY LOAM, 6 TO 9 PERCENT SLOPES


muname:
BEISIGL-FLASHER-VEBAR COMPLEX, 3 TO 9 PERCENT SLOPES


muname:
BEISIGL-FLASHER LOAMY SANDS, 9 TO 15 PERCENT SLOPES


muname:
CABBA-CHAMA SILT LOAMS, 3 TO 9 PERCENT SLOPES


muname:
CABBA-CHAMA SILT LOAMS, 9 TO 15 PERCENT SLOPES


muname:
MANDAN-LINTON SILT LOAMS, 0 TO 3 PERCENT SLOPES


muname:
LINTON-MANDAN SILT LOAMS, 3 TO 6 PERCENT SLOPES


muname:
BADLAND, OUTCROP-CABBA COMPLEX, 9 TO 70 PERCENT SLOPES


muname:
USTORTHENTS, LOAMY, 0 TO 6 PERCENT SLOPES


muname:
ARIKARA-SHAMBO-CABBA LOAMS, 9 TO 70 PERCENT SLOPES


muname:
BEISIGL-FLASHER-ARIKARA COMPLEX, 15 TO 70 PERCENT SLOPES


muname:
BANKS LOAMY FINE SAND, SLIGHTLY WET, 0 TO 6 PERCENT SLOPES


muname:
HAVRELON FINE SANDY LOAM, SLIGHTLY WET, 0 TO 2 PERCENT SLOPES


muname:
HAVRELON SILT LOAM, SLIGHTLY WET, 0 TO 2 PERCENT SLOPES


muname:
ZAHL-WILLIAMS LOAMS, DISSECTED, 15 TO 45 PERCENT SLOPES


muname:
AMOR-ARNEGARD LOAMS, 0 TO 3 PERCENT SLOPES


muname:
CHAMA-CABBA SILT LOAMS, 3 TO 6 PERCENT SLOPES


muname:
CHAMA-CABBA-SEN SILT LOAMS, 6 TO 9 PERCENT SLOPES


muname:
CABBA-CHAMA-SEN SILT LOAMS, 9 TO 15 PERCENT SLOPES


muname:
CABBA-CHAMA-ARNEGARD SILT LOAMS, 15 TO 70 PERCENT SLOPES


muname:
RINGLING-DAGLUM LOAMS, 6 TO 15 PERCENT SLOPES


muname:
BRANDENBURG-CABBA-SAVAGE COMPLEX, 6 TO 70 PERCENT SLOPES


muname:
SEN-CHAMA SILT LOAMS, 3 TO 6 PERCENT SLOPES


muname:
REEDER-FARNUF LOAMS, 3 TO 6 PERCENT SLOPES


muname:
FARLAND SILT LOAM, 0 TO 2 PERCENT SLOPES


muname:
FARLAND SILT LOAM, 2 TO 6 PERCENT SLOPES


muname:
FARLAND SILT LOAM, 6 TO 9 PERCENT SLOPES


muname:
FARLAND SILT LOAM, 9 TO 15 PERCENT SLOPES


muname:
MORTON-FARLAND SILT LOAMS, 3 TO 6 PERCENT SLOPES


muname:
CABBA-ROCK OUTCROP-CHAMA COMPLEX, 15 TO 70 PERCENT SLOPES


muname:
MORTON-CABBA SILT LOAMS, 3 TO 9 PERCENT SLOPES


muname:
GRAIL SILTY CLAY LOAM, 0 TO 2 PERCENT SLOPES


muname:
BELFIELD-GRAIL SILTY CLAY LOAMS, 0 TO 2 PERCENT SLOPES


muname:
GRAIL-BELFIELD SILTY CLAY LOAMS, 2 TO 6 PERCENT SLOPES


muname:
BELFIELD-DAGLUM SILT LOAMS, 0 TO 2 PERCENT SLOPES


muname:
BELFIELD-DAGLUM SILT LOAMS, 2 TO 6 PERCENT SLOPES


muname:
SAVAGE SILTY CLAY LOAM, 0 TO 2 PERCENT SLOPES


muname:
SAVAGE SILTY CLAY LOAM, 2 TO 6 PERCENT SLOPES


muname:
SAVAGE SILTY CLAY LOAM, 6 TO 9 PERCENT SLOPES


muname:
VELVA FINE SANDY LOAM, 0 TO 2 PERCENT SLOPES


muname:
REGENT-SAVAGE SILTY CLAY LOAMS, 0 TO 3 PERCENT SLOPES


muname:
REGENT-SAVAGE SILTY CLAY LOAMS, 3 TO 6 PERCENT SLOPES


muname:
REGENT-SAVAGE SILTY CLAY LOAMS, 6 TO 9 PERCENT SLOPES


muname:
REGENT-JANESBURG COMPLEX, 0 TO 6 PERCENT SLOPES


muname:
REGENT-JANESBURG COMPLEX, 6 TO 9 PERCENT SLOPES


muname:
MOREAU SILTY CLAY, 0 TO 6 PERCENT SLOPES


muname:
MOREAU-WAYDEN SILTY CLAYS, 6 TO 9 PERCENT SLOPES


muname:
MOREAU-WAYDEN SILTY CLAYS, 9 TO 15 PERCENT SLOPES


muname:
LAWTHER SILTY CLAY, 0 TO 2 PERCENT SLOPES


muname:
SEARING-RINGLING LOAMS, 0 TO 6 PERCENT SLOPES


muname:
LALLIE SILTY CLAY LOAM, PONDED, 0 TO 1 PERCENT SLOPES


muname:
RHOADES-SLICKSPOTS-DAGLUM COMPLEX, 0 TO 9 PERCENT SLOPES


muname:
DAGLUM-RHOADES COMPLEX, 0 TO 6 PERCENT SLOPES


muname:
DAGLUM-RHOADES COMPLEX, BEDROCK SUBSTRATUM, 6 TO 9 PERCENT SLOPES


muname:
DOGTOOTH-JANESBURG-CABBA COMPLEX, 6 TO 30 PERCENT SLOPES


muname:
RHOADES-DAGLUM FINE SANDY LOAMS, 0 TO 9 PERCENT SLOPES


muname:
EKALAKA-LAKOTA FINE SANDY LOAMS, 0 TO 6 PERCENT SLOPES


muname:
HARRIET SILT LOAM, 0 TO 2 PERCENT SLOPES


muname:
LAKOTA-EKALAKA FINE SANDY LOAMS, GULLIED, 0 TO 9 PERCENT SLOPES


muname:
DOGTOOTH-JANESBURG SILT LOAMS, 0 TO 6 PERCENT SLOPES


muname:
DESART-EKALAKA-TELFER COMPLEX, 0 TO 6 PERCENT SLOPES


muname:
LEFOR FINE SANDY LOAM, 0 TO 6 PERCENT SLOPES


muname:
DIMMICK SILTY CLAY, 0 TO 1 PERCENT SLOPES


muname:
VEBAR-FLASHER-TALLY COMPLEX, 9 TO 15 PERCENT SLOPES


muname:
FLASHER-VEBAR-PARSHALL COMPLEX, 9 TO 35 PERCENT SLOPES


muname:
VEBAR-PARSHALL FINE SANDY LOAMS, 0 TO 6 PERCENT SLOPES


muname:
TALLY-PARSHALL FINE SANDY LOAMS, 0 TO 6 PERCENT SLOPES


muname:
TALLY-PARSHALL FINE SANDY LOAMS, 6 TO 9 PERCENT SLOPES


muname:
VEBAR-FLASHER COMPLEX, 6 TO 9 PERCENT SLOPES


muname:
BEISIGL-LIHEN LOAMY FINE SANDS, 0 TO 6 PERCENT SLOPES


muname:
PARSHALL FINE SANDY LOAM, 0 TO 2 PERCENT SLOPES


muname:
BEISIGL-FLASHER LOAMY FINE SANDS, 6 TO 15 PERCENT SLOPES


muname:
LIHEN-PARSHALL COMPLEX, 0 TO 6 PERCENT SLOPES


muname:
FLASHER-ROCK OUTCROP-VEBAR COMPLEX, 9 TO 70 PERCENT SLOPES


muname:
WABEK-MANNING COMPLEX, 6 TO 15 PERCENT SLOPES


muname:
MANNING FINE SANDY LOAM, 0 TO 6 PERCENT SLOPES


muname:
WABEK-CABBA-SHAMBO COMPLEX, 6 TO 35 PERCENT SLOPES


muname:
VIRGELLE FINE SANDY LOAM, 0 TO 6 PERCENT SLOPES


muname:
TELFER LOAMY FINE SAND, 6 TO 15 PERCENT SLOPES


muname:
TELFER LOAMY FINE SAND, 15 TO 25 PERCENT SLOPES


muname:
WILLIAMS-BOWBELLS LOAMS, 0 TO 3 PERCENT SLOPES


muname:
WILLIAMS-BOWBELLS LOAMS, 3 TO 6 PERCENT SLOPES


muname:
WILLIAMS-REEDER LOAMS, 3 TO 6 PERCENT SLOPES


muname:
TEMVIK-WILTON SILT LOAMS, 0 TO 3 PERCENT SLOPES


muname:
TEMVIK-WILLIAMS SILT LOAMS, 3 TO 6 PERCENT SLOPES


muname:
BREIEN FINE SANDY LOAM, 0 TO 2 PERCENT SLOPES


muname:
MCKEEN LOAM, PONDED, 0 TO 1 PERCENT SLOPES


muname:
BANKS LOAMY FINE SAND, 0 TO 6 PERCENT SLOPES


muname:
HAVRELON FINE SANDY LOAM, 0 TO 2 PERCENT SLOPES


muname:
MINNEWAUKAN FINE SANDY LOAM, 0 TO 2 PERCENT SLOPES


muname:
HAVRELON SILT LOAM, 0 TO 2 PERCENT SLOPES


muname:
STRAW AND VELVA SOILS, CHANNELED, 0 TO 2 PERCENT SLOPES


muname:
LOHLER SILTY CLAY, 0 TO 2 PERCENT SLOPES


muname:
Ogontz fine sandy loam, 0 to 2 percent slopes


muname:
Bennington silt loam, 0 to 2 percent slopes


muname:
Bennington silt loam, 2 to 6 percent slopes


muname:
Bixler loamy fine sand, 0 to 2 percent slopes


muname:
Dunbridge loamy sand, 2 to 6 percent slopes


muname:
Elliott silt loam, bedrock substratum, 0 to 2 percent slopes


muname:
Ellsworth silt loam, 2 to 6 percent slopes


muname:
Ellsworth silt loam, 6 to 12 percent slopes, eroded


muname:
Elnora loamy fine sand, 0 to 4 percent slopes


muname:
Elnora loamy fine sand, bedrock substratum, 0 to 4 percent slopes


muname:
Fluvaquents, silty, 0 to 1 percent slopes, frequently flooded


muname:
Fries silty clay loam, 0 to 1 percent slopes


muname:
Fulton silty clay loam, 0 to 2 percent slopes


muname:
Gilford fine sandy loam, 0 to 1 percent slopes


muname:
Endoaquents, loamy, 0 to 1 percent slopes


muname:
Holly silt loam, 0 to 1 percent slopes, occasionally flooded


muname:
Hornell silt loam, 2 to 6 percent slopes


muname:
Harrod silt loam, 0 to 1 percent slopes, frequently flooded


muname:
Algiers silt loam, 0 to 2 percent slopes


muname:
Amanda loam, 12 to 18 percent slopes, eroded


muname:
Amanda-Dekalb-Rock outcrop association, 40 to 70 percent slopes


muname:
Zurich silt loam, 6 to 12 percent slopes, eroded


muname:
Zurich silt loam, 12 to 18 percent slopes, eroded


muname:
Zurich silt loam, 18 to 25 percent slopes, eroded


muname:
Zurich silt loam, 25 to 40 percent slopes


muname:
Hornell silty clay loam, 0 to 2 percent slopes


muname:
Kibbie fine sandy loam, 0 to 2 percent slopes


muname:
Mahoning silt loam, 0 to 2 percent slopes


muname:
Mahoning silt loam, 2 to 6 percent slopes


muname:
Mermill silty clay loam, 0 to 1 percent slopes


muname:
Milford silty clay loam, 0 to 1 percent slopes


muname:
Millsdale silty clay loam, 0 to 1 percent slopes


muname:
Miner silty clay loam, 0 to 1 percent slopes


muname:
Miner silt loam, bedrock substratum, 0 to 1 percent slopes


muname:
Mitiwanga silt loam, 0 to 2 percent slopes


muname:
Mitiwanga silt loam, 2 to 6 percent slopes


muname:
Nolin silt loam, 0 to 2 percent slopes, occasionally flooded


muname:
Oakville loamy fine sand, 0 to 6 percent slopes


muname:
Orrville silt loam, bedrock substratum, 0 to 2 percent slopes, occasionally flooded


muname:
Orrville silt loam, bedrock substratum, 0 to 2 percent slopes, frequently flooded


muname:
Oshtemo loamy sand, 0 to 6 percent slopes


muname:
Pewamo silty clay loam, 0 to 1 percent slopes


muname:
Plumbrook fine sandy loam, 0 to 2 percent slopes


muname:
Randolph silt loam, 0 to 2 percent slopes


muname:
Rawson sandy loam, 0 to 2 percent slopes


muname:
Rawson sandy loam, 2 to 6 percent slopes


muname:
Rimer loamy fine sand, 0 to 2 percent slopes


muname:
Saylesville silt loam, 25 to 40 percent slopes


muname:
Shinrock silt loam, 2 to 6 percent slopes


muname:
Shinrock silty clay loam, 6 to 12 percent slopes, eroded


muname:
Shinrock silty clay loam, 12 to 18 percent slopes, eroded


muname:
Spinks loamy fine sand, 0 to 6 percent slopes


muname:
Spinks loamy fine sand, 12 to 18 percent slopes


muname:
Tioga loam, 0 to 2 percent slopes, occasionally flooded


muname:
Toledo silty clay loam, 0 to 1 percent slopes


muname:
Toledo silty clay, 0 to 1 percent slopes


muname:
Toledo silty clay, 0 to 1 percent slopes, ponded


muname:
Tuscola fine sandy loam, 0 to 2 percent slopes


muname:
Tuscola fine sandy loam, 2 to 6 percent slopes


muname:
Udipsamments-Spinks complex, 0 to 6 percent slopes


muname:
Udorthents, loamy, 0 to 6 percent slopes


muname:
Wakeman sandy loam, 2 to 6 percent slopes


muname:
Wakeman sandy loam, 6 to 12 percent slopes


muname:
Bixler loamy fine sand, 2 to 6  percent slopes


muname:
Brecksville silt loam, 40 to 70 percent slopes


muname:
Cardington silt loam, 0 to 2 percent slopes


muname:
Cardington silt loam, 2 to 6 percent slopes


muname:
Cardington silty clay loam, 6 to 12 percent slopes, eroded


muname:
Castalia very channery loam, 0 to 2 percent slopes


muname:
Castalia very channery loam, 2 to 6 percent slopes


muname:
Castalia very channery loam, 12 to 18 percent slopes


muname:
Chili loam, loamy substratum, 2 to 6 percent slopes


muname:
Colwood silt loam, bedrock substratum, 0 to 1 percent slopes


muname:
Conotton gravelly loam, 6 to 12 percent slopes


muname:
Dekalb channery loam, 2 to 6 percent slopes


muname:
Dekalb channery loam, 12 to 18 percent slopes


muname:
Del Rey silt loam, 0 to 2 percent slopes


muname:
Dunbridge loamy sand, 0 to 2 percent slopes


muname:
Bixler loamy fine sand, 2 to 6 percent slopes


muname:
Castalia very stony loam, 1 to 6 percent slopes


muname:
Dixboro-Kibbie complex, 0 to 2 percent slopes


muname:
Dunbridge sandy loam, 1 to 4 percent slopes


muname:
Fulton silty clay loam, 0 to 3 percent slopes


muname:
Glenford silt loam, 2 to 6 percent slopes


muname:
Glynwood silt loam, 2 to 6 percent slopes


muname:
Haskins sandy loam, 1 to 4 percent slopes


muname:
Mentor silt loam, 25 to 50 percent slopes


muname:
Nappanee silt loam, 0 to 3 percent slopes


muname:
Rimer loamy fine sand, 1 to 4 percent slopes


muname:
Rossburg silt loam, occasionally flooded


muname:
Saylesville silty clay loam, 6 to 12 percent slopes, eroded


muname:
Seward loamy fine sand, 2 to 6 percent slopes


muname:
Tedrow loamy fine sand, 0 to 2 percent slopes


muname:
Tedrow-Dixboro complex, 0 to 2 percent slopes


muname:
Abilene clay loam, 0 to 1 percent slopes


muname:
Acme-Vinson complex, 1 to 3 percent slopes


muname:
Altus fine sandy loam, 0 to 1 percent slopes


muname:
Knoco-Badland complex, 1 to 30 percent slopes


muname:
Cornick-Vinson-Rock outcrop complex, 0 to 5 percent slopes


muname:
Hardeman fine sandy loam, 0 to 1 percent slopes


muname:
Hardeman fine sandy loam, 1 to 3 percent slopes


muname:
Hardeman fine sandy loam, 3 to 5 percent slopes


muname:
Hardeman fine sandy loam, 5 to 8 percent slopes


muname:
Grandfield, Devol, and Eda soils, 3 to 8 percent slopes, severely eroded


muname:
Hollister clay loam, 0 to 1 percent slopes


muname:
Tillman clay loam, 1 to 3 percent slopes


muname:
Madge loam, 3 to 5 percent slopes, eroded


muname:
Lawton-Brico complex, 3 to 8 percent slopes


muname:
Mangum clay, 0 to 1 percent slopes, occasionally flooded


muname:
Grandmore loamy fine sand, 0 to 1 percent slopes


muname:
McKnight loamy fine sand, 3 to 5 percent slopes


muname:
Grandfield and McKnight soils, 3 to 5 percent slopes, eroded


muname:
Grandfield and Farry soils, 0 to 1 percent slopes


muname:
Grandfield and Farry soils, 1 to 3 percent slopes


muname:
Grandfield and Delwin soils, 0 to 3 percent slopes


muname:
Nobscot fine sand, 0 to 5 percent slopes


muname:
Quinlan-Rock outcrop complex, 8 to 20 percent slopes


muname:
Quinlan-Woodward complex, 3 to 5 percent slopes, eroded


muname:
Quinlan-Woodward complex, 5 to 12 percent slopes


muname:
Rock outcrop-Brico complex, 8 to 45 percent slopes


muname:
Knoco-Cornick-Rock outcrop complex, 2 to 20 percent slopes


muname:
Westola and Lincoln soils, 0 to 1 percent slopes, frequently flooded


muname:
Hardeman-Likes-Fortyone complex, 5 to 20 percent slopes


muname:
Devol loamy fine sand, 0 to 3 percent slopes


muname:
Devol loamy fine sand, 3 to 8 percent slopes


muname:
Spur clay loam, 0 to 1 percent slopes, occasionally flooded


muname:
Spur loam, 0 to 1 percent slopes, occasionally flooded


muname:
Spur clay loam, 0 to 1 percent slopes, frequently flooded, channeled


muname:
St. Paul silt loam, 0 to 1 percent slopes


muname:
St. Paul silt loam, 1 to 3 percent slopes


muname:
Tillman and Hollister soils, 0 to 1 percent slopes


muname:
Jester fine sand, 1 to 30 percent slopes


muname:
Treadway clay loam, 0 to 3 percent slopes


muname:
Vernon-Knoco complex, 5 to 12 percent slopes


muname:
Knoco-Burford complex, 10 to 20 percent slopes


muname:
Gracemont soils, 0 to 1 percent slopes, frequently flooded


muname:
Burford clay loam, 1 to 3 percent slopes


muname:
Burford clay loam, 3 to 5 percent slopes


muname:
Burford clay loam, 3 to 5 percent slopes, eroded


muname:
Talpa-Burford complex, 0 to 5 percent slopes


muname:
Woodward-Quinlan complex, 3 to 5 percent slopes


muname:
Westola fine sandy loam, 0 to 1 percent slopes, occasionally flooded


muname:
Alspaugh clay loam, 15 to 30 percent slopes


muname:
Aschoff-Brightwood complex, 60 to 90 percent slopes


muname:
Zygore-Wilhoit gravelly loams, 30 to 60 percent slopes


muname:
Abiqua silty clay loam, 0 to 3 percent slopes


muname:
Abiqua silty clay loam, 3 to 5 percent slopes


muname:
Cumley silty clay loam, 2 to 20 percent slopes


muname:
Chehalem silt loam, 2 to 12 percent slopes


muname:
Henline very stony sandy loam, 6 to 30 percent slopes


muname:
Henline very stony sandy loam, 30 to 55 percent slopes


muname:
Henline very stony sandy loam, 55 to 80 percent slopes


muname:
Horeb gravelly silt loam, gravelly substratum, 0 to 15 percent slopes


muname:
Horeb gravelly silt loam, gravelly substratum, 15 to 35 percent slopes


muname:
Hullt clay loam, 20 to 30 percent slopes


muname:
Hullt clay loam, 30 to 60 percent slopes


muname:
Hazelair silt loam, 2 to 6 percent slopes


muname:
Hazelair silt loam, 6 to 20 percent slopes


muname:
Hazelair silty clay loam, 2 to 15 percent slopes, eroded


muname:
Jory silty clay loam, 2 to 7 percent slopes


muname:
Jory silty clay loam, 7 to 12 percent slopes


muname:
Jory silty clay loam, 12 to 20 percent slopes


muname:
Jory silty clay loam, 20 to 30 percent slopes


muname:
Kinney cobbly loam, 2 to 20 percent slopes


muname:
Kinney cobbly loam, 20 to 50 percent slopes


muname:
Kinney cobbly loam, 50 to 70 percent slopes


muname:
McCully clay loam, 2 to 30 percent slopes


muname:
McCully clay loam, 30 to 50 percent slopes


muname:
McCully clay loam, 50 to 70 percent slopes


muname:
Minniece silty clay loam, 0 to 8 percent slopes


muname:
McAlpin silty clay loam, 0 to 3 percent slopes


muname:
McAlpin silty clay loam, 3 to 6 percent slopes


muname:
McCully clay loam, 2 to 7 percent slopes


muname:
McCully clay loam, 7 to 12 percent slopes


muname:
McCully clay loam, 12 to 20 percent slopes


muname:
McCully clay loam, 20 to 30 percent slopes


muname:
McCully stony clay loam, 2 to 20 percent slopes


muname:
McCully very stony clay loam, 2 to 30 percent slopes


muname:
Nekia silty clay loam, 2 to 7 percent slopes


muname:
Nekia silty clay loam, 7 to 12 percent slopes


muname:
Nekia silty clay loam, 12 to 20 percent slopes


muname:
Nekia silty clay loam, 20 to 30 percent slopes


muname:
Nekia silty clay loam, 30 to 50 percent slopes


muname:
Nekia stony silty clay loam, 2 to 12 percent slopes


muname:
Nekia very stony silty clay loam, 2 to 30 percent slopes


muname:
Nekia very stony silty clay loam, 30 to 50 percent slopes


muname:
Steiwer and Chehulpum silt loams, 3 to 40 percent slopes


muname:
Salkum silty clay loam, 2 to 6 percent slopes


muname:
Salkum silty clay loam, 6 to 20 percent slopes


muname:
Salkum silty clay loam, basin, 0 to 6 percent slopes


muname:
Santiam silt loam, 0 to 3 percent slopes


muname:
Santiam silt loam, 3 to 6 percent slopes


muname:
Santiam silt loam, 6 to 15 percent slopes


muname:
Silverton silt loam, 2 to 12 percent slopes


muname:
Silverton silt loam, 12 to 20 percent slopes


muname:
Stayton silt loam, 0 to 7 percent slopes


muname:
Steiwer silt loam, 3 to 6 percent slopes


muname:
Steiwer silt loam, 6 to 20 percent slopes


muname:
Whetstone stony loam, 3 to 25 percent slopes


muname:
Willamette silt loam, 3 to 12 percent slopes


muname:
Witzel very stony silt loam, 3 to 40 percent slopes


muname:
Woodburn silt loam, 0 to 3 percent slopes


muname:
Woodburn silt loam, 3 to 12 percent slopes


muname:
Woodburn silt loam, 12 to 20 percent slopes


muname:
Whetstone stony loam, 25 to 55 percent slopes


muname:
Whetstone stony loam, 55 to 75 percent slopes


muname:
Willamette silt loam, 0 to 3 percent slopes


muname:
Fernwood very gravelly loam, 30 to 60 percent slopes


muname:
Hardscrabble silt loam, 7 to 20 percent slopes


muname:
Highcamp very gravelly loam, 30 to 60 percent slopes


muname:
Highcamp-Rock outcrop complex, 50 to 90 percent slopes


muname:
Highcamp-Soosap complex, 5 to 30 percent slopes


muname:
Kinzel-Divers complex, 5 to 30 percent slopes


muname:
Kinzel-Divers complex, 30 to 60 percent slopes


muname:
Springwater loam, 30 to 60 percent slopes


muname:
Wilhoit-Zygore gravelly loams, 5 to 30 percent slopes


muname:
Xerochrepts and Haploxerolls, very steep


muname:
DUNBAR AND ARDILLA FINE SANDY LOAMS, 0 TO 2 PERCENT SLOPES


muname:
FACEVILLE FINE SANDY LOAM, 2 TO 6 PERCENT SLOPES


muname:
HOCKLEY LOAMY FINE SAND, 0 TO 2 PERCENT SLOPES


muname:
HOCKLEY LOAMY FINE SAND, 2 TO 6 PERCENT SLOPES


muname:
NORFOLK AND DOTHAN SOILS, 0 TO 2 PERCENT SLOPES


muname:
ORANGEBURG LOAMY FINE SAND, 0 TO 2 PERCENT SLOPES


muname:
ORANGEBURG LOAMY FINE SAND, 2 TO 6 PERCENT SLOPES


muname:
WAGRAM LOAMY FINE SAND, 0 TO 6 PERCENT SLOPES


muname:
WANDO LOAMY FINE SAND, 0 TO 6 PERCENT SLOPES


muname:
WICKSBURG LOAMY FINE SAND, 0 TO 6 PERCENT SLOPES


muname:
AILEY SAND, MODERATELY WET, 0 TO 6 PERCENT SLOPES


muname:
AILEY LOAMY SAND, 6 TO 10 PERCENT SLOPES


muname:
AILEY LOAMY SAND, 10 TO 15 PERCENT SLOPES


muname:
AILEY GRAVELLY LOAMY SAND, 6 TO 15 PERCENT SLOPES


muname:
AILEY GRAVELLY LOAMY SAND, 15 TO 25 PERCENT SLOPES


muname:
BADIN SILT LOAM, 15 TO 40 PERCENT SLOPES


muname:
CANDOR SAND, MODERATELY WET, 0 TO 6 PERCENT SLOPES


muname:
CHENNEBY SILT LOAM, OCCASIONALLY FLOODED


muname:
CHEWACLA LOAM, 0 TO 2 PERCENT SLOPES, FREQUENTLY FLOODED


muname:
CLAYHAM CLAY LOAM, 2 TO 6 PERCENT SLOPES, ERODED


muname:
COWARTS LOAMY SAND, 6 TO 10 PERCENT SLOPES


muname:
COWARTS LOAMY SAND, 10 TO 15 PERCENT SLOPES


muname:
COWARTS GRAVELLY LOAMY SAND, 6 TO 10 PERCENT SLOPES


muname:
COWARTS GRAVELLY LOAMY SAND, 10 TO 15 PERCENT SLOPES


muname:
COWARTS GRAVELLY LOAMY SAND, 15 TO 25 PERCENT SLOPES


muname:
EMPORIA LOAMY SAND, 0 TO 2 PERCENT SLOPES


muname:
EMPORIA LOAMY SAND, 2 TO 6 PERCENT SLOPES


muname:
EMPORIA SANDY LOAM, 2 TO 6 PERCENT SLOPES, ERODED


muname:
EUNOLA LOAMY SAND, 0 TO 2 PERCENT SLOPES


muname:
FACEVILLE LOAMY SAND, 0 TO 2 PERCENT SLOPES


muname:
FACEVILLE LOAMY SAND, 2 TO 6 PERCENT SLOPES


muname:
FACEVILLE SANDY CLAY LOAM, 2 TO 6 PERCENT SLOPES, ERODED


muname:
GOLDSBORO LOAMY SAND, 0 TO 2 PERCENT SLOPES


muname:
HORNSVILLE SANDY CLAY LOAM, 2 TO 6 PERCENT SLOPES, ERODED


muname:
MARLBORO FINE SANDY LOAM, MODERATELY WET, 0 TO 2 PERCENT SLOPES


muname:
MARLBORO FINE SANDY LOAM, MODERATELY WET, 2 TO 6 PERCENT SLOPES


muname:
NANKIN LOAMY FINE SAND, 2 TO 6 PERCENT SLOPES


muname:
NANKIN SANDY CLAY LOAM, 2 TO 6 PERCENT SLOPES, ERODED


muname:
NANKIN SANDY CLAY LOAM, 6 TO 10 PERCENT SLOPES, ERODED


muname:
NOBOCO LOAMY SAND, 0 TO 2 PERCENT SLOPES


muname:
NOBOCO LOAMY SAND, 2 TO 6 PERCENT SLOPES


muname:
NOBOCO SANDY LOAM, 2 TO 6 PERCENT SLOPES, ERODED


muname:
NORFOLK LOAMY SAND, 0 TO 2 PERCENT SLOPES


muname:
NORFOLK LOAMY SAND, 2 TO 6 PERCENT SLOPES


muname:
NORFOLK SANDY CLAY LOAM, 2 TO 6 PERCENT SLOPES, ERODED


muname:
ORANGEBURG LOAMY SAND, 0 TO 2 PERCENT SLOPES


muname:
PELION LOAMY SAND, 0 TO 2 PERCENT SLOPES


muname:
PELION LOAMY SAND, 2 TO 6 PERCENT SLOPES


muname:
RIVERVIEW FINE SANDY LOAM, OCCASIONALLY FLOODED


muname:
UCHEE GRAVELLY SAND, 0 TO 6 PERCENT SLOPES


muname:
UCHEE GRAVELLY SAND, 6 TO 10 PERCENT SLOPES


muname:
WICKHAM FINE SANDY LOAM, 0 TO 2 PERCENT SLOPES


muname:
BLACKPIPE SILTY CLAY LOAM, 0 TO 2 PERCENT SLOPES


muname:
BLACKPIPE SILTY CLAY LOAM, 2 TO 6 PERCENT SLOPES


muname:
KIRLEY CLAY LOAM, 6 TO 15 PERCENT SLOPES


muname:
KIRLEY-CANNING COMPLEX, 2 TO 6 PERCENT SLOPES


muname:
KIRLEY-MOSHER COMPLEX, 0 TO 2 PERCENT SLOPES


muname:
KIRLEY-MOSHER COMPLEX, 2 TO 6 PERCENT SLOPES


muname:
KIRLEY-OTTUMWA COMPLEX, 0 TO 2 PERCENT SLOPES


muname:
KIRLEY-OTTUMWA COMPLEX, 2 TO 6 PERCENT SLOPES


muname:
KIRLEY-OTTUMWA COMPLEX, 6 TO 9 PERCENT SLOPES


muname:
KIRLEY-VIVIAN COMPLEX, 6 TO 15 PERCENT SLOPES


muname:
LAKOMA SILTY CLAY, 3 TO 6 PERCENT SLOPES


muname:
LAKOMA SILTY CLAY, 6 TO 9 PERCENT SLOPES


muname:
LAKOMA SILTY CLAY, 6 TO 15 PERCENT SLOPES


muname:
LAKOMA-VIVIAN COMPLEX, 9 TO 25 PERCENT SLOPES


muname:
MIDWAY SILTY CLAY LOAM, 15 TO 40 PERCENT SLOPES


muname:
NUNN-NIHILL COMPLEX, 6 TO 15 PERCENT SLOPES


muname:
OKATON-LAKOMA SILTY CLAYS, 15 TO 40 PERCENT SLOPES


muname:
OPAL-PROMISE CLAYS, 3 TO 6 PERCENT SLOPES


muname:
OPAL-PROMISE CLAYS, 6 TO 9 PERCENT SLOPES


muname:
OTTUMWA SILTY CLAY, 0 TO 3 PERCENT SLOPES


muname:
OTTUMWA SILTY CLAY, 3 TO 6 PERCENT SLOPES


muname:
OTTUMWA-CAPA COMPLEX, 0 TO 3 PERCENT SLOPES


muname:
OTTUMWA-LAKOMA SILTY CLAYS, 3 TO 6 PERCENT SLOPES


muname:
OTTUMWA-LAKOMA SILTY CLAYS, 6 TO 9 PERCENT SLOPES


muname:
OTTUMWA-RAZOR SILTY CLAYS, 6 TO 9 PERCENT SLOPES


muname:
OTTUMWA-RAZOR-SAVO COMPLEX, 6 TO 15 PERCENT SLOPES


muname:
PIERRE-SAMSIL CLAYS, 15 TO 25 PERCENT SLOPES


muname:
RAZOR-MIDWAY COMPLEX, 6 TO 15 PERCENT SLOPES


muname:
RAZOR-SHINGLE COMPLEX, 6 TO 15 PERCENT SLOPES


muname:
REE-CANNING LOAMS, 2 TO 6 PERCENT SLOPES


muname:
REE-CANNING LOAMS, 6 TO 9 PERCENT SLOPES


muname:
REE-VIVIAN COMPLEX, 6 TO 15 PERCENT SLOPES


muname:
SAMSIL-NIHILL COMPLEX, 6 TO 40 PERCENT SLOPES


muname:
SAMSIL-ROCK OUTCROP COMPLEX, 15 TO 60 PERCENT SLOPES


muname:
SANSARC-0PAL CLAYS, 9 TO 40 PERCENT SLOPES


muname:
SCHAMBER-SAMSIL COMPLEX, 6 TO 60 PERCENT SLOPES


muname:
SHINGLE SILTY CLAY LOAM, 15 TO 40 PERCENT SLOPES


muname:
SHINGLE-RAZOR COMPLEX, 15 TO 25 PERCENT SLOPES


muname:
WENDTE, CHANNELED-SANSARC COMPLEX, 0 TO 60 PERCENT SLOPES


muname:
WORTMAN-WANBLEE SILT LOAMS, 0 TO 2 PERCENT SLOPES


muname:
AMARILLO FINE SANDY LOAM, 0 TO 1 PERCENT SLOPES


muname:
AMARILLO FINE SANDY LOAM, 1 TO 3 PERCENT SLOPES


muname:
AMARILLO FINE SANDY LOAM, 3 TO 5 PERCENT SLOPES


muname:
AMARILLO LOAM, 0 TO 1 PERCENT SLOPES (ACUFF)


muname:
AMARILLO LOAM, 1 TO 2 PERCENT SLOPES (ACUFF)


muname:
AMARILLO LOAMY FINE SAND, 0 TO 3 PERCENT SLOPES


muname:
ARVANA FINE SANDY LOAM, 0 TO 1 PERCENT SLOPES


muname:
ARVANA FINE SANDY LOAM, 1 TO 3 PERCENT SLOPES


muname:
ARVANA FINE SANDY LOAM, SHALLOW, 0 TO 1 PERCENT SLOPES (SHARVANA)


muname:
BROWNFIELD FINE SAND, THIN SURFACE (PATRICIA)


muname:
BROWNFIELD SOILS, SEVERELY ERODED (PATRICIA)


muname:
GOMEZ AND PORTALES SOILS (GOMEZ-MIDESSA)


muname:
MANSKER FINE SANDY LOAM, 0 TO 1 PERCENT SLOPES


muname:
MANSKER FINE SANDY LOAM, 1 TO 3 PERCENT SLOPES


muname:
PORTALES FINE SANDY LOAM, 0 TO 1 PERCENT SLOPES (MIDESSA)


muname:
PORTALES FINE SANDY LOAM, 1 TO 3 PERCENT SLOPES (MIDESSA)


muname:
STEGALL LOAM, SHALLOW, 0 TO 1 PERCENT SLOPES (SLAUGHTER)


muname:
ZITA FINE SANDY LOAM, 0 TO 1 PERCENT SLOPES


muname:
ZITA FINE SANDY LOAM, 1 TO 3 PERCENT SLOPES


muname:
ALTOGA SILTY CLAY, 5 TO 12 PERCENT SLOPES, ERODED


muname:
AXTELL FINE SANDY LOAM, 0 TO 1 PERCENT SLOPES


muname:
AXTELL FINE SANDY LOAM, 1 TO 3 PERCENT SLOPES


muname:
AXTELL FINE SANDY LOAM, 2 TO 5 PERCENT SLOPES, ERODED


muname:
AXTELL-URBAN LAND COMPLEX, 1 TO 5 PERCENT SLOPES


muname:
BASTSIL FINE SANDY LOAM, 0 TO 3 PERCENT SLOPES


muname:
BASTSIL-URBAN LAND COMPLEX, 0 TO 2 PERCENT SLOPES


muname:
BRACKETT LOAM, 3 TO 5 PERCENT SLOPES (WHITEWRIGHT)


muname:
CROCKETT FINE SANDY LOAM, 0 TO 1 PERCENT SLOPES


muname:
CROCKETT FINE SANDY LOAM, 1 TO 3 PERCENT SLOPES


muname:
CROCKETT FINE SANDY LOAM, 2 TO 5 PERCENT SLOPES, ERODED


muname:
DALCO-URBAN LAND COMPLEX, 0 TO 3 PERCENT SLOPES


muname:
DUTEK LOAMY FINE SAND, 1 TO 5 PERCENT SLOPES


muname:
EDDY-BRACKETT COMPLEX, 8 TO 20 PERCENT SLOPES (EDDY-WHITEWRIGHT)


muname:
EDDY-BRACKETT-URBAN LAND COMPLEX, 8 TO 15 PERCENT SLOPES (EDDY-WHITEWRIGHT-URBAN LAND)


muname:
EDDY-STEPHEN COMPLEX, 1 TO 5 PERCENT SLOPES


muname:
EDDY-URBAN LAND COMPLEX, 1 TO 4 PERCENT SLOPES


muname:
EDDY-URBAN LAND COMPLEX, 4 TO 8 PERCENT SLOPES


muname:
EUFAULA LOAMY FINE SAND, 0 TO 2 PERCENT SLOPES


muname:
FERRIS-HEIDEN COMPLEX, 5 TO 12 PERCENT SLOPES


muname:
FERRIS-URBAN LAND COMPLEX, 5 TO 12 PERCENT SLOPES


muname:
HEIDEN CLAY, 2 TO 5 PERCENT SLOPES, ERODED


muname:
HOUSTON BLACK CLAY, 0 TO 1 PERCENT SLOPES


muname:
HOUSTON BLACK CLAY, 1 TO 3 PERCENT SLOPES


muname:
HOUSTON BLACK-URBAN LAND COMPLEX, 0 TO 4 PERCENT SLOPES


muname:
LEWISVILLE SILTY CLAY, 1 TO 3 PERCENT SLOPES


muname:
LEWISVILLE SILTY CLAY, 3 TO 5 PERCENT SLOPES


muname:
LEWISVILLE SILTY CLAY, 5 TO 8 PERCENT SLOPES


muname:
LEWISVILLE-URBAN LAND COMPLEX, 0 TO 4 PERCENT SLOPES


muname:
AUSTIN SILTY CLAY, 1 TO 3 PERCENT SLOPES


muname:
LEWISVILLE-URBAN LAND COMPLEX, 4 TO 8 PERCENT SLOPES


muname:
MABANK FINE SANDY LOAM, 0 TO 1 PERCENT SLOPES


muname:
MABANK FINE SANDY LOAM, 1 TO 3 PERCENT SLOPES


muname:
NORMANGEE CLAY LOAM, 1 TO 3 PERCENT SLOPES


muname:
RADER-MABANK COMPLEX, 0 TO 2 PERCENT SLOPES


muname:
RADER-URBAN LAND COMPLEX, 0 TO 2 PERCENT SLOPES


muname:
AUSTIN SILTY CLAY, 3 TO 5 PERCENT SLOPES


muname:
SILAWA FINE SANDY LOAM, 1 TO 3 PERCENT SLOPES


muname:
SILAWA FINE SANDY LOAM, 3 TO 8 PERCENT SLOPES


muname:
SILAWA FINE SANDY LOAM, 2 TO 8 PERCENT SLOPES, ERODED


muname:
SILAWA-URBAN LAND COMPLEX, 2 TO 6 PERCENT SLOPES


muname:
SILSTID LOAMY FINE SAND, 0 TO 3 PERCENT SLOPES


muname:
SILSTID-URBAN LAND COMPLEX, 0 TO 6 PERCENT SLOPES


muname:
STEPHEN SILTY CLAY, 1 TO 3 PERCENT SLOPES


muname:
STEPHEN SILTY CLAY, 3 TO 5 PERCENT SLOPES


muname:
STEPHEN-URBAN LAND COMPLEX, 1 TO 4 PERCENT SLOPES


muname:
AUSTIN-LEWISVILLE COMPLEX, 5 TO 8 PERCENT SLOPES, ERODE D


muname:
AUSTIN-URBAN LAND COMPLEX, 0 TO 2 PERCENT SLOPES


muname:
WILSON-URBAN LAND COMPLEX, 0 TO 2 PERCENT SLOPES


muname:
AUSTIN-URBAN LAND COMPLEX, 2 TO 5 PERCENT SLOPES


muname:
BIPPUS CLAY LOAM, 0 TO 2 PERCENT SLOPES, OCCASIONALLY FLOODED


muname:
BERDA-POTTER COMPLEX, 2 TO 12 PERCENT SLOPES


muname:
CHAPEL CLAY, 0 TO 1 PERCENT SLOPES, OCCASIONALLY PONDED


muname:
KIMBERSON GRAVELLY LOAM, 0 TO 3 PERCENT SLOPES


muname:
LENORAH FINE SANDY LOAM, 0 TO 1 PERCENT SLOPES


muname:
MIDESSA FINE SANDY LOAM, 0 TO 1 PERCENT SLOPES


muname:
MIDESSA FINE SANDY LOAM, 1 TO 3 PERCENT SLOPES


muname:
POSEY FINE SANDY LOAM, 0 TO 1 PERCENT SLOPES


muname:
POSEY FINE SANDY LOAM, 1 TO 3 PERCENT SLOPES


muname:
POSEY FINE SANDY LOAM, 3 TO 8 PERCENT SLOPES


muname:
RANCO CLAY, 0 TO 1 PERCENT SLOPES, FREQUENTLY PONDED


muname:
SHARVANA FINE SANDY LOAM, 0 TO 3 PERCENT SLOPES


muname:
CRETA VERY FINE SANDY LOAM, 1 TO 5 PERCENT SLOPES


muname:
LEVELLAND SOILS, 0 TO 2 PERCENT SLOPES, OCCASIONALLY FLOODED


muname:
NUTIVOLI FINE SAND, 3 TO 8 PERCENT SLOPES


muname:
MIDESSA AND POSEY SOILS, 3 TO 8 PERCENT SLOPES


muname:
PATRICIA AND AMARILLO SOILS, 0 TO 3 PERCENT SLOPES


muname:
SPARENBERG CLAY,0 TO 1 PERCENT SLOPES, OCCASIONALLY PONDED


muname:
TOKIO LOAMY FINE SAND, 0 TO 2 PERCENT SLOPES


muname:
TOKIO FINE SANDY LOAM, 0 TO 1 PERCENT SLOPES


muname:
YELLOWLAKE SILTY CLAY LOAM, 0 TO 1 PERCENT SLOPES, RARELY PONDED


muname:
YELLOWHOUSE VERY GRAVELLY CLAY LOAM, 3 TO 20 PERCENT SLOPES


muname:
VEAL FINE SANDY LOAM, 1 TO 3 PERCENT SLOPES


muname:
VEAL FINE SANDY LOAM, 3 TO 5 PERCENT SLOPES


muname:
WEYMOUTH-VERNON CLAY LOAMS, 1 TO 3 PERCENT SLOPES


muname:
AMARILLO AND COBB FINE SANDY LOAMS, 1 TO 3 PERCENT SLOP ES (MILES AND COBB)


muname:
AMARILLO AND COBB FINE SANDY LOAMS, 3 TO 5 PERCENT SLOP ES (MILES AND COBB)


muname:
ARVANA FINE SANDY LOAM, SHALLOW, 1 TO 3 PERCENT SLOPES (SHARVANA)


muname:
BERTHOUD LOAM, 1 TO 3 PERCENT SLOPES (BERDA)


muname:
BERTHOUD LOAM, 3 TO 5 PERCENT SLOPES (BERDA)


muname:
BROWNFIELD FINE SAND, 0 TO 3 PERCENT SLOPES


muname:
BROWNFIELD FINE SAND, THIN SURFACE VARIANT, 0 TO 3 PERC ENT SLOPES (PATRICIA)


muname:
LATOM FINE SANDY LOAM, 1 TO 8 PERCENT SLOPES


muname:
MOBEETIE FINE SANDY LOAM, 1 TO 3 PERCENT SLOPES


muname:
MOBEETIE FINE SANDY LOAM, 3 TO 5 PERCENT SLOPES


muname:
OZONA CLAY LOAM, 1 TO 3 PERCENT SLOPES (VALERA)


muname:
PORTALES FINE SANDY LOAM, 0 TO 1 PERCENT SLOPES (MIDESS A)


muname:
PORTALES FINE SANDY LOAM, 1 TO 3 PERCENT SLOPES (MIDESS A)


muname:
SIMONA FINE SANDY LOAM, 1 TO 3 PERCENT SLOPES


muname:
SPADE-LATOM SANDY LOAMS, 1 TO 3 PERCENT SLOPES


muname:
SPADE-LATOM SANDY LOAMS, 3 TO 5 PERCENT SLOPES


muname:
SPRINGER FINE SANDY LOAM, 0 TO 1 PERCENT SLOPES


muname:
SPRINGER FINE SANDY LOAM, 1 TO 3 PERCENT SLOPES


muname:
STAMFORD AND DALBY CLAYS, 0 TO 1 PERCENT SLOPES (STAMFORD STAMFO RD)


muname:
STAMFORD AND DALBY CLAYS, 1 TO 3 PERCENT SLOPES (STAMFORD STAMFO RD)


muname:
UVALDE SILTY CLAY LOAM, 0 TO 1 PERCENT SLOPES (ANGELO)


muname:
UVALDE SILTY CLAY LOAM, 1 TO 3 PERCENT SLOPES (ANGELO)


muname:
BIPPUS FINE SANDY LOAM, FREQUENTLY FLOODED


muname:
ESTACADO CLAY LOAM, 0 TO 1 PERCENT SLOPES


muname:
ESTACADO CLAY LOAM, 1 TO 3 PERCENT SLOPES


muname:
ESTACADO-URBAN LAND COMPLEX, 0 TO 2 PERCENT SLOPES


muname:
MANSKER CLAY LOAM, 1 TO 3 PERCENT SLOPES


muname:
MANSKER CLAY LOAM, 3 TO 5 PERCENT SLOPES


muname:
MOBEETIE FINE SANDY LOAM, 5 TO 8 PERCENT SLOPES


muname:
ACUFF-URBAN LAND COMPLEX, 0 TO 2 PERCENT SLOPES


muname:
OLTON-URBAN LAND COMPLEX, 0 TO 2 PERCENT SLOPES


muname:
POSEY FINE SANDY LOAM, 3 TO 5 PERCENT SLOPES


muname:
POSEY FINE SANDY LOAM, 5 TO 8 PERCENT SLOPES


muname:
POTTER-KIMBROUGH-URBAN LAND COMPLEX, 1 TO 5 PERCENT SLO PES


muname:
PULLMAN CLAY LOAM, 0 TO 1 PERCENT SLOPES


muname:
AMARILLO-URBAN LAND COMPLEX, 0 TO 2 PERCENT SLOPES


muname:
ARVANA LOAMY FINE SAND, 1 TO 5 PERCENT SLOPES


muname:
ARCH FINE SANDY LOAM, 0 TO 1 PERCENT SLOPES


muname:
BROWNFIELD-NUTIVOLI COMPLEX, 1 TO 8 PERCENT SLOPES


muname:
BROWNFIELD SOILS, 1 TO 8 PERCENT SLOPES, HUMMOCKY


muname:
CEDARLAKE SOILS, 0 TO 1 PERCENT SLOPES, FREQUENTLY PONDED


muname:
GOMEZ LOAMY FINE SAND, 0 TO 2 PERCENT SLOPES


muname:
LENORAH AND HINDMAN SOILS, 0 TO 2 PERCENT SLOPES


muname:
LAMESA SOILS, 0 TO 1 PERCENT SLOPES, FREQUENTLY PONDED


muname:
MIDESSA, POTTER, AND POSEY SOILS, 3 TO 12 PERCENT SLOPES


muname:
PLAINS-YOAKRAN-NUTIVOLI COMPLEX, 1 TO 8 PERCENT SLOPES


muname:
SPARENBERG CLAY, 0 TO 1 PERCENT SLOPES, OCCASIONALLY PONDED


muname:
BLUE STAR GRAVELLY LOAM, 6 TO 20 PERCENT SLOPES


muname:
BLUE STAR GRAVELLY LOAM, GRAVELLY SUBSOIL VARIANT, 6 TO 10 PERCENT SLOPES


muname:
ELZINGA-MAUGHAN COMPLEX, 25 TO 50 PERCENT SLOPES


muname:
ECCLES FINE SANDY LOAM, 0 TO 1 PERCENT SLOPES


muname:
ECCLES FINE SANDY LOAM, 1 TO 6 PERCENT SLOPES


muname:
ECCLES FINE SANDY LOAM, 6 TO 10 PERCENT SLOPES


muname:
ECCLES LOAMY SAND, SANDY VARIANT, 1 TO 6 PERCENT SLOPES


muname:
FOXOL-ROCK OUTCROP COMPLEX, 50 TO 70 PERCENT SLOPES


muname:
PASS CANYON-ROCK OUTCROP COMPLEX,6 TO 30 PERCENT SLOPES


muname:
PARLEYS LOAM, COOL, 0 TO 3 PERCENT SLOPES


muname:
PARLEYS SILT LOAM, 0 TO 1 PERCENT SLOPES


muname:
PARLEYS SILT LOAM, 1 TO 6 PERCENT SLOPES


muname:
PARLEYS SILT LOAM,  6 TO 10 PERCENT SLOPES


muname:
PARLEYS SILT LOAM, 10 TO 20 PERCENT SLOPES


muname:
PARLEYS SILTY CLAY LOAM, 0 TO 3 PERCENT SLOPES


muname:
PARLEYS-MUNK COMPLEX, 6 TO 10 PERCENT SLOPES


muname:
PARLEYS-MUNK COMPLEX, 10 TO 20 PERCENT SLOPES


muname:
PARLEYS-POMAT SILT LOAMS, 6 TO 10 PERCENT SLOPES


muname:
PETEETNEET PEAT, MODERATELY DEEP VARIANT


muname:
POMAT SILT LOAM, 10 TO 30 PERCENT SLOPES


muname:
POMAT SILT LOAM, 30 TO 40 PERCENT SLOPES,ERODED


muname:
POMAT-KEARNS SILT LOAMS, 10 TO 30 PERCENT SLOPES


muname:
POMAT-PARLEYS SILT LOAMS, 10 TO 30 PERCENT SLOPES


muname:
RICHMOND-MIDDLE COMPLEX, 30 TO 70 PERCENT SLOPES,ERODED


muname:
ROZLEE-ROCK OUTCROP COMPLEX, 30 TO 70 PERCENT SLOPES


muname:
RED ROCK SILT LOAM, HIGH RAINFALL, 0 TO 3 PERCENT SLOPES


muname:
RED ROCK SILT LOAM, 0 TO 1 PERCENT SLOPES


muname:
RED ROCK SILT LOAM, 1 TO 6 PERCENT SLOPES


muname:
RIDD-ROCK OUTCROP COMPLEX, 10 TO 30 PERCENT SLOPES


muname:
ABELA GRAVELLY LOAM, 10 TO 20 PERCENT SLOPES


muname:
ABELA STONY LOAM, 6 TO 20 PERCENT SLOPES


muname:
SANDALL COBBLY SILT LOAM, 10 TO 30 PERCENT SLOPES


muname:
SANDALL COBBLY SILT LOAM, 30 TO 60 PERCENT SLOPES


muname:
SANDALL-ROCK OUTCROP COMPLEX, 3 TO 30 PERCENT SLOPES


muname:
SAXBY-THIOKOL COMPLEX, 1 TO 6 PERCENT SLOPES


muname:
SANPETE GRAVELLY SILT LOAM, 6 TO 30 PERCENT SLOPES


muname:
SANPETE GRAVELLY SILT LOAM, HIGH RAINFALL, 1 TO 6 PERCENT SLOPES


muname:
SANPETE GRAVELLY SILT LOAM, HIGH RAINFALL, 6 TO 10 PERCENT SLOPES


muname:
SANPETE GRAVELLY SILT LOAM, HIGH RAINFALL,10 TO 30 PERCENT SLOPES


muname:
SANPETE GRAVELLY SILT LOAM, HIGH RAINFALL, 30 TO 50 PERCENT SLOPES


muname:
SHEEPROCK GRAVELLY SANDY LOAM, 6 TO 10 PERCENT SLOPES


muname:
SHEEPROCK GRAVELLY LOAM, 10 TO 40 PERCENT SLOPES, SEVERELY ERODED


muname:
SNOWVILLE GRAVELLY SILT LOAM, 6 TO 20 PERCENT SLOPES


muname:
STERLING GRAVELLY LOAM, 1 TO 6 PERCENT SLOPES


muname:
STERLING GRAVELLY LOAM, 6 TO 20 PERCENT SLOPES


muname:
STERLING GRAVELLY LOAM, 20 TO 30 PERCENT SLOPES


muname:
STERLING GRAVELLY LOAM, 30 TO 50 PERCENT SLOPES


muname:
STERLING VERY STONY LOAM, 10 TO 30 PERCENT SLOPES


muname:
STERLING-PARLEYS COMPLEX, 6 TO 20 PERCENT SLOPES


muname:
THIOKOL SILT LOAM, 0 TO 1 PERCENT SLOPES


muname:
THIOKOL SILT LOAM, 1 TO 6 PERCENT SLOPES


muname:
THIOKOL SILT LOAM, 6 TO 10 PERCENT SLOPES


muname:
THIOKOL SILT LOAM, LOW RAINFALL, 0 TO 1 PERCENT SLOPES


muname:
THIOKOL SILT LOAM, LOW RAINFALL, 1 TO 3 PERCENT SLOPES


muname:
TIMPANOGOS LOAM, COOL, 0 TO 3 PERCENT SLOPES


muname:
TIMPANOGOS SILT LOAM, 1 TO 6 PERCENT SLOPES


muname:
TIMPANOGOS SILT LOAM, 6 TO 10 PERCENT SLOPES


muname:
WASATCH GRAVELLY SANDY LOAM, 3 TO 10 PERCENT SLOPES


muname:
WASATCH GRAVELLY SANDY LOAM, 10 TO 25 PERCENT SLOPES


muname:
WASATCH GRAVELLY SANDY LOAM, GRAVELLY SUBSOIL VARIANT, 30 TO 70 PERCENT SLOPES


muname:
WASATCH COBBLY SANDY LOAM, GRAVELLY SUBSOIL VARIANT, 10 TO 20 PERCENT SLOPES


muname:
WHEELON SILT LOAM, 30 TO 60 PERCENT SLOPES


muname:
WHEELON GRAVELLY SILT LOAM, SHALLOW VARIANT, 20 TO 60 PERCENT


muname:
WHEELON-COLLINSTON SILT LOAMS, 10 TO 30 PERCENT SLOPES


muname:
WINDMILL GRAVELLY LOAM, 1 TO 6 PERCENT SLOPES


muname:
WINDMILL GRAVELLY LOAM, 6 TO 10 PERCENT SLOPES


muname:
WINDMILL GRAVELLY LOAM, 10 TO 20 PERCENT SLOPES


muname:
WOODS CROSS SILTY CLAY LOAM, MODERATELY SALINE


muname:
YEATES HOLLOW COBBLY CLAY LOAM,20 TO 30 PERCENT SLOPES


muname:
YEATES HOLLOW COBBLY CLAY LOAM, 30 TO 60 PERCENT SLOPES


muname:
ANTY FINE SANDY LOAM, 1 TO 6 PERCENT SLOPES


muname:
ANTY FINE SANDY LOAM, 6 TO 10 PERCENT SLOPES


muname:
BROAD COBBLY LOAM, 20 TO 30 PERCENT SLOPES


muname:
BROAD COBBLY LOAM, 30 TO 60 PERCENT SLOPES


muname:
BINGHAM GRAVELLY LOAM, 1 TO 6 PERCENT SLOPES


muname:
BINGHAM GRAVELLY LOAM, 6 TO 10 PERCENT SLOPES


muname:
RIDD-ROCK OUTCROP COMPLEX, 30 TO 70 PERCENT SLOPES


muname:
MELLOR-THIOKOL SILT LOAMS, 1 TO 6 PERCENT SLOPES


muname:
MIDDLE-ROCK OUTCROP COMPLEX,10 TO 30 PERCENT SLOPES


muname:
MIDDLE-ROCK OUTCROP COMPLEX,30 TO 60 PERCENT SLOPES


muname:
COLLINSTON-WHEELON SILT LOAMS, 6 TO 10 PERCENT SLOPES


muname:
DEJARNET GRAVELLY SILT LOAM, 1 TO 6 PERCENT SLOPES


muname:
DEJARNET GRAVELLY SILT LOAM, 6 TO 10 PERCENT SLOPES


muname:
MENDON SILT LOAM, 6 TO 10 PERCENT SLOPES


muname:
MILLVILLE SILT LOAM, 0 TO 2 PERCENT SLOPES


muname:
MILLVILLE SILT LOAM, 2 TO 4 PERCENT SLOPES


muname:
MIDDLE COBBLY SILT LOAM, 10 TO 30 PERCENT SLOPES


muname:
MIDDLE COBBLY SILT LOAM,30 TO 70 PERCENT SLOPES


muname:
MILLVILLE SILT LOAM, MODERATELY DEEP WATER TABLE,2 TO 4 PERCENT SLOPES


muname:
MUNK GRAVELLY SILT LOAM, 10 TO 20 PERCENT SLOPES


muname:
PALISADE SILT LOAM, 1 TO 6 PERCENT SLOPES


muname:
PALISADE SILT LOAM, 6 TO 10 PERCENT SLOPES


muname:
FORSGREN SILT LOAM, 1 TO 6 PERCENT SLOPES


muname:
FORSGREN SILT LOAM, 6 TO 10 PERCENT SLOPES


muname:
FORSGREN SILT LOAM, 10 TO 20 PERCENT SLOPES


muname:
FRANCIS LOAMY FINE SAND, 3 TO 6 PERCENT SLOPES


muname:
GORING-YEATES HOLLOW ASSOCIATION, MODERATELY STEEP


muname:
GEMSON SILTY CLAY LOAM, 6 TO 10 PERCENT SLOPES


muname:
GEMSON SILTY CLAY LOAM, 10 TO 20 PERCENT SLOPES


muname:
HANSEL SILT LOAM, 6 TO 10 PERCENT SLOPES


muname:
HENDRICKS SILT LOAM, 1 TO 6 PERCENT SLOPES


muname:
HENDRICKS SILT LOAM, 6 TO 10 PERCENT SLOPES


muname:
HENDRICKS SILT LOAM, 10 TO 20 PERCENT SLOPES


muname:
HENDRICKS COMPLEX, 6 TO 10 PERCENT SLOPES


muname:
HUPP GRAVELLY SILT LOAM, 1 TO 6 PERCENT SLOPES


muname:
HUPP GRAVELLY SILT LOAM, 6 TO 10 PERCENT SLOPES


muname:
JAMES CANYON LOAM, 0 TO 3 PERCENT SLOPES


muname:
KAPOD STONY LOAM, 6 TO 20 PERCENT SLOPES


muname:
KEARNS SILT LOAM, 6 TO 10 PERCENT SLOPES


muname:
KEARNS SILT LOAM, 10 TO 20 PERCENT SLOPES


muname:
KEARNS-STINGAL COMPLEX, 6 TO 10 PERCENT SLOPES


muname:
KEARNS SILT LOAM, HIGH LIME VARIANT, 10 TO 20 PERCENT SLOPES


muname:
KIDMAN FINE SANDY LOAM, 0 TO 2 PERCENT SLOPES


muname:
KIDMAN FINE SANDY LOAM, 2 TO 4 PERCENT SLOPES


muname:
KILBURN GRAVELLY SANDY LOAM, 3 TO 6 PERCENT SLOPES


muname:
KILBURN GRAVELLY SANDY LOAM, 6 TO 10 PERCENT SLOPES


muname:
KILBURN GRAVELLY SANDY LOAM, 10 TO 20 PERCENT SLOPES


muname:
KILBURN GRAVELLY SANDY LOAM, 20 TO 30 PERCENT SLOPES


muname:
KILBURN GRAVELLY SANDY LOAM, 30 TO 60 PERCENT SLOPES


muname:
KILBURN GRAVELLY LOAM, 1 TO 3 PERCENT SLOPES


muname:
ACANA GRAVELLY LOAM, 1 TO 3 PERCENT SLOPES


muname:
BORVANT GRAVELLY LOAM, 5 TO 15 PERCENT SLOPES


muname:
BROBETT-PLEGOMIR ASSOCIATION, 3 TO 8 PERCENT SLOPES


muname:
CROOKED CREEK SILTY CLAY LOAM, 0 TO 2 PERCENT SLOPES


muname:
CROOKED CREEK-HUPP COMPLEX, 1 TO 6 PERCENT SLOPES


muname:
DAHAR-CODQUIN GRAVELLY SANDY LOAMS, 8 TO 60 PERCENT SLOPES


muname:
DATEMAN-BICKMORE, COOL-NIELSEN FAMILIES COMPLEX, 20 TO 60 PERCENT SLOPES


muname:
DECLO-DARKBULL ASSOCIATION, 1 TO 10 PERCENT SLOPES


muname:
DECLO-LEMBOS-TARNACH ASSOCIATION, 1 TO 6 PERCENT SLOPES


muname:
DONNARDO GRAVELLY LOAM, 2 TO 8 PERCENT SLOPES


muname:
DONNARDO-BIRDOW COMPLEX, 1 TO 8 PERCENT SLOPES


muname:
ACANA-JERICHO ASSOCIATION, 3 TO 10 PERCENT SLOPES


muname:
DYNAL-PLAYAS ASSOCIATION, 0 TO 15 PERCENT SLOPES


muname:
FONTREEN-BORVANT GRAVELLY LOAMS, 5 TO 20 PERCENT SLOPES


muname:
FONTREEN-BULLUMP COMPLEX, 3 TO 15 PERCENT SLOPES


muname:
FONTREEN-PHAGE ASSOCIATION, 15 TO 40 PERCENT SLOPES


muname:
HADES-BEARSKIN-ROCK OUTCROP ASSOCIATION, 5 TO 30 PERCENT SLOPES


muname:
HIKO PEAK GRAVELLY LOAM, 3 TO 12 PERCENT SLOPES


muname:
HIKO PEAK-KUNZLER ASSOCIATION, 3 TO 12 PERCENT SLOPES


muname:
HIKO PEAK-SHEEPROCK-ROCK OUTCROP ASSOCIATION, 3 TO 25 PE RCENT SLOPES


muname:
HIKO PEAK-TAYLORSFLAT COMPLEX, 1 TO 12 PERCENT SLOPES


muname:
HIKO PEAK-TAYLORSFLAT-SKUMPAH ASSOCIATION, 1 TO 12 PERCE NT SLOPES


muname:
ACORD VERY COBBLY LOAM, 5 TO 15 PERCENT SLOPES


muname:
HIKO SPRINGS-OKRIST ASSOCIATION, 1 TO 8 PERCENT SLOPES


muname:
JERICHO-AMTOFT COMPLEX, 20 TO 50 PERCENT SLOPES


muname:
JUGHANDLE-PARKAY FAMILIES COMPLEX, 15 TO 45 PERCENT SLOP ES


muname:
KAPOD-DONNARDO COMPLEX, 2 TO 10 PERCENT SLOPES


muname:
KOOSHAREM SILT LOAM, 0 TO 2 PERCENT SLOPES


muname:
KUNZLER-LEMBOS ASSOCIATION, 1 TO 5 PERCENT SLOPES


muname:
LEMBOS-JERICHO-SCALADE COMPLEX, 1 TO 30 PERCENT SLOPES


muname:
LEMBOS-TAYLORSFLAT COMPLEX, 1 TO 6 PERCENT SLOPES


muname:
LUNDY-SONLET-LODAR VERY GRAVELLY LOAMS, 15 TO 50 PERCENT SLOPES


muname:
LYNNDYL LOAMY SAND, 1 TO 5 PERCENT SLOPES


muname:
ANT FLAT-ACORD ASSOCIATION, 10 TO 30 PERCENT SLOPES


muname:
MELLOR-DECLO SILT LOAMS, 2 TO 12 PERCENT SLOPES


muname:
MELLOR-POMAT ASSOCIATION, 0 TO 3 PERCENT SLOPES


muname:
BULLUMP-SONLET-RODROF ASSOCIATION, 5 TO 30 PERCENT SLOPE S


muname:
CLAVICON-ROCK OUTCROP COMPLEX, 30 TO 60 PERCENT SLOPES


muname:
CLIFFDOWN VERY GRAVELLY SANDY LOAM, ALKALI, 3 TO 10 PERCENT SLOPES


muname:
CLIFFDOWN VERY GRAVELLY LOAM, 3 TO 10 PERCENT SLOPES


muname:
CLIFFDOWN-HIKO PEAK-OKRIST, THICK SURFACE ASSOCIATION, 3 TO 12 PERCENT SLOPES


muname:
CLIFFDOWN, ALKALI-ROCK OUTCROP-PROMO COMPLEX, 10 TO 35 PE RCENT SLOPES


muname:
COLLARD, MOIST-HUPP COMPLEX, 2 TO 10 PERCENT SLOPES


muname:
ACANA-COLLARD GRAVELLY LOAMS, 3 TO 8 PERCENT SLOPES


muname:
COTTONTHOMAS-TOMSHERRY FINE SANDY LOAMS, 0 TO 15 PERCENT SLOPES


muname:
NIELSEN-BICKMORE FAMILIES-ROCK OUTCROP ASSOCIATION, 20 T O 60 PERCENT SLOPES


muname:
OKRIST-OKRIST, THICK SURFACE COMPLEX, 1 TO 10 PERCENT SLO PES


muname:
OVERLAND-SONLET COMPLEX, 15 TO 40 PERCENT SLOPES


muname:
PARKAY FAMILY GRAVELLY LOAM, MOIST, 5 TO 35 PERCENT SLOPE S


muname:
PARKAY-DATEMAN FAMILIES ASSOCIATION, 20 TO 60 PERCENT SLOPES


muname:
PARKAY-BROAD CANYON FAMILIES ASSOCIATION, 20 TO 60 PERCENT SLOPES


muname:
BICKMORE-EYRE FAMILIES-ROCK OUTCROP ASSOCIATION, 30 TO 6 0 PERCENT SLOPES


muname:
PLEGOMIR-HIKO PEAK-BULLUMP ASSOCIATION, 3 TO 25 PERCENT SLOPES


muname:
PROMO-PUETT COMPLEX, 10 TO 35 PERCENT SLOPES


muname:
PUETT-PLEGOMIR GRAVELLY LOAMS, 3 TO 15 PERCENT SLOPES


muname:
RAFTRIVER-DUCKREE COMPLEX, 2 TO 50 PERCENT SLOPES


muname:
RAFTRIVER-KOOSHAREM COMPLEX, 2 TO 20 PERCENT SLOPES


muname:
REEBOK-PUETT ASSOCIATION, 2 TO 35 PERCENT SLOPES


muname:
REXMONT-SHALPER-ROCK OUTCROP COMPLEX, 15 TO 40 PERCENT S LOPES


muname:
RIDD-BULLUMP COMPLEX, 3 TO 20 PERCENT SLOPES


muname:
BICKMORE-NIELSEN FAMILIES ASSOCIATION, 5 TO 45 PERCENT SLOPES


muname:
RIDGECREST-BICKMORE FAMILIES ASSOCIATION, 30 TO 60 PERCENT SLOPES


muname:
ROCK OUTCROP-AMTOFT ASSOCIATION, 35 TO 80 PERCENT SLOPES


muname:
RODROF EXTREMELY GRAVELLY LOAM,10 TO 40 PERCENT SLOPES


muname:
RUBBLE LAND-NIELSEN FAMILY COMPLEX,30 TO 60 PERCENT SLO PES


muname:
SALTAIR-PLAYAS ASSOCIATION, 0 TO 2 PERCENT SLOPES


muname:
SAXBY-ROCK OUTCROP COMPLEX, 10 TO 50 PERCENT SLOPES


muname:
SCALADE-LODAR ASSOCIATION, 3 TO 25 PERCENT SLOPES


muname:
SKUMPAH-PLAYAS COMPLEX, 1 TO 3 PERCENT SLOPES


muname:
SKUMPAH,SODIC-PLAYAS COMPLEX, 0 TO 3 PERCENT SLOPES


muname:
SKUMPAH-SKUMPAH, SODIC-SWINGLER ASSOCIATION, 1 TO 3 PERCE NT SLOPES


muname:
SKYLICK-HOODLE ASSOCIATION, 15 TO 50 PERCENT SLOPES


muname:
SMAUG VERY FINE SANDY LOAM, 0 TO 5 PERCENT SLOPES


muname:
SOLAK-ROCK OUTCROP ASSOCIATION, 15 TO 50 PERCENT SLOPES


muname:
SONLET-LODAR-RUBBLE LAND COMPLEX, 40 TO 60 PERCENT SLOPE S


muname:
STUCKY-HIKO PEAK ASSOCIATION, 8 TO 25 PERCENT SLOPES


muname:
TARNACH GRAVELLY LOAM, 6 TO 15 PERCENT SLOPES


muname:
TARNACH VERY GRAVELLY LOAM, 15 TO 45 PERCENT SLOPES


muname:
TARNACH-AMTOFT VERY GRAVELLY LOAMS, 15 TO 50 PERCENT SLOPES


muname:
BLUEHILL-COALBANK ASSOCIATION, 20 TO 60 PERCENT SLOPES


muname:
TARNACH, MOIST-TARNACH ASSOCIATION, 30 TO 70 PERCENT SLOP ES


muname:
TOSSER VERY GRAVELLY SANDY LOAM, 3 TO 15 PERCENT SLOPES


muname:
TOSSER-PLEGOMIR COMPLEX, 3 TO 15 PERCENT SLOPES


muname:
TOSSER-PUETT ASSOCIATION, 15 TO 30 PERCENT SLOPES


muname:
TOSSER-SITAR ASSOCIATION, 3 TO 15 PERCENT SLOPES


muname:
VICKING SILT LOAM, 3 TO 8 PERCENT SLOPES


muname:
VICKING-RAFTRIVER-CODQUIN COMPLEX, 2 TO 60 PERCENT SLOPE S


muname:
VICKING-RAMSHORN FAMILY ASSOCIATION, 3 TO 25 PERCENT SLO PES


muname:
FLYGARE SILT LOAM, 3 TO 20 PERCENT SLOPES


muname:
FOXOL ROCKY LOAM, 30 TO 60 PERCENT SLOPES


muname:
GORING SILT LOAM, 6 TO 30 PERCENT SLOPES


muname:
GREEN CANYON GRAVELLY LOAM, 0 TO 3 PERCENT SLOPES


muname:
GREEN CANYON GRAVELLY LOAM, 3 TO 7 PERCENT SLOPES


muname:
GREENSON LOAM, DEEP OVER CLAY, 0 TO 1 PERCENT SLOPES


muname:
GREENSON LOAM, DEEP OVER GRAVEL, 0 TO 1 PERCENT SLOPES


muname:
HOSKIN GRAVELLY LOAM, THICK SURFACE, 1 TO 6 PERCENT SLOPES


muname:
HOSKIN COBBLY LOAM, 30 TO 70 PERCENT SLOPES, ERODED


muname:
HENDRICKS SILT LOAM, 1 TO 3 PERCENT SLOPES


muname:
HENDRICKS SILT LOAM, 3 TO 6 PERCENT SLOPES


muname:
HIIBNER GRAVELLY CLAY LOAM, 3 TO 10 PERCENT SLOPES


muname:
HIIBNER GRAVELLY CLAY LOAM, 10 TO 30 PERCENT SLOPES


muname:
HIIBNER GRAVELLY CLAY LOAM, 20 TO 30 PERCENT SLOPES


muname:
HIIBNER EXTREMELY STONY CLAY LOAM, 1 TO 30 PERCENT SLOPES


muname:
HILLFIELD SILT LOAM, 20 TO 30 PERCENT SLOPES, ERODED


muname:
HILLFIELD-TIMPANOGOS SILT LOAMS, 10 TO 30 PERCENT SLOPES, ERODED


muname:
HYRUM GRAVELLY LOAM, 4 TO 8 PERCENT SLOPES


muname:
HYRUM GRAVELLY LOAM, 10 TO 25 PERCENT SLOPES


muname:
HYRUM COBBLY LOAM, 4 TO 8 PERCENT SLOPES


muname:
KIDMAN FINE SANDY LOAM, 8 TO 15 PERCENT SLOPES


muname:
KIDMAN FINE SANDY LOAM, DEEP WATER TABLE, 0 TO 2 PERCENT SLOPES


muname:
AGASSIZ VERY COBBLY SILT LOAM, 6 TO 30 PERCENT SLOPES


muname:
KIDMAN FINE SANDY LOAM, DEEP WATER TABLE, 2 TO 4 PERCENT SLOPES


muname:
KIDMAN FINE SANDY LOAM, DEEP WATER TABLE, 4 TO 8 PERCENT SLOPES


muname:
LAPLATTA SILTY CLAY LOAM, 30 TO 50 PERCENT SLOPES


muname:
LUCKY STAR SILT LOAM, 6 TO 30 PERCENT SLOPES


muname:
LUCKY STAR GRAVELLY SILT LOAM, 30 TO 60 PERCENT SLOPES


muname:
LUCKY STAR-RED SPUR COMPLEX, 6 TO 30 PERCENT SLOPES


muname:
LEWISTON FINE SANDY LOAM, STRONGLY ALKALI


muname:
MCMURDIE SILT LOAM, 0 TO 3 PERCENT SLOPES


muname:
MCMURDIE SILT LOAM, 3 TO 6 PERCENT SLOPES


muname:
MCMURDIE SILT LOAM, 6 TO 10 PERCENT SLOPES


muname:
MCMURDIE-HILLFIELD SILT LOAMS, 10 TO 30 PERCENT SLOPES, ERODED


muname:
MENDON-COLLINSTON COMPLEX, 1 TO 6 PERCENT SLOPES


muname:
MENDON-COLLINSTON COMPLEX, 6 TO 30 PERCENT SLOPES,ERODED


muname:
MUNK-BLACKROCK GRAVELLY LOAMS, 30 TO 70 PERCENT SLOPES, ERODED


muname:
NEBEKER SILT LOAM, 3 TO 6 PERCENT SLOPES


muname:
NEBEKER SILT LOAM, 6 TO 10 PERCENT SLOPES


muname:
NEBEKER SILT LOAM, 10 TO 25 PERCENT SLOPES


muname:
NIBLEY SILTY CLAY LOAM, 0 TO 3 PERCENT SLOPES


muname:
NIBLEY SILTY CLAY LOAM, 3 TO 6 PERCENT SLOPES


muname:
PARLEYS SILT LOAM, 0 TO 3 PERCENT SLOPES


muname:
PARLEYS SILT LOAM, 3 TO 6 PERCENT SLOPES


muname:
PARLEYS SILT LOAM, 6 TO 10 PERCENT SLOPES


muname:
PRESTON FINE SAND, 0 TO 10 PERCENT SLOPES


muname:
RICHMOND VERY STONY LOAM, 30 TO 70 PERCENT SLOPES,ERODED


muname:
RICKS GRAVELLY LOAM, 0 TO 3 PERCENT SLOPES


muname:
RICKS GRAVELLY LOAM, 3 TO 6 PERCENT SLOPES


muname:
RICKS GRAVELLY LOAM, 6 TO 10 PERCENT SLOPES


muname:
ST. MARYS GRAVELLY VERY FINE SANDY LOAM, 30 TO 60 PERCENT SLOPES


muname:
SCAVE SILT LOAM, 10 TO 30 PERCENT SLOPES


muname:
SCAVE COBBLY SILT LOAM, 10 TO 30 PERCENT SLOPES


muname:
SCOUT GRAVELLY LOAM, 40 TO 70 PERCENT SLOPES


muname:
SHEEP CREEK COBBLY LOAM, 30 TO 70 PERCENT SLOPES,ERODED


muname:
SMARTS SILT LOAM, 10 TO 30 PERCENT SLOPES


muname:
STEED GRAVELLY LOAM, 0 TO 3 PERCENT SLOPES


muname:
STEED GRAVELLY LOAM, 3 TO 6 PERCENT SLOPES


muname:
STEED GRAVELLY LOAM, 6 TO 10 PERCENT SLOPES


muname:
STERLING GRAVELLY LOAM, 6 TO 10 PERCENT SLOPES


muname:
STERLING GRAVELLY LOAM, 10 TO 20 PERCENT SLOPES


muname:
STERLING GRAVELLY LOAM, 20 TO 50 PERCENT SLOPES,ERODED


muname:
TIMPANOGOS SILT LOAM, 0 TO 3 PERCENT SLOPES


muname:
TIMPANOGOS SILT LOAM, 3 TO 6 PERCENT SLOPES


muname:
TIMPANOGOS SILT LOAM, 10 TO 20 PERCENT SLOPES, ERODED


muname:
TIMPANOGOS SILT LOAM, DEEP WATER TABLE, 0 TO 3 PERCENT SLOPES


muname:
TRENTON SILTY CLAY LOAM, 0 TO 2 PERCENT SLOPES


muname:
TRENTON SILTY CLAY LOAM, 2 TO 4 PERCENT SLOPES


muname:
TRENTON SILTY CLAY LOAM, 4 TO 8 PERCENT SLOPES


muname:
TRENTON SILTY CLAY LOAM, 8 TO 20 PERCENT SLOPES, ERODED


muname:
TRENTON SILTY CLAY LOAM, MODERATELY DEEP WATER TABLE, 0 TO 2 PERCENT SLOPES


muname:
WHEELON SILT LOAM, 10 TO 30 PERCENT SLOPES


muname:
WHEELON SILT LOAM, 30 TO 50 PERCENT SLOPES, ERODED


muname:
WHEELON-COLLINSTON COMPLEX, 10 TO 30 PERCENT SLOPES, ERODED


muname:
YEATES HOLLOW COBBLY SILT LOAM, 6 TO 30 PERCENT SLOPES


muname:
YEATES HOLLOW COBBLY SILT LOAM, 30 TO 70 PERCENT SLOPES


muname:
YEATES HOLLOW COBBLY SILTY CLAY LOAM, 3 TO 30 PERCENT SLOPES, ERODED


muname:
AGASSIZ VERY COBBLY SILT LOAM, 30 TO 70 PERCENT SLOPES,ERODED


muname:
AIRPORT SILT LOAM, 0 TO 3 PERCENT SLOPES


muname:
AVON SILTY CLAY LOAM, 0 TO 3 PERCENT SLOPES


muname:
AVON SILTY CLAY LOAM, 3 TO 6 PERCENT SLOPES


muname:
AVON SILTY CLAY LOAM, 6 TO 10 PERCENT SLOPES


muname:
AVON SILTY CLAY LOAM, 10 TO 20 PERCENT SLOPES


muname:
AVON-COLLINSTON COMPLEX, 6 TO 10 PERCENT SLOPES


muname:
AVON-COLLINSTON COMPLEX, 10 TO 30 PERCENT SLOPES


muname:
BICKMORE GRAVELLY SILT LOAM, 30 TO 70 PERCENT SLOPES


muname:
BATTLE CREEK SILTY CLAY LOAM, 0 TO 2 PERCENT SLOPES


muname:
BATTLE CREEK SILTY CLAY LOAM, 8 TO 15 PERCENT SLOPES


muname:
BLACKROCK GRAVELLY LOAM, 3 TO 6 PERCENT SLOPES


muname:
BLACKROCK GRAVELLY LOAM, 6 TO 10 PERCENT SLOPES


muname:
BLACKROCK GRAVELLY LOAM, 10 TO 20 PERCENT SLOPES


muname:
BLACKROCK STONY LOAM, 10 TO 20 PERCENT SLOPES


muname:
CLEGG SILT LOAM, 20 TO 30 PERCENT SLOPES


muname:
COLLINSTON LOAMY FINE SAND, 0 TO 3 PERCENT SLOPES


muname:
COLLINSTON LOAM, 10 TO 30 PERCENT SLOPES, ERODED


muname:
CROWSHAW GRAVELLY LOAM, 3 TO 6 PERCENT SLOPES


muname:
CROWSHAW GRAVELLY LOAM, 6 TO 10 PERCENT SLOPES


muname:
CROWSHAW GRAVELLY LOAM, 10 TO 20 PERCENT SLOPES


muname:
DATEMAN EXTREMELY ROCKY SILT LOAM, 40 TO 80 PERCENT SLOPES


muname:
DATWYLER COBBLY SILTY CLAY LOAM, 30 TO 60 PERCENT SLOPES


muname:
DAGOR SILT LOAM, 10 TO 20 PERCENT SLOPES


muname:
ELWOOD SILT LOAM, 30 TO 60 PERCENT SLOPES


muname:
FITZGERALD STONY LOAM, 10 TO 20 PERCENT SLOPES


muname:
STERLING GRAVELLY FINE SANDY LOAM,1 TO 3 PERCENT SLOPES


muname:
STERLING GRAVELLY FINE SANDY LOAM,3 TO 6 PERCENT SLOPES


muname:
STERLING GRAVELLY FINE SANDY LOAM,6 TO 10 PERCENT SLOPES


muname:
TAYLORSVILLE SILTY CLAY LOAM,0 TO 1 PERCENT SLOPES


muname:
TAYLORSVILLE SILTY CLAY LOAM,1 TO 3 PERCENT SLOPES


muname:
TAYLORSVILLE SILTY CLAY LOAM,EXTENDED SEASON,0 TO 1 PERCENT SLOPES


muname:
TAYLORSVILLE SILTY CLAY LOAM,EXTENDED SEASON,1 TO 3 PERCENT SLOPES


muname:
TAYLORSVILLE SILTY CLAY LOAM,EXTENDED SEASON,3 TO 6 PERCENT SLOPES,ERODED


muname:
TIMPANOGOS LOAM,WATER TABLE,0 TO 3 PERCENT SLOPES


muname:
VINEYARD FINE SANDY LOAM,0 TO 2 PERCENT SLOPES


muname:
VINEYARD FINE SANDY LOAM,MODERATELY SALINE,0 TO 2 PERCENT SLOPES


muname:
WELBY SILT LOAM,EXTENDED SEASON,0 TO 1 PERCENT SLOPES


muname:
WELBY SILT LOAM,EXTENDED SEASON,1 TO 3 PERCENT SLOPES


muname:
WELBY SILT LOAM,EXTENDED SEASON,3 TO 6 PERCENT SLOPES


muname:
WELBY SILT LOAM,EXTENDED SEASON,6 TO 10 PERCENT SLOPES


muname:
WELBY-HILLFIELD SILT LOAMS,6 TO 10 PERCENT SLOPES


muname:
WELBY-HILLFIELD SILT LOAMS,10 TO 30 PERCENT SLOPES


muname:
BINGHAM GRAVELLY LOAM,1 TO 3 PERCENT SLOPES


muname:
BINGHAM COBBLY LOAM,3 TO 6 PERCENT SLOPES


muname:
BINGHAM COBBLY LOAM,6 TO 10 PERCENT SLOPES


muname:
CHIPMAN SILTY CLAY LOAM, MODERATELY DEEP WATER TABLE


muname:
CHIPMAN SILTY CLAY LOAM, MODERATELY SALINE


muname:
CHIPMAN SILTY CLAY LOAM, STRONGLY SALINE


muname:
CLEVERLY COBBLY SANDY LOAM,6 TO 15 PERCENT SLOPES


muname:
CLEVERLY GRAVELLY FINE SANDY LOAM,1 TO 3 PERCENT SLOPES


muname:
CLEVERLY GRAVELLY FINE SANDY LOAM,3 TO 6 PERCENT SLOPES


muname:
CLEVERLY GRAVELLY FINE SANDY LOAM,6 TO 15 PERCENT SLOPES


muname:
DRY CREEK COBBLY LOAM,10 TO 30 PERCENT SLOPES


muname:
DRY CREEK EXTREMELY STONY LOAM,STONY SUBSOIL VARIANT,6 TO 30 PERCENT SLOPES


muname:
DRY CREEK COBBLY LOAM,THIN SURFACE VARIANT,30 TO 60 PERCENT SLOPES,ERODED


muname:
GAPPMAYER COBBLY LOAM,50 TO 70 PERCENT SLOPES


muname:
HENEFER-MCPHIE ASSOCIATION,5 TO 30 PERCENT SLOPES


muname:
HENEFER-MCPHIE ASSOCIATION,30 TO 60 PERCENT SLOPES


muname:
HENEFER-RAKE ASSOCIATION, 35 TO 70 PERCENT SLOPES


muname:
HILLFIELD-LAYTON COMPLEX,30 TO 60 PERCENT SLOPES


muname:
HILLFIELD-STERLING COMPLEX,20 TO 35 PERCENT SLOPES


muname:
HILLFIELD SILT LOAM,10 TO 20 PERCENT SLOPES


muname:
HILLFIELD SILT LOAM,20 TO 30 PERCENT SLOPES


muname:
HILLFIELD-WELBY SILT LOAMS,6 TO 35 PERCENT SLOPES


muname:
HOLDAWAY SILT LOAM, STRONGLY SALINE-ALKALI


muname:
KILBURN VERY GRAVELLY SANDY LOAM,30 TO 50 PERCENT SLOPES,ERODED


muname:
KILBURN STONY SANDY LOAM,3 TO 15 PERCENT SLOPES


muname:
KILBURN GRAVELLY FINE SANDY LOAM,15 TO 30 PERCENT SLOPES,ERODED


muname:
RAKE EXTREMELY STONY LOAM,20 TO 70 PERCENT SLOPES,ERODED


muname:
REDOLA GRAVELLY LOAM,3 TO 6 PERCENT SLOPES


muname:
STERLING-TERRACE ESCARPMENTS COMPLEX,30 TO 70 PERCENT SLOPES


muname:
KEIGLEY SILTY CLAY LOAM,0 TO 1 PERCENT SLOPES


muname:
KEIGLEY SILTY CLAY LOAM,1 TO 3 PERCENT SLOPES


muname:
KEIGLEY SILTY CLAY LOAM,EXTENDED SEASON,0 TO 2 PERCENT SLOPES


muname:
KIDMAN VERY FINE SANDY LOAM,0 TO 1 PERCENT SLOPES


muname:
KIDMAN VERY FINE SANDY LOAM,1 TO 3 PERCENT SLOPES


muname:
KIDMAN VERY FINE SANDY LOAM,3 TO 6 PERCENT SLOPES


muname:
KIRKHAM SILTY CLAY LOAM, MODERATELY SALINE-ALKALI


muname:
KIRKHAM SILTY CLAY LOAM, STRONGLY SALINE-ALKALI


muname:
LAKEWIN GRAVELLY FINE SANDY LOAM,1 TO 6 PERCENT SLOPES


muname:
LAKEWIN GRAVELLY FINE SANDY LOAM,6 TO 15 PERCENT SLOPES


muname:
LAKEWIN COBBLY FINE SANDY LOAM,15 TO 30 PERCENT SLOPES


muname:
LAYTON LOAMY FINE SAND, 6 TO 15 PERCENT SLOPES


muname:
LAYTON FINE SANDY LOAM,1 TO 6 PERCENT SLOPES


muname:
LAYTON FINE SANDY LOAM,SLOWLY PERMEABLE SUBSTRATUM,0 TO 1 PERCENT SLOPES


muname:
LAYTON FINE SANDY LOAM,WATER TABLE,1 TO 3 PERCENT SLOPES


muname:
MANILA SILT LOAM,10 TO 30 PERCENT SLOPES


muname:
MCMURDIE SILT LOAM,3 TO 6 PERCENT SLOPES


muname:
MCMURDIE-TAYLORSVILLE COMPLEX,6 TO 20 PERCENT SLOPES,ERODED


muname:
PAYSON-TERRACE ESCARPMENTS COMPLEX,1 TO 20 PERCENT SLOPES,ERODED


muname:
PICAYUNE COBBLY SILT LOAM, 35 TO 70 PERCENT SLOPES, ERODED


muname:
PICAYUNE COBBLY LOAM, RED VARIANT, 30 TO 60 PERCENT SLOPES


muname:
PICAYUNE-RAKE ASSOCIATION,35 TO 70 PERCENT SLOPES,ERODED


muname:
PLEASANT GROVE-TERRACE ESCARPMENTS COMPLEX,30 TO 60 PERCENT SLOPES,ERODED


muname:
PARLEYS GRAVELLY LOAM,OVERWASHED,3 TO 6 PERCENT SLOPES


muname:
PARLEYS SILTY CLAY LOAM,0 TO 3 PERCENT SLOPES


muname:
PLEASANT GROVE GRAVELLY LOAM,3 TO 6 PERCENT SLOPES


muname:
PLEASANT GROVE GRAVELLY LOAM,6 TO 10 PERCENT SLOPES


muname:
PLEASANT GROVE STONY LOAM,10 TO 25 PERCENT SLOPES,ERODED


muname:
PLEASANT VALE LOAM,0 TO 2 PERCENT SLOPES


muname:
PLEASANT VALE LOAM,EXTENDED SEASON,0 TO 2 PERCENT SLOPES


muname:
PLEASANT VALE LOAM,EXTENDED SEASON,3 TO 6 PERCENT SLOPES


muname:
PLEASANT VALE GRAVELLY LOAM,EXTENDED SEASON,1 TO 3 PERCENT SLOPE


muname:
PLEASANT VALE GRAVELLY SANDY LOAM,EXTENDED SEASON,6 TO 10 PERCENT SLOPES


muname:
PLEASANT VALE SILTY CLAY LOAM,1 TO 3 PERCENT SLOPES


muname:
PLEASANT VIEW FINE SANDY LOAM,1 TO 3 PERCENT SLOPES


muname:
PRESTON FINE SAND,1 TO 10 PERCENT SLOPES


muname:
PRESTON LOAMY FINE SAND,HIGH WATER TABLE VARIANT


muname:
Anders silt loam, 5 to 20 percent slopes


muname:
Royal very fine sandy loam, 2 to 5 percent slopes


muname:
Royal fine sandy loam, moderately shallow, 2 to 5 percent slopes


muname:
Royal loamy fine sand, 0 to 5 percent slopes, eroded


muname:
Royal loamy fine sand, loamy subsoil, 0 to 5 percent slopes, eroded


muname:
Royal loamy fine sand, moderately shallow, 0 to 5 percent slopes, eroded


muname:
Shano silt loam, 30 to 45 percent slopes


muname:
Shano silt loam, moderately shallow, 0 to 5 percent slopes


muname:
Shano silt loam, moderately shallow, 5 to 30 percent slopes


muname:
Shano very fine sandy loam, 0 to 30 percent slopes, eroded


muname:
Stanfield silt loam, 0 to 6 percent slopes


muname:
Starbuck silt loam, 0 to 15 percent slopes


muname:
Stratford silt loam, 0 to 15 percent slopes


muname:
Stratford cobbly silt loam, 0 to 15 percent slopes


muname:
Stratford very stony silt loam, 0 to 15 percent slopes


muname:
Sagemoor silt loam, 0 to 2 percent slopes


muname:
Sagemoor silt loam, 2 to 5 percent slopes


muname:
Sagemoor silt loam, 5 to 15 percent slopes


muname:
Sagemoor silt loam, compact substratum, 0 to 2 percent slopes


muname:
Sagemoor silt loam, compact substratum, 2 to 5 percent slopes


muname:
Sagemoor silt loam, compact substratum, 5 to 15 percent slopes


muname:
Sagemoor silt loam, compact substratum, 15 to 30 percent slopes


muname:
Sagemoor silt loam, compact substratum, shallow, 0 to 2 percent


muname:
Scooteney cobbly loam, 0 to 5 percent slopes


muname:
Scooteney stony loam, 0 to 15 percent slopes


muname:
Shano silt loam, 10 to 15 percent slopes


muname:
Shano silt loam, moderately shallow, 0 to 2 percent slopes


muname:
Shano silt loam, moderately shallow, 2 to 5 percent slopes


muname:
Shano silt loam, moderately shallow, 5 to 10 percent slopes


muname:
Shano silt loam, moderatley shallow, 10 to 15 percent slopes


muname:
Shano silt loam, moderately shallow, 15 to 30 percent slopes


muname:
Shano very fine sandy loam, 0 to 2 percent slopes


muname:
Shano very fine sandy loam, 2 to 5 percent slopes, eroded


muname:
Taunton fine sandy loam, 2 to 5 percent slopes


muname:
Taunton fine sandy loam, shallow, 0 to 6 percent slopes


muname:
Umapine silt loam, 0 to 2 percent slopes


muname:
Umapine loamy sand, overwash, 0 to 2 percent slopes


muname:
Wacota silt loam, 0 to 30 percent slopes, eroded


muname:
Wacota silt loam, 30 to 65 percent slopes, eroded


muname:
Walla Walla silt loam, 0 to 5 percent slopes


muname:
Walla Walla silt loam, 5 to 30 percent slopes


muname:
Walla Walla silt loam, 5 to 30 percent slopes, eroded


muname:
Walla Walla silt loam, 30 to 40 percent slopes


muname:
Walla Walla silt loam, 30 to 40 percent slopes, eroded


muname:
Walla Walla silt loam, 40 to 65 percent slopes


muname:
Walla Walla silt loam, moderately shallow, 0 to 5 percent slopes


muname:
Walla Walla silt loam, moderately shallow, 5 to 30 percent slopes


muname:
Walla Walla silt loam, moderately shallow, 30 to 40 percent slopes


muname:
Walla Walla silt loam, moderately shallow, 40 to 65 percent slopes


muname:
Walvan very fine sandy loam, 0 to 30 percent slopes


muname:
Walvan very fine sandy loam, 30 to 65 percent slopes


muname:
Warden very fine sandy loam, 0 to 5 percent slopes


muname:
Warden very fine sandy loam, 0 to 15 percent slopes, eroded


muname:
Warden very fine sandy loam, 5 to 30 percent slopes


muname:
Willis silt loam, 0 to 15 percent slopes


muname:
Willis silt loam, 0 to 15 percent slopes, eroded


muname:
Willis silt loam, shallow, 0 to 15 percent slopes


muname:
Warden very fine sandy loam, 0 to 2 percent slopes


muname:
Warden very fine sandy loam, 2 to 5 percent slopes


muname:
Warden very fine sandy loam, 5 to 10 percent slopes


muname:
Warden fine sandy loam, 0 to 2 percent slopes, eroded


muname:
Warden fine sandy loam, 2 to 5 percent slopes, eroded


muname:
Warden fine sandy loam, 5 to 10 percent slopes, eroded


muname:
Warden fine sandy loam, 10 to 15 percent slopes, eroded


muname:
Warden loamy fine sand, 0 to 5 percent slopes, eroded


muname:
Wiehl fine sandy loam, 0 to 2 percent slopes


muname:
Wiehl fine sandy loam, 2 to 5 percent slopes


muname:
Wiehl fine sandy loam, 5 to 10 percent slopes


muname:
Bagdad silt loam, 7 to 25 percent slopes


muname:
Anders cobbly silt loam, 0 to 15 percent slopes


muname:
Anders-Kuhl very stony silt loams, 0 to 15 percent slopes


muname:
Anders-Kuhl very rocky silt loams, 0 to 15 percent slopes


muname:
Anders-Kuhl extremely rocky silt loams, 0 to 15 percent slopes


muname:
Beckley coarse sandy loam, 5 to 30 percent slopes


muname:
Benge gravelly silt loam, 0 to 15 percent slopes


muname:
Benge gravelly silt loam, 15 to 30 percent slopes


muname:
Royal very fine sandy loam, 5 to 10 percent slopes


muname:
Royal very fine sandy loam, 10 to 20 percent slopes


muname:
Royal fine sandy loam, 0 to 2 percent slopes


muname:
Royal fine sandy loam, 2 to 5 percent slopes


muname:
Royal fine sandy loam, 5 to 15 percent slopes


muname:
Royal fine sandy loam, 15 to 30 percent slopes


muname:
Royal fine sandy loam, loamy subsoil, 0 to 2 percent slopes


muname:
Royal fine sandy loam, loamy subsoil, 2 to 5 percent slopes


muname:
Royal fine sandy loam, loamy subsoil, 5 to 15 percent slopes


muname:
Royal fine sandy loam, moderately shallow, 0 to 2 percent slopes


muname:
Benge very stony silt loam, 0 to 30 percent slopes


muname:
Benge very rocky silt loam, 0 to 30 percent slopes


muname:
Benge extremely rocky silt loam, 0 to 30 percent slopes


muname:
Burke silt loam, 0 to 30 percent slopes, eroded


muname:
Burke silt loam, 30 to 40 percent slopes, eroded


muname:
Burke silt loam, 10 to 15 percent slopes


muname:
Burke silt loam, 15 to 30 percent slopes


muname:
Burke silt loam, shallow, 0 to 5 percent slopes


muname:
Burke silt loam, shallow, 5 to 10 percent slopes


muname:
Burke silt loam, shallow, 15 to 30 percent slopes


muname:
Burke gravelly silt loam, 0 to 5 percent slopes


muname:
Chamber silt loam, calcareous variant, 0 to 2 percent slopes


muname:
Emdent silt loam, drained, 0 to 5 percent slopes


muname:
Emdent silt loam, moderately shallow, 0 to 8 percent slopes


muname:
Emdent very rocky silt loam, 0 to 15 percent slopes


muname:
Emdent extremely rocky silt loam, 0 to 15 percent slopes


muname:
Endicott silt loam, 0 to 5 percent slopes


muname:
Endicott silt loam, 5 to 15 percent slopes


muname:
Endicott silt loam, 5 to 15 percent slopes, eroded


muname:
Ephrata sandy loam, 0 to 15 percent slopes


muname:
Ephrata cobbly sandy loam, 0 to 15 percent slopes


muname:
Esquatzel silt loam, 0 to 2 percent slopes


muname:
Esquatzel fine sandy loam, 0 to 2 percent slopes


muname:
Ephrata sandy loam, 0 to 2 percent slopes


muname:
Ephrata sandy loam, 2 to 5 percent slopes


muname:
Ephrata sandy loam, 5 to 10 percent slopes


muname:
Ephrata sandy loam, 10 to 15 percent slopes


muname:
Ephrata gravelly sandy loam, 0 to 5 percent slopes


muname:
Ephrata very gravelly sandy loam, 0 to 5 percent slopes


muname:
Ephrata very gravelly sandy loam, 5 to 15 percent slopes


muname:
Ephrata stony sandy loam, 15 to 30 percent slopes


muname:
Ephrata loamy sand, 0 to 5 percent slopes, eroded


muname:
Farrell very fine sandy loam, 0 to 5 percent slopes


muname:
Farrell very fine sandy loam, 5 to 30 percent slopes


muname:
Farrell fine sandy loam, 0 to 30 percent slopes, eroded


muname:
Farrell fine sandy loam, 30 to 40 percent slopes, eroded


muname:
Hermiston silt loam, 0 to 2 percent slopes


muname:
Magallon silt loam, 5 to 30 percent slopes


muname:
Magallon sandy loam, 5 to 30 percent slopes, eroded


muname:
Neppel very fine sandy loam, 0 to 2 percent slopes


muname:
Neppel very fine sandy loam, 2 to 5 percent slopes


muname:
Neppel fine sandy loam, 0 to 2 percent slopes, eroded


muname:
Neppel fine sandy loam, 2 to 5 percent slopes, eroded


muname:
Prosser very fine sandy loam, 0 to 20 percent slopes


muname:
Prosser very fine sandy loam, 15 to 30 percent slopes, eroded


muname:
Prosser-Starbuck very fine sandy loams, 0 to 5 percent slopes


muname:
Prosser-Starbuck very rocky very fine sandy loams, 0 to 20 percent slopes


muname:
Prosser very fine sandy loam, 0 to 2 percent slopes


muname:
Prosser very fine sandy loam, 2 to 8 percent slopes


muname:
Prosser-Starbuck extremely rocky very fine sandy loams, 0 to 20 percent slopes


muname:
Quincy fine sand, 8 to 40 percent slopes


muname:
Quincy loamy fine sand, 0 to 10 percent slopes, eroded


muname:
Quincy fine sand, 0 to 10 percent slopes, eroded


muname:
Ritzcal silt loam, 15 to 30 percent slopes, eroded


muname:
Ritzcal silt loam, 30 to 40 percent slopes, eroded


muname:
Ritzville silt loam, 0 to 1 percent slopes


muname:
Ritzville silt loam, 1 to 5 percent slopes


muname:
Ritzville silt loam, 5 to 30 percent slopes


muname:
Ritzville silt loam, 2 to 30 percent slopes, eroded


muname:
Ritzville silt loam, 30 to 40 percent slopes


muname:
Ritzville silt loam, 30 to 40 percent slopes, eroded


muname:
Ritzville silt loam, 40 to 65 percent slopes


muname:
Ritzville silt loam, moderately shallow, 0 to 5 percent slopes


muname:
Ritzville silt loam, moderately shallow, 0 to 15 percent slopes, eroded


muname:
Ritzville silt loam, moderately shallow, 5 to 30 percent slopes


muname:
Ritzville silt loam, moderately shallow, 30 to 40 percent slopes


muname:
Ritzville silt loam, moderately shallow, 40 to 65 percent slopes


muname:
Roloff silt loam, 0 to 15 percent slopes


muname:
Roloff-Starbuck stony silt loams, 10 to 30 percent slopes


muname:
Roloff-Starbuck very rocky silt loams, 10 to 30 percent slopes


muname:
Roloff-Starbuck extremely rocky silt loams, 0 to 15 percent slopes


muname:
Royal very fine sandy loam, 0 to 15 percent slopes


muname:
Royal very fine sandy loam, 0 to 2 percent slopes


muname:
Scooteney stony silt loam, 0 to 30 percent slopes


muname:
Prosser silt loam, 0 to 2 percent slopes


muname:
Prosser silt loam, 2 to 5 percent slopes


muname:
Prosser silt loam, 5 to 15 percent slopes


muname:
Prosser silt loam, 0 to 30 percent slopes


muname:
Prosser very fine sandy loam, 0 to 15 percent slopes, eroded


muname:
Quincy loamy sand, 0 to 2 percent slopes


muname:
Quincy loamy sand, 2 to 15 percent slopes


muname:
Quincy loamy sand, moderately shallow, 0 to 30 percent slopes


muname:
Ritzville silt loam, 0 to 5 percent slopes


muname:
Ritzville silt loam, 15 to 30 percent slopes, severely eroded


muname:
Ritzville silt loam, 30 to 65 percent slopes


muname:
Ritzville very fine sandy loam, 0 to 15 percent slopes, eroded


muname:
Scooteney silt loam, 0 to 2 percent slopes


muname:
Scooteney silt loam, 0 to 5 percent slopes


muname:
Scootney silt loam, 2 to 5 percent slopes


muname:
Scooteney silt loam, 5 to 8 percent slopes


muname:
Scooteney silt loam, gravelly subsoil, 0 to 2 percent slopes


muname:
Scooteney silt loam, gravelly subsoil, 2 to 5 percent slopes


muname:
Scooteney silt loam, gravelly subsoil, 5 to 15 percent slopes


muname:
Scooteney gravelly silt loam, 2 to 5 percent slopes


muname:
Shano silt loam, 15 to 30 percent slopes, severely eroded


muname:
Shano silt loam, 30 to 65 percent slopes


muname:
Shano silt loam, deep, 2 to 5 percent slopes


muname:
Shano silt loam, deep, 5 to 8 percent slopes


muname:
Shano very fine sandy loam, 0 to 15 percent slopes, eroded


muname:
Shano very fine sandy loam, 15 to 30 percent slopes, eroded


muname:
Shano very fine sandy loam, deep, 2 to 8 percent slopes, eroded


muname:
Starbuck silt loam, 0 to 5 percent slopes


muname:
Starbuck silt loam, 0 to 8 percent slopes


muname:
Starbuck silt loam, 5 to 8 percent slopes


muname:
Starbuck rocky silt loam, 5 to 45 percent slopes


muname:
Starbuck stony silt loam, 0 to 15 percent slopes


muname:
Umapine silt loam, 0 to 5 percent slopes


muname:
Umapine silt loam, drained, 0 to 2 percent slopes


muname:
Walla Walla silt loam, 5 to 15 percent slopes


muname:
Walla Walla silt loam, 15 to 30 percent slopes, severely eroded


muname:
Walla Walla silt loam, 30 to 65 percent slopes


muname:
Warden silt loam, 8 to 15 percent slopes


muname:
Warden silt loam, 15 to 30 percent slopes, severely eroded


muname:
Warden silt loam, 30 to 65 percent slopes


muname:
Warden very fine sandy loam, 0 to 2 percent slopes, eroded


muname:
Warden very fine sandy loam, 2 to 8 percent slopes, eroded


muname:
Warden very fine sandy loam, 0 to 15 percent slopes


muname:
Warden very fine sandy loam, 8 to 15 percent slopes, eroded


muname:
Warden very fine sandy loam, 15 to 30 percent slopes, eroded


muname:
Willis silt loam, 15 to 30 percent slopes, severely eroded


muname:
Willis silt loam, 30 to 65 percent slopes


muname:
Burbank loamy fine sand, 0 to 2 percent slopes


muname:
Burbank loamy fine sand, 0 to 15 percent slopes


muname:
Burbank loamy fine sand, 2 to 15 percent slopes


muname:
Burbank loamy fine sand, basalt substratum, 0 to 30 percent slopes


muname:
Burbank rocky loamy fine sand, basalt substratum, 0 to 30 percent slopes


muname:
Burbank loamy fine sand, gravelly substratum, 0 to 2 percent slopes


muname:
Burbank loamy fine sand, gravelly substratum, 2 to 15 percent slopes


muname:
Burbank rocky loamy fine sand, 30 to 65 percent slopes


muname:
Burke silt loam, 15 to 30 percent slopes, severely eroded


muname:
Burke silt loam, 30 to 65 percent slopes


muname:
Burke silt loam, shallow, 5 to 8 percent slopes


muname:
Burke very fine sandy loam, 0 to 2 percent slopes, eroded


muname:
Burke very fine sandy loam, 2 to 5 percent slopes, eroded


muname:
Burke very fine sandy laom, 5 to 8 percent slopes, eroded


muname:
Burke very fine sandy loam, 0 to 15 percent slopes, eroded


muname:
Burke very fine sandy loam, shallow, 0 to 8 percent slopes, eroded


muname:
Ellisforde silt loam, 0 to 5 percent slopes


muname:
Ellisforde silt loam, 15 to 30 percent slopes, severely eroded


muname:
Endicott variant silt loam, 0 to 40 percent slopes


muname:
Esquatzel fine sandy loam, 0 to 5 percent slopes


muname:
Esquatzel silt loam, 0 to 5 percent slopes


muname:
Esquatzel silt loam, 2 to 5 percent slopes


muname:
Finley fine sandy loam, 0 to 2 percent slopes


muname:
Finley fine sandy loam, 2 to 5 percent slopes


muname:
Finley fine sandy loam, 0 to 15 percent slopes


muname:
Finley fine sandy loam, 5 to 15 percent slopes


muname:
Finley stony fine sandy loam, 0 to 30 percent slopes


muname:
Finley gravelly fine sandy loam, 2 to 5 percent slopes


muname:
Finley fine sandy loam, moderately deep, 0 to 2 percent slopes


muname:
Finley fine sandy loam, moderately deep, 2 to 5 percent slopes


muname:
Hezel loamy fine sand, 0 to 2 percent slopes


muname:
Hezel loamy fine sand, 2 to 15 percent slopes


muname:
Hezel loamy fine sand, 0 to 30 percent slopes


muname:
Kennewick silt loam, 0 to 2 percent slopes


muname:
Kennewick silt loam, 2 to 5 percent slopes


muname:
Kennewick silt loam, 5 to 8 percent slopes


muname:
Kennewick silt loam, 8 to 15 percent slopes


muname:
Kennewick silt loam, 15 to 30 percent slopes, severely eroded


muname:
Kiona very stony silt loam, 0 to 30 percent slopes


muname:
Kiona very stony silt loam, 30 to 65 percent slopes


muname:
Koehler loamy fine sand, 0 to 8 percent slopes


muname:
Lickskillet very stony silt loam, 0 to 30 percent slopes


muname:
Lickskillet very stony silt loam, 30 to 65 percent slopes


muname:
Pasco fine sandy loam, 0 to 2 percent slopes


muname:
Aarup fine sandy loam, 0 to 8 percent slopes


muname:
Beca-Dougville-Slickear complex, 15 to 40 percent slopes


muname:
Royal loamy fine sand, 0 to 10 percent slopes


muname:
Benwy-Selah-Alstown complex, 15 to 30 percent slopes


muname:
Ebadlow-Spofford-Badgermont complex, 3 to 8 percent slopes


muname:
Ebadlow-Spofford-Badgermont complex, 8 to 15 percent slopes


muname:
Logy very stony sandy loam, 3 to 15 percent slopes


muname:
Van Nostern-Camaspatch complex, 3 to 8 percent slopes


muname:
Van Nostern-Camaspatch complex, 8 to 15 percent slopes


muname:
Van Nostern-Camaspatch complex, 15 to 30 percent slopes


muname:
Sanbee loamy fine sand, 0 to 15 percent slopes


muname:
Sagehill very fine sandy loam, 10 to 15 percent slopes


muname:
Logy cobbly sandy loam, 3 to 15 percent slopes


muname:
Ebadlow silt loam, 3 to 8 percent slopes


muname:
Malaga gravelly fine sandy loam, 0 to 8 percent slopes


muname:
Malaga cobbly fine sandy loam, 0 to 8 percent slopes


muname:
Pogue fine sandy loam, 0 to 3 percent slopes


muname:
Schawana complex, 0 to 15 percent slopes


muname:
Cashmont gravelly sandy loam, 3 to 8 percent slopes


muname:
Cashmont gravelly sandy loam, 8 to 15 percent slopes


muname:
Silico-Sevar-Dutchenry complex, 0 to 8 percent slopes


muname:
Silico-Sevar-Dutchenry complex, 8 to 15 percent slopes


muname:
Silico-Sevar-Dutchenry complex, 15 to 30 percent slopes


muname:
Logy cobbly sandy loam, 15 to 30 percent slopes


muname:
Terlan-Selah complex, 0 to 8 percent slopes


muname:
Starbuck-Bakeoven-Rock outcrop complex, 0 to 45 percent slopes


muname:
Pogue fine sandy loam, 3 to 8 percent slopes


muname:
Pogue fine sandy loam, 8 to 15 percent slopes


muname:
Strat cobbly loam, 0 to 15 percent slopes


muname:
Pogue gravelly fine sandy loam, 8 to 15 percent slopes


muname:
Strat stony loam, 0 to 25 percent slopes


muname:
Pogue gravelly fine sandy loam, 15 to 25 percent slopes


muname:
Winblow fine sandy loam, 0 to 8 percent slopes


muname:
Winblow fine sandy loam, 8 to 15 percent slopes


muname:
Pogue cobbly fine sandy loam, 0 to 15 percent slopes


muname:
Pogue extremely stony fine sandy loam, 3 to 25 percent slopes


muname:
Taunton fine sandy loam, 10 to 15 percent slopes


muname:
Broadax silt loam, cemented substratum, 3 to 8 percent slopes


muname:
Broadax silt loam, cemented substratum, 8 to 15 percent slopes


muname:
Van Nostern-Argabak-Camaspatch complex, 3 to 30 percent slopes


muname:
Taunton silt loam, 5 to 10 percent slopes


muname:
Pogue cobbly fine sandy loam, 30 to 65 percent slopes


muname:
Taunton silt loam, 15 to 25 percent slopes


muname:
Pogue bouldery fine sandy loam, 3 to 8 percent slopes


muname:
Taunton-Finley complex, 0 to 10 percent slopes


muname:
Deercut fine sandy loam, 0 to 8 percent slopes


muname:
Quincy fine sand, 15 to 30 percent slopes


muname:
Magallon fine sandy loam, 3 to 8 percent slopes


muname:
Magallon fine sandy loam, 8 to 15 percent slopes


muname:
Warden very fine sandy loam, 3 to 8 percent slopes


muname:
Whiteye fine sandy loam, 0 to 8 percent slopes


muname:
Silico fine sandy loam, 0 to 8 percent slopes


muname:
Peshastin fine sandy loam, compacted substratum, 3 to 8 percent slopes


muname:
Peshastin fine sandy loam, compacted substratum, 8 to 15 percent slopes


muname:
Sevar fine sandy loam, 3 to 8 percent slopes


muname:
Cashmont sandy loam, 0 to 3 percent slopes


muname:
Willis silt loam, 8 to 15 percent slopes


muname:
Toler-Horseflat complex, 0 to 3 percent slopes


muname:
Zen-Lickskillet-Ralls complex, 5 to 45 percent slopes


muname:
Zen-Horseflat-Benwy complex, 3 to 8 percent slopes


muname:
Zen-Horseflat-Ralls complex, 8 to 15 percent slopes


muname:
Zen-Horseflat-Ralls complex, 15 to 30 percent slopes


muname:
Zen-Horseflat complex, 3 to 8 percent slopes


muname:
Zen-Horseflat complex, 8 to 15 percent slopes


muname:
Toler-Horseflat complex, 15 to 30 percent slopes


muname:
Sanbee fine sandy loam, 0 to 8 percent slopes


muname:
Touhey-Argabak complex, 0 to 15 percent slopes


muname:
Siweeka-Argabak complex, 0 to 15 percent slopes


muname:
Touhey-Argabak-Rock outcrop complex, 15 to 30 percent slopes


muname:
Siweeka-Argabak-Rock outcrop complex, 15 to 30 percent slopes


muname:
Touhey-Argabak-Rock outcrop complex, 30 to 65 percent slopes


muname:
Siweeka-Argabak-Rock outcrop complex, 30 to 65 percent slopes


muname:
Cashmont sandy loam, 8 to 15 percent slopes


muname:
Aeneas fine sandy loam, 3 to 8 percent slopes


muname:
Cashmont sandy loam, 3 to 8 percent slopes


muname:
DelRio fine sandy loam, 0 to 8 percent slopes


muname:
Nemire fine sandy loam, 3 to 8 percent slopes


muname:
DelRio fine sandy loam, 8 to 15 percent slopes


muname:
Cashmere fine sandy loam, 0 to 3 percent slopes


muname:
Cashmere fine sandy loam, 3 to 8 percent slopes


muname:
Nemire fine sandy loam, 0 to 3 percent slopes


muname:
Kester fine sandy loam, 0 to 5 percent slopes


muname:
Dougville fine sandy loam, 0 to 8 percent slopes


muname:
Dougville fine sandy loam, 8 to 15 percent slopes


muname:
Dougville fine sandy loam, 15 to 30 percent slopes


muname:
Simsfield fine sandy loam, 0 to 3 percent slopes


muname:
Simsfield fine sandy loam, 3 to 8 percent slopes


muname:
Simsfield fine sandy loam, 8 to 15 percent slopes


muname:
Durixerolls-Ellisforde-Elvedere complex, 15 to 30 percent slopes


muname:
Aarup fine sandy loam, 8 to 15 percent slopes


muname:
Durixerolls-Ellisforde-Elvedere complex, 8 to 15 percent slopes


muname:
Sanbee sandy loam, 0 to 8 percent slopes


muname:
Cashmere fine sandy loam, 8 to 15 percent slopes


muname:
Peshastin stony fine sandy loam, 8 to 15 percent slopes


muname:
Sanbee-Quincy complex, 0 to 3 percent slopes


muname:
Siweeka complex, 15 to 30 percent slopes


muname:
Durixerolls-Halaquepts complex, cool, nearly level


muname:
Zeemal fine sandy loam, 0 to 3 percent slopes


muname:
Zeemal fine sandy loam, 3 to 8 percent slopes


muname:
Leahy-Elvedere-Halaquepts complex, 0 to 3 percent slopes


muname:
Deercut-Aarup-Whiteye complex, 3 to 8 percent slopes


muname:
Lickskillet very cobbly loam, 0 to 15 percent slopes


muname:
Ginnis fine sandy loam, 3 to 15 percent slopes


muname:
Ginnis fine sandy loam, 15 to 30 percent slopes


muname:
Deercut-Aarup-Whiteye complex, 0 to 3 percent slopes


muname:
Deercut-Aarup-Whiteye complex, 8 to 15 percent slopes


muname:
Quincy-Ellisforde-Cashmere complex, 3 to 15 percent slopes


muname:
Quincy loamy fine sand, 0 to 15 percent slopes


muname:
Quincy fine sand, high precipitation, 3 to 15 percent slopes


muname:
Ewall loamy fine sand, 3 to 15 percent slopes


muname:
Skaha-Quincy complex, 3 to 15 percent slopes


muname:
Ewall-Alecanyon complex, 3 to 15 percent slopes


muname:
Skaha cobbly loamy sand, 0 to 8 percent slopes


muname:
Strat very cobbly sandy loam, 0 to 10 percent slopes


muname:
Timentwa fine sandy loam, 0 to 8 percent slopes


muname:
Tagear fine sandy loam, 0 to 8 percent slopes


muname:
Tagear fine sandy loam, 8 to 15 percent slopes


muname:
Timentwa fine sandy loam, 8 to 15 percent slopes


muname:
Tagear fine sandy loam, 15 to 30 percent slopes


muname:
Timentwa fine sandy loam, 15 to 30 percent slopes


muname:
Touhey-Stubblefield complex, extremely bouldery, 3 to 15 percent slopes


muname:
Siweeka-Brazlan complex, extremely bouldery, 3 to 15 percent slopes


muname:
Taunton-Scoon complex, 3 to 8 percent slopes


muname:
Taunton-Scoon complex, 8 to 15 percent slopes


muname:
Skaha very cobbly loamy sand, 30 to 65 percent slopes


muname:
Alecanyon very cobbly loamy sand, 30 to 65 percent slopes, eroded


muname:
Timmerman coarse sandy loam, 0 to 3 percent slopes


muname:
Timmerman coarse sandy loam, 3 to 8 percent slopes


muname:
Timmerman coarse sandy loam, 8 to 15 percent slopes


muname:
Wellsdam-Couleedam-Rock outcrop complex, 3 to 30 percent slopes


muname:
Wellsdam-Couleedam-Rock outcrop complex, 30 to 60 percent slopes


muname:
Elvedere silt loam, 0 to 3 percent slopes


muname:
Elvedere silt loam, 3 to 8 percent slopes


muname:
Elvedere-Leahy complex, 0 to 8 percent slopes


muname:
Ellisforde-Halaquepts complex, 0 to 3 percent slopes


muname:
Ginnis-Swakane-Rock outcrop complex, 30 to 70 percent slopes


muname:
Dougville fine sandy loam, cemented substratum, 0 to 8 percent slopes


muname:
Dougville fine sandy loam, cemented substratum, 8 to 15 percent slopes


muname:
Dougville fine sandy loam, cemented substratum, 15 to 30 percent slopes


muname:
Rock outcrop-Ginnis-Swakane complex, 30 to 70 percent slopes


muname:
Norax-Dutchenry-Dougville complex, 3 to 8 percent slopes


muname:
Norax-Dutchenry-Dougville complex, 8 to 15 percent slopes


muname:
Norax-Dutchenry-Dougville complex, 15 to 30 percent slopes


muname:
Durixerolls-Ellisforde-Elvedere complex, 30 to 45 percent slopes


muname:
Chelan fine sandy loam, gravelly substratum, 0 to 8 percent slopes


muname:
Chelan fine sandy loam, gravelly substratum, 8 to 15 percent slopes


muname:
Chelan fine sandy loam, gravelly substratum, 15 to 30 percent slopes


muname:
Chelan fine sandy loam, bedrock substratum, 15 to 30 percent slopes


muname:
Van Nostern silt loam, 3 to 8 percent slopes


muname:
Van Nostern silt loam, 8 to 15 percent slopes


muname:
Van Nostern silt loam, 15 to 30 percent slopes


muname:
Wellsdam fine sandy loam, 30 to 65 percent slopes


muname:
Wellsdam fine sandy loam, 3 to 8 percent slopes


muname:
Wellsdam fine sandy loam, 8 to 15 percent slopes


muname:
Wellsdam fine sandy loam, 15 to 30 percent slopes


muname:
Wellsdam-Peshastin complex, 3 to 8 percent slopes


muname:
Wellsdam-Peshastin complex, 8 to 15 percent slopes


muname:
Wellsdam-Peshastin complex, 15 to 30 percent slopes


muname:
Chelan fine sandy loam, 0 to 8 percent slopes


muname:
Chelan fine sandy loam, 8 to 15 percent slopes


muname:
Chelan fine sandy loam, 15 to 30 percent slopes


muname:
Tubspring fine sandy loam, 0 to 8 percent slopes


muname:
Cachebutte sandy loam, 0 to 8 percent slopes


muname:
Tubspring fine sandy loam, 8 to 15 percent slopes


muname:
Stratford silt loam, 0 to 3 percent slopes


muname:
Stratford silt loam, 3 to 8 percent slopes


muname:
Stratford silt loam, 8 to 15 percent slopes


muname:
Strat-Tubspring complex, 0 to 8 percent slopes


muname:
Alecanyon-Cachebutte complex, 0 to 8 percent slopes


muname:
Tubspring-DelRio-Strat complex, 0 to 8 percent slopes


muname:
Cachebutte-Nemire-Alecanyon complex, 0 to 8 percent slopes


muname:
Jordy fine sandy loam, 0 to 8 percent slopes


muname:
Jordy fine sandy loam, 8 to 15 percent slopes


muname:
Jordy fine sandy loam, 15 to 30 percent slopes


muname:
Jordy-Argabak complex, 3 to 8 percent slopes


muname:
Jordy-Argabak complex, 8 to 15 percent slopes


muname:
Jordy-Argabak complex, 15 to 30 percent slopes


muname:
Beca fine sandy loam, 8 to 15 percent slopes


muname:
Beca fine sandy loam, 15 to 30 percent slopes


muname:
Alstown silt loam, 0 to 8 percent slopes


muname:
Alstown silt loam, 8 to 15 percent slopes


muname:
Alsash fine sandy loam, 15 to 30 percent slopes


muname:
Beca fine sandy loam, 3 to 8 percent slopes


muname:
Alstown-Cheviot complex, 30 to 65 percent slopes


muname:
Alstown-Renslow complex, 0 to 8 percent slopes


muname:
Alstown-Renslow complex, 8 to 15 percent slopes


muname:
Alsash-Slusser complex, 8 to 15 percent slopes


muname:
Benwy-Alstown complex, 0 to 8 percent slopes


muname:
Benwy-Alstown complex, 8 to 15 percent slopes


muname:
Alsash-Slusser complex, 0 to 8 percent slopes


muname:
Supplee very fine sandy loam, 3 to 8 percent slopes


muname:
Supplee very fine sandy loam, 8 to 15 percent slopes


muname:
Quincy-Ellisforde-Cashmere complex, 30 to 60 percent slopes


muname:
Skaha very cobbly loamy sand, 0 to 15 percent slopes


muname:
Tubspring fine sandy loam, thin solum, 0 to 3 percent slopes


muname:
Strat very cobbly sandy loam, 10 to 30 percent slopes


muname:
Alecanyon very cobbly fine sandy loam, 3 to 30 percent slopes


muname:
Strat-Tubspring complex, 8 to 30 percent slopes


muname:
Alecanyon-Cachebutte complex, 8 to 30 percent slopes


muname:
Sprauer fine sandy loam, 0 to 8 percent slopes


muname:
Sprauer fine sandy loam, 8 to 30 percent slopes


muname:
Strat very stony silt loam, 0 to 8 percent slopes


muname:
Strat very cobbly sandy loam, 30 to 65 percent slopes


muname:
Toler-Argabak-Horseflat complex, 0 to 20 percent slopes


muname:
Slusser fine sandy loam, cemented substratum, 0 to 8 percent slopes


muname:
Slusser fine sandy loam, cemented substratum, 8 to 30 percent slopes


muname:
Slusser fine sandy loam, 0 to 8 percent slopes


muname:
Slusser fine sandy loam, 8 to 15 percent slopes


muname:
Achelake fine sandy loam, 0 to 3 percent slopes


muname:
Farmer fine sandy loam, 0 to 8 percent slopes


muname:
Farmer fine sandy loam, 8 to 15 percent slopes


muname:
Farmer fine sandy loam, cemented substratum, 3 to 8 percent slopes


muname:
Farmer fine sandy loam, cemented substratum, 8 to 15 percent slopes


muname:
Farmer fine sandy loam, 15 to 30 percent slopes


muname:
Brays fine sandy loam, 3 to 15 percent slopes


muname:
Brays-Entiat complex, 15 to 30 percent slopes


muname:
Brays-Entiat-Rock outcrop complex, 30 to 65 percent slopes


muname:
Touhey-Stubblefield complex, 0 to 8 percent slopes


muname:
Siweeka-Brazlan complex, 0 to 8 percent slopes


muname:
Touhey-Stubblefield complex, 8 to 15 percent slopes


muname:
Siweeka-Brazlan complex, 8 to 15 percent slopes


muname:
Touhey-Stubblefield complex, 15 to 30 percent slopes


muname:
Siweeka-Brazlan complex, 15 to 30 percent slopes


muname:
Simsfield-Zeemal complex, 0 to 8 percent slopes


muname:
Simsfield-Zeemal complex, 8 to 30 percent slopes


muname:
Dutchenry fine sandy loam, 0 to 8 percent slopes


muname:
Cashmere fine sandy loam, cemented substratum, 0 to 3 percent slopes


muname:
Cashmere fine sandy loam, cemented substratum, 3 to 8 percent slopes


muname:
Cashmere fine sandy loam, cemented substratum, 8 to 15 percent slopes


muname:
Cashmere-Willis complex, 15 to 30 percent slopes


muname:
Dougville-Farmer complex, 8 to 15 percent slopes


muname:
Dougville-Farmer-Dutchenry complex, 15 to 30 percent slopes


muname:
Renslow-Alstown-Kester complex, 3 to 8 percent slopes


muname:
Renslow-Alstown-Kester complex, 8 to 15 percent slopes


muname:
Renslow-Alstown-Kester complex, 15 to 30 percent slopes


muname:
Slusser-Alsash-Nemire complex, 3 to 8 percent slopes


muname:
Slusser-Alsash-Nemire complex, 8 to 15 percent slopes


muname:
Slickear fine sandy loam, 0 to 8 percent slopes


muname:
Slickear fine sandy loam, 8 to 15 percent slopes


muname:
McCue-Broadax complex, 15 to 30 percent slopes


muname:
Cashmere-Willis complex, 30 to 45 percent slopes


muname:
Heytou-Stubblefield complex, 3 to 15 percent slopes


muname:
Dezellem-Brazlan complex, 3 to 15 percent slopes


muname:
Dezellem-Stubblefield complex, 20 to 45 percent slopes


muname:
Heytou-Stubblefield complex, 15 to 30 percent slopes


muname:
Dezellem-Brazlan complex, 15 to 30 percent slopes


muname:
Heytou-Stubblefield complex, 30 to 45 percent slopes


muname:
Dezellem-Brazlan complex, 30 to 45 percent slopes


muname:
Beca-Camaspatch complex, 15 to 30 percent slopes


muname:
Renslow silt loam, 15 to 30 percent north slopes


muname:
Toler fine sandy loam, 0 to 8 percent slopes


muname:
Toler fine sandy loam, 8 to 15 percent slopes


muname:
Toler fine sandy loam, 15 to 30 percent slopes


muname:
Ritzville silt loam, 3 to 8 percent slopes


muname:
Ritzville silt loam, 15 to 30 percent north slopes


muname:
Ritzville silt loam, cemented substratum, 30 to 65 percent slopes


muname:
Ritzville silt loam, cemented substratum, 0 to 8 percent slopes


muname:
Ritzville silt loam, cemented substratum, 8 to 15 percent slopes


muname:
Ritzville silt loam, cemented substratum, 15 to 30 percent slopes


muname:
McCue-Broadax-Mondovi complex, 0 to 8 percent slopes


muname:
McCue-Broadax-Mondovi complex, 3 to 15 percent slopes


muname:
Bagdad silt loam, cemented substratum, 0 to 8 percent slopes


muname:
Bagdad silt loam, cemented substratum, 8 to 15 percent slopes


muname:
Titchenal silt loam, 3 to 8 percent slopes


muname:
Titchenal silt loam, 8 to 15 percent slopes


muname:
Broadax-Titchenal complex, 3 to 15 percent slopes


muname:
Morrow silt loam, 8 to 15 percent slopes


muname:
Morrow-Argabak complex, 3 to 8 percent slopes


muname:
Morrow-Argabak complex, 8 to 15 percent slopes


muname:
Morrow-Argabak-Badge complex, 15 to 30 percent slopes


muname:
Argabak-Morrow complex, 0 to 30 percent slopes


muname:
Broadax-Morrow-Spofford complex, 3 to 8 percent slopes


muname:
Broadax-Morrow-Spofford complex, 8 to 15 percent slopes


muname:
Lorena silt loam, 3 to 15 percent slopes


muname:
Lorena silt loam, 15 to 30 percent slopes


muname:
Lorena-Broadax complex, 3 to 15 percent slopes


muname:
Lorena-Shinn complex, 3 to 30 percent slopes


muname:
Shinn-Lorena complex, 30 to 65 percent slopes


muname:
Renshigh-Alstown-Renslow complex, 3 to 15 percent slopes


muname:
Renshigh-Alstown-Renslow complex, 15 to 30 percent slopes


muname:
Renslow-Achelake-Willis complex, 8 to 15 percent slopes


muname:
Renslow-Achelake-Willis complex, 15 to 30 percent slopes


muname:
Ellisforde very fine sandy loam, 0 to 8 percent slopes


muname:
Ellisforde fine sandy loam, 30 to 60 percent slopes


muname:
Simsfield-Ellisforde-DelRio complex, 0 to 15 percent slopes


muname:
Conconully-Swakane-Rock outcrop complex, 0 to 15 percent slopes


muname:
Conconully-Swakane-Rock outcrop complex, 15 to 30 percent slopes


muname:
Conconully-Swakane-Rock outcrop complex, 30 to 60 percent slopes


muname:
Touhey fine sandy loam, low elevation, 3 to 8 percent slopes


muname:
Touhey fine sandy loam, low elevation, 8 to 15 percent slopes


muname:
Touhey fine sandy loam, low elevation, 15 to 30 percent slopes


muname:
Conconully-Wagberg complex, 3 to 8 percent slopes


muname:
Conconully-Wagberg complex, 8 to 15 percent slopes


muname:
Conconully-Wagberg complex, 15 to 30 percent slopes


muname:
Conconully-Wagberg complex, 30 to 65 percent slopes


muname:
Conconully complex, 0 to 8 percent slopes


muname:
Conconully complex, 8 to 15 percent slopes


muname:
Conconully complex, 15 to 30 percent slopes


muname:
Willock fine sandy loam, 0 to 8 percent slopes


muname:
Willock fine sandy loam, 8 to 15 percent slopes


muname:
Willock-Conconully complex, 3 to 8 percent slopes


muname:
Willock-Conconully complex, 8 to 15 percent slopes


muname:
Willock-Conconully complex, 15 to 30 percent slopes


muname:
Nemire fine sandy loam, sandy substratum, 0 to 3 percent slopes


muname:
Nespelem-Nemire complex, 0 to 8 percent slopes


muname:
Nespelem-Nemire complex, 8 to 15 percent slopes


muname:
Timentwa-Siweeka-Dezellem complex, 30 to 60 percent slopes


muname:
Timentwa-Siweeka-Brazlan complex, 0 to 15 percent slopes


muname:
Timentwa-Siweeka complex, 3 to 8 percent slopes


muname:
Timentwa-Siweeka complex, 8 to 15 percent slopes


muname:
Timentwa-Siweeka complex, 15 to 30 percent slopes


muname:
Watco-Dezellem-Timentwa complex, 3 to 35 percent slopes


muname:
Stubblefield stony loam, 45 to 70 percent slopes


muname:
Timentwa-Lickskillet-Argabak complex, warm, 0 to 15 percent slopes


muname:
Touhey-Lickskillet-Argabak complex, 0 to 15 percent slopes


muname:
Siweeka-Lickskillet-Argabak complex, 0 to 20 percent slopes


muname:
Argabak-Timentwa-Rock outcrop complex, warm, 0 to 15 percent slopes


muname:
Timentwa-Lickskillet-Argabak complex, 0 to 15 percent slopes


muname:
Siweeka-Brazlan-Argabak complex, 0 to 20 percent slopes


muname:
Argabak-Tagear-Rock outcrop complex, 0 to 15 percent slopes


muname:
Argabak-Timentwa-Rock outcrop complex, 0 to 15 percent slopes


muname:
Pateros-Rock outcrop complex, 25 to 70 percent slopes


muname:
Willock complex, 15 to 30 percent slopes


muname:
Willock complex, 30 to 60 percent slopes


muname:
Willock-Watco complex, 15 to 30 percent slopes


muname:
Willock-Watco complex, 30 to 60 percent slopes


muname:
Watco fine sandy loam, 30 to 60 percent slopes


muname:
Ellisforde-DelRio-Nyssaton complex, 30 to 65 percent slopes


muname:
Argabak-Winblow-Rock outcrop complex, 0 to 20 percent slopes


muname:
Winblow-Argabak-Horseflat complex, 0 to 20 percent slopes


muname:
Siweeka-Timentwa-Stubblefield complex, 15 to 40 percent slopes


muname:
Ellisforde-Nyssaton-DelRio complex, 15 to 30 percent slopes


muname:
Haploxerolls-Aquolls-Halaquepts complex, nearly level to gently sloping


muname:
Durixerolls-Halaquepts complex, cool, nearly level to rolling


muname:
Durixerolls-Halaquepts complex, nearly level to rolling


muname:
Strat-Tubspring-Nemire complex, 0 to 30 percent slopes


muname:
Strat-Tubspring-Skaha complex, 0 to 15 percent slopes


muname:
Cachebutte-Alecanyon-Haploxerolls complex, 0 to 30 percent slopes


muname:
Strat-Tubspring-DelRio complex, 0 to 30 percent slopes


muname:
Alecanyon-Cachebutte-Nemire complex, 0 to 30 percent slopes


muname:
Argabak-Nemire-Siweeka complex, 0 to 30 percent slopes


muname:
Argabak-Haploxerolls-Siweeka complex, 0 to 30 percent slopes


muname:
Siweeka-Stubblefield-Timentwa complex, 0 to 15 percent slopes


muname:
Touhey-Stubblefield-Tagear complex, 0 to 15 percent slopes


muname:
Siweeka-Timentwa-Dezellem complex, 0 to 15 percent slopes


muname:
Kiakus-Shinn-Lorena complex, 30 to 60 percent slopes


muname:
Heytou-Timentwa-Strat complex, 20 to 70 percent slopes


muname:
Leidl-Stemilt complex, 3 to 15 percent slopes


muname:
Kiakus-Shinn-Lorena complex, 3 to 30 percent slopes


muname:
Leidl-Stemilt complex, 15 to 30 percent slopes


muname:
Cordy-Stemilt complex, 3 to 30 percent slopes


muname:
Stemilt-Cordy complex, 30 to 60 percent slopes


muname:
Dezellem-Timentwa-Rock outcrop complex, warm, 20 to 70 percent slopes


muname:
Dezellem-Timentwa-Rock outcrop complex, 20 to 70 percent slopes


muname:
Heytou-Stubblefield-Rock outcrop complex, 20 to 50 percent slopes


muname:
Dezellem-Brazlan-Rock outcrop complex, 20 to 50 percent slopes


muname:
Quincy-Sanbee-DelRio complex, 0 to 20 percent slopes


muname:
Quincy-DelRio-Sanbee complex, 20 to 60 percent slopes


muname:
Heytou-Stubblefield-Siweeka complex, 0 to 20 percent slopes


muname:
Lickskillet-Brazlan-Dezellem complex, 0 to 20 percent slopes


muname:
Skaha-Tubspring complex, 0 to 8 percent slopes


muname:
Zen-Argabak-Horseflat complex, 0 to 20 percent slopes


muname:
Ellisforde-Nespelem-Nemire complex, 0 to 8 percent slopes


muname:
Argabak-Horseflat-Toler complex, 0 to 20 percent slopes


muname:
Toler silt loam, 15 to 30 percent slopes


muname:
Toler-Horseflat-Benwy complex, 3 to 8 percent slopes


muname:
Toler-Horseflat-Ralls complex, 8 to 15 percent slopes


muname:
Toler-Horseflat-Ralls complex, 15 to 30 percent slopes


muname:
Toler-Horseflat complex, 3 to 8 percent slopes


muname:
Toler-Horseflat complex, 8 to 15 percent slopes


muname:
Drysel silt loam, 5 to 15 percent slopes


muname:
Drysel-Wanapum complex, 5 to 15 percent slopes


muname:
Burch fine sandy loam, 8 to 15 percent slopes


muname:
Soaplake-Roosevelt-Rock outcrop complex, 30 to 65 percent slopes


muname:
Xerofluvents, nearly level to strongly sloping


muname:
Rock outcrop-Couleedam-Roosevelt complex, 30 to 70 percent slopes


muname:
Soaplake-Roosevelt-Rock outcrop complex, 0 to 30 percent slopes


muname:
Badge-Bakeoven complex, 25 to 55 percent slopes


muname:
Rubble land-Rock outcrop complex, very steep


muname:
Argabak-Rock outcrop complex, 0 to 35 percent slopes


muname:
Ellisforde fine sandy loam, 3 to 8 percent slopes


muname:
Argabak very cobbly loam, 0 to 20 percent slopes


muname:
Bakeoven very cobbly loam, 0 to 35 percent slopes


muname:
Argabak-Badge complex, 8 to 30 percent slopes


muname:
Argabak-Horseflat complex, 0 to 30 percent slopes


muname:
Argabak-Camaspatch-Badge complex, 30 to 65 percent slopes


muname:
Argabak-Horseflat-Zen complex, 0 to 20 percent slopes


muname:
Bakeoven-Lickskillet-Zen complex, 5 to 25 percent slopes


muname:
Bakeoven-Roloff complex, 0 to 25 percent slopes


muname:
Bakeoven-Touhey complex, 0 to 25 percent slopes


muname:
Rubble land-Stemilt-Rock outcrop complex, 30 to 65 percent slopes


muname:
Cheviot-Ralls-Dougville complex, 8 to 15 percent slopes


muname:
Cheviot-Ralls-Grinrod complex, 15 to 30 percent slopes


muname:
Cheviot-Ralls-Rubble land complex, 30 to 65 percent slopes


muname:
Entiat-Roosevelt-Rock outcrop complex, 8 to 30 percent slopes


muname:
Entiat-Rock outcrop-Torriorthents complex, 30 to 70 percent slopes


muname:
McCue-Broadax complex, 3 to 8 percent slopes


muname:
McCue-Broadax complex, 8 to 15 percent slopes


muname:
Finley stony loam, 3 to 8 percent slopes


muname:
Esquatzel silt loam, channeled, 0 to 3 percent slopes


muname:
Esquatzel silt loam, cemented substratum, 0 to 3 percent slopes


muname:
Ephrata fine sandy loam, 2 to 5 percent slopes


muname:
Peshastin fine sandy loam, 3 to 8 percent slopes


muname:
Peshastin fine sandy loam 8 to 15 percent slopes


muname:
Peshastin fine sandy loam, 15 to 30 percent slopes


muname:
Peshastin stony fine sandy loam, 30 to 60 percent slopes


muname:
Esquatzel silt loam, 0 to 3 percent slopes


muname:
Haploxerolls, moderately well drained, nearly level to gently sloping


muname:
Haploxerolls, nearly level to gently sloping


muname:
Finley gravelly fine sandy loam, 0 to 15 percent slopes


muname:
Waterflat fine sandy loam, 0 to 3 percent slopes


muname:
Finley very cobbly fine sandy loam, 0 to 15 percent slopes


muname:
Grinrod-Ralls-Argabak complex, 8 to 50 percent slopes


muname:
Vitrandic Argixerolls-Argabak complex, 30 to 60 percent slopes


muname:
Grinrod-Ralls-Rubble land complex, 30 to 70 percent slopes


muname:
Grinrod-Rock outcrop-Rubble land complex, 30 to 70 percent slopes


muname:
Dougville-Norax-Nemire complex, 0 to 25 percent slopes


muname:
Hanning silt loam, 3 to 8 percent slopes


muname:
Kiona cobbly very fine sandy loam, 25 to 65 percent slopes


muname:
Kiona-Rock outcrop complex, 25 to 65 percent slopes


muname:
Lickskillet very cobbly loam, 15 to 35 percent slopes


muname:
Lickskillet very cobbly loam, 35 to 65 percent slopes


muname:
Dinkels-Rock outcrop complex, 35 to 70 percent slopes


muname:
Corbaley-Kester complex, 0 to 5 percent slopes


muname:
Hanning-McCue-Badgermont complex, 3 to 8 percent slopes


muname:
Hanning-McCue-Badgermont complex, 8 to 15 percent slopes


muname:
Toler-Kester complex, 3 to 8 percent slopes


muname:
Beverly cobbly fine sandy loam, 0 to 8 percent slopes


muname:
Burbank loamy fine sand, 0 to 8 percent slopes


muname:
Burbank loamy fine sand, 8 to 25 percent slopes


muname:
Broadax silt loam, 0 to 8 percent slopes


muname:
Broadax silt loam, 8 to 15 percent slopes


muname:
Dougville-Badge complex, 30 to 65 percent slopes


muname:
Jordy-Camaspatch complex, 3 to 8 percent slopes


muname:
Jordy-Camaspatch complex, 8 to 15 percent slopes


muname:
Jordy-Camaspatch complex, 15 to 30 percent slopes


muname:
Badge-Dougville complex, 8 to 30 percent slopes


muname:
Badge very cobbly silt loam, 15 to 30 percent slopes


muname:
Badge very cobbly silt loam, 30 to 65 percent slopes


muname:
Slusser fine sandy loam, indurated substratum, 3 to 8 percent slopes


muname:
Badge-Stemilt complex, 3 to 30 percent slopes


muname:
Badge-Stemilt complex, 30 to 65 percent slopes


muname:
Prosser-Starbuck complex, 15 to 45 percent slopes


muname:
Toler-Corbaley complex, 3 to 8 percent slopes


muname:
Toler-Corbaley complex, 8 to 15 percent slopes


muname:
Toler-Corbaley complex, 15 to 30 percent slopes


muname:
Ralls silt loam, 25 to 55 percent slopes


muname:
Renslow silt loam, 0 to 8 percent slopes


muname:
Renslow silt loam, 8 to 15 percent slopes


muname:
Renslow silt loam, 15 to 30 percent south slopes


muname:
Benwy-Selah-Alstown complex, 0 to 8 percent slopes


muname:
Benwy-Selah-Alstown complex, 8 to 15 percent slopes


muname:
Renslow silt loam, cemented substratum, 0 to 8 percent slopes


muname:
Renslow silt loam, cemented substratum, 8 to 15 percent slopes


muname:
Roloff-Bakeoven complex, 5 to 25 percent slopes


muname:
Renslow silt loam, cemented substratum, 15 to 30 percent slopes


muname:
Quincy-Wanser complex, 0 to 15 percent slopes


muname:
Rinquin loamy fine sand, 0 to 10 percent slopes


muname:
Wacota silt loam, 10 to 15 percent slopes


muname:
Wacota silt loam, 15 to 30 percent slopes


muname:
Wacota silt loam, 30 to 40 percent slopes


muname:
Wacota silt loam, flooded, 0 to 2 percent slopes


muname:
Wacota-Ritzcal complex, 10 to 30 percent slopes


muname:
Quincy fine sand, 30 to 55 percent slopes


muname:
Quincy fine sand, moist, 0 to 15 percent slopes


muname:
Quincy loamy fine sand, 15 to 30 percent slopes


muname:
Quincy loamy fine sand, 30 to 55 percent slopes


muname:
Quincy loamy fine sand, loamy substratum, 0 to 10 percent slopes


muname:
Quincy loamy fine sand, loamy substratum, 10 to 15 percent slopes


muname:
Quincy loamy fine sand, loamy substratum, 15 to 25 percent slopes


muname:
Quincy-Dune land complex, 5 to 40 percent slopes


muname:
Quincy-Hezel complex, 0 to 15 percent slopes


muname:
Quincy-Hezel complex, 15 to 30 percent slopes


muname:
Quincy-Hezel complex, fine sand, 15 to 30 percent slopes


muname:
Ritzcal-Ritzville complex, 15 to 30 percent slopes


muname:
Ritzcal-Ritzville complex, 30 to 60 percent slopes


muname:
Ritzville silt loam, 0 to 2 percent slopes


muname:
Ritzville silt loam, 2 to 5 percent slopes


muname:
Ritzville silt loam, 5 to 10 percent slopes


muname:
Chedehap fine sandy loam, 2 to 5 percent slopes


muname:
Ritzville silt loam, 10 to 15 percent slopes


muname:
Ritzville silt loam, 15 to 30 percent slopes


muname:
Ritzville silt loam, stratified substratum, 2 to 5 percent slopes


muname:
Ritzville silt loam, stratified substratum, 5 to 10 percent slopes


muname:
Ritzville silt loam, stratified substratum, 10 to 15 percent slopes


muname:
Ritzville silt loam, stratified substratum, 15 to 30 percent slopes


muname:
Ritzville silt loam, stratified substratum, 30 to 60 percent slopes


muname:
Ritzville-Nansene complex, 30 to 45 percent slopes


muname:
Chedehap fine sandy loam, 5 to 10 percent slopes


muname:
Roloff silt loam, 15 to 30 percent slopes


muname:
Roloff silt loam, 30 to 60 percent slopes


muname:
Roloff-Lickskillet-Rock outcrop complex, 0 to 15 percent slopes


muname:
Roloff-Rock outcrop complex, 30 to 70 percent slopes


muname:
Roloff-Rock outcrop-Rubble land complex, 30 to 70 percent slopes


muname:
Royal loamy fine sand, 10 to 30 percent slopes


muname:
Cleman fine sandy loam, 0 to 2 percent slopes


muname:
Royal fine sandy loam, 5 to 10 percent slopes


muname:
Royal-Timmerman complex, 15 to 30 percent slopes


muname:
Sagehill very fine sandy loam, 0 to 2 percent slopes


muname:
Sagehill very fine sandy loam, 2 to 5 percent slopes


muname:
Sagehill very fine sandy loam, 5 to 10 percent slopes


muname:
Sagehill very fine sandy loam, 15 to 30 percent slopes


muname:
Sagehill very fine sandy loam, cemented substratum, 0 to 2 percent slopes


muname:
Sagehill very fine sandy loam, cemented substratum, 2 to 5 percent slopes


muname:
Eltopia very fine sandy loam, 0 to 2 percent slopes


muname:
Sagehill very fine sandy loam, gravelly substratum, 0 to 2 percent slopes


muname:
Sagehill very fine sandy loam, gravelly substratum, 2 to 5 percent slopes


muname:
Sagehill-Kennewick complex, 0 to 2 percent slopes


muname:
Sagehill-Kennewick-Shano complex, 15 to 60 percent slopes


muname:
Sagemoor very fine sandy loam, 0 to 2 percent slopes


muname:
Sagemoor very fine sandy loam, 2 to 5 percent slopes


muname:
Sagemoor very fine sandy loam, 5 to 10 percent slopes


muname:
Schlomer silt loam, 0 to 2 percent slopes


muname:
Schlomer silt loam, 2 to 5 percent slopes


muname:
Schlomer silt loam, 5 to 10 percent slopes


muname:
Eltopia very fine sandy loam, 2 to 5 percent slopes


muname:
Schlomer silt loam, 10 to 15 percent slopes


muname:
Schlomer silt loam, 15 to 25 percent slopes


muname:
Shano silt loam, 15 to 25 percent slopes


muname:
Shano silt loam, 25 to 40 percent slopes


muname:
Shano silt loam, stratified substratum, 0 to 2 percent slopes


muname:
Shano silt loam, stratified substratum, 2 to 5 percent slopes


muname:
Shano silt loam, stratified substratum, 5 to 10 percent slopes


muname:
Shano silt loam, stratified substratum, 10 to 15 percent slopes


muname:
Shano silt loam, stratified substratum, 15 to 30 percent slopes


muname:
Shano-Kennewick complex, 15 to 30 percent slopes


muname:
Shano-Kennewick complex, 30 to 60 percent slopes


muname:
Starbuck fine sandy loam, 0 to 15 percent slopes


muname:
Starbuck-Prosser complex, 0 to 15 percent slopes


muname:
Starbuck-Prosser-Finley complex, 0 to 25 percent slopes


muname:
Starbuck-Prosser-Rock outcrop complex, 15 to 30 percent slopes


muname:
Alderdale extremely cobbly loamy sand, 0 to 5 percent slopes


muname:
Chedehap fine sandy loam, 0 to 2 percent slopes


muname:
Quincy-Hezel-Warden complex, 0 to 15 percent slopes


muname:
Warden very fine sandy loam, 10 to 15 percent slopes


muname:
Warden very fine sandy loam, 15 to 25 percent slopes


muname:
Warden very fine sandy loam, 25 to 40 percent slopes


muname:
Warden silt loam, 5 to 10 percent slopes


muname:
Warden silt loam, 10 to 15 percent slopes


muname:
Warden silt loam, 15 to 25 percent slopes


muname:
Warden silt loam, 25 to 40 percent slopes


muname:
Warden silt loam, cemented substratum, 0 to 2 percent slopes


muname:
Warden silt loam, cemented substratum, 2 to 5 percent slopes


muname:
Warden silt loam, cemented substratum, 5 to 10 percent slopes


muname:
Wiehl fine sandy loam, 15 to 35 percent slopes


muname:
Wiehl very fine sandy loam, 0 to 2 percent slopes


muname:
Wiehl very fine sandy loam, 2 to 5 percent slopes


muname:
Wiehl-Schlomer complex, 10 to 35 percent slopes


muname:
Willis silt loam, 5 to 15 percent slopes


muname:
Winchester loamy coarse sand, 2 to 5 percent slopes


muname:
Winchester loamy coarse sand, 5 to 10 percent slopes


muname:
Finley gravelly sandy loam, 5 to 10 percent slopes


muname:
Finley very fine sandy loam, 0 to 2 percent slopes


muname:
Finley very fine sandy loam, 2 to 5 percent slopes


muname:
Finley-Burbank-Starbuck complex, 0 to 10 percent slopes


muname:
Finley-Neppel complex, 0 to 10 percent slopes


muname:
Hezel loamy fine sand, 0 to 15 percent slopes


muname:
Badland-Xeric Torriorthents complex, very steep


muname:
Hezel loamy fine sand, 15 to 30 percent slopes


muname:
Hezel loamy fine sand, 30 to 60 percent slopes


muname:
Hezel loamy fine sand, cobbly substratum, 0 to 10 percent slopes


muname:
Kahlotus very fine sandy loam, 0 to 2 percent slopes


muname:
Kahlotus very fine sandy loam, 2 to 5 percent slopes


muname:
Kahlotus very fine sandy loam, 5 to 10 percent slopes


muname:
Kahlotus very fine sandy loam, 10 to 15 percent slopes


muname:
Kahlotus very fine sandy loam, 15 to 30 percent slopes


muname:
Kahlotus very fine sandy loam, 30 to 40 percent slopes


muname:
Kahlotus-Kennewick complex, 15 to 30 percent slopes


muname:
Burbank loamy fine sand, 0 to 5 percent slopes


muname:
Kahlotus-Kennewick complex, 30 to 60 percent slopes


muname:
Kahlotus-Stratford complex, 0 to 15 percent slopes


muname:
Kahlotus-Stratford complex, 15 to 30 percent slopes


muname:
Kennewick silt loam, 5 to 10 percent slopes


muname:
Kennewick silt loam, 10 to 15 percent slopes


muname:
Kennewick silt loam, 15 to 35 percent slopes


muname:
Kiona-Prosser-Starbuck complex, 30 to 60 percent slopes


muname:
Kiona-Rock outcrop complex, 30 to 120 percent slopes


muname:
Burbank loamy fine sand, 5 to 10 percent slopes


muname:
Koehler fine sand, 0 to 15 percent slopes


muname:
Koehler loamy fine sand, 0 to 10 percent slopes


muname:
Lickskillet-Bakeoven complex, 0 to 35 percent slopes


muname:
Magallon-Stratford-Farrell complex, 10 to 30 percent slopes


muname:
Magallon-Winchester-Farrell complex, 30 to 60 percent slopes


muname:
Malaga cobbly sandy loam, 0 to 15 percent slopes


muname:
Nansene-Ritzville complex, 45 to 65 percent slopes


muname:
Neppel fine sandy loam, 0 to 2 percent slopes


muname:
Neppel fine sandy loam, 2 to 5 percent slopes


muname:
Neppel fine sandy loam, 5 to 10 percent slopes


muname:
Burbank gravelly loamy fine sand, 15 to 35 percent slopes


muname:
Neppel very fine sandy loam, 5 to 10 percent slopes


muname:
Neppel very fine sandy loam, 10 to 15 percent slopes


muname:
Neppel very fine sandy loam, 15 to 30 percent slopes


muname:
Neppel-Finley complex, 15 to 50 percent slopes


muname:
Ottmar silt loam, 5 to 10 percent slopes


muname:
Burke very fine sandy loam, 0 to 2 percent slopes


muname:
Ottmar silt loam, very deep, 0 to 2 percent slopes


muname:
Ottmar silt loam, very deep, 2 to 5 percent slopes


muname:
Ottmar silt loam, very deep, 5 to 10 percent slopes


muname:
Ottmar clay loam, very deep, 0 to 5 percent slopes


muname:
Ottmar clay loam, very deep, 5 to 10 percent slopes


muname:
Ottmar-Schlomer complex, 5 to 15 percent slopes


muname:
Prosser fine sandy loam, 0 to 2 percent slopes


muname:
Prosser fine sandy loam, 2 to 5 percent slopes


muname:
Prosser fine sandy loam, 5 to 10 percent slopes


muname:
Burke very fine sandy loam, 2 to 5 percent slopes


muname:
Prosser silt loam, 5 to 10 percent slopes


muname:
Prosser-Starbuck-Rock outcrop complex, 2 to 15 percent slopes


muname:
Prosser-Starbuck-Rock outcrop complex, droughty, 2 to 15 percent slopes


muname:
Quincy fine sand, 2 to 15 percent slopes


muname:
Quincy-Quinton-Rock outcrop complex, 0 to 30 percent slopes


muname:
Quincy-Timmerman complex, 0 to 15 percent slopes


muname:
Starbuck-Prosser-Rock outcrop complex, droughty, 15 to 30 percent slopes


muname:
Starbuck-Roloff-Rock outcrop complex, 15 to 30 percent slopes


muname:
Stratford silt loam, 0 to 5 percent slopes


muname:
Stratford silt loam, 5 to 10 percent slopes


muname:
Stratford silt loam, 15 to 30 percent slopes


muname:
Tauncal very fine sandy loam, 2 to 5 percent slopes


muname:
Tauncal very fine sandy loam, 5 to 10 percent slopes


muname:
Tauncal very fine sandy loam, 10 to 15 percent slopes


muname:
Tauncal very fine sandy loam, 15 to 30 percent slopes


muname:
Taunton very fine sandy loam, 0 to 2 percent slopes


muname:
Taunton very fine sandy loam, 2 to 5 percent slopes


muname:
Timmerman fine sandy loam, 0 to 2 percent slopes


muname:
Timmerman fine sandy loam, 2 to 5 percent slopes


muname:
Timmerman fine sandy loam, 5 to 10 percent slopes


muname:
Urban land-Torripsamments complex, gently rolling


muname:
Wacota silt loam, 5 to 10 percent slopes


muname:
Willis silt loam, 0 to 10 percent slopes


muname:
Timentwa very fine sandy loam, 0 to 15 percent slopes


muname:
Timmerman loamy sand, 0 to 5 percent slopes


muname:
Timmerman coarse sandy loam, 0 to 2 percent slopes


muname:
Timmerman coarse sandy loam, 2 to 5 percent slopes


muname:
Timmerman coarse sandy loam, 5 to 10 percent slopes


muname:
Timmerman coarse sandy loam, thin solum, 0 to 2 percent slopes


muname:
Timmerman coarse sandy loam, thin solum, 2 to 5 percent slopes


muname:
Bagdad-Endicott silt loams, 7 to 20 percent slopes


muname:
Touhey very fine sandy loam, 0 to 15 percent slopes


muname:
Wahluke very fine sandy loam, 0 to 2 percent slopes


muname:
Wahluke very fine sandy loam, 2 to 5 percent slopes


muname:
Wanser loamy fine sand, 0 to 5 percent slopes


muname:
Wanser-Quincy fine sands, 0 to 5 percent slopes


muname:
Bagdad-Endicott silt loams, 25 to 40 percent slopes


muname:
Bakeoven very cobbly loam, 0 to 7 percent slopes


muname:
Beckley fine sandy loam, 0 to 7 percent slopes


muname:
Bakeoven-Anders complex, 0 to 15 percent slopes


muname:
Adkins very fine sandy loam, 0 to 5 percent slopes


muname:
Bakeoven-Condon complex, 0 to 25 percent slopes


muname:
Benco gravelly loam, 0 to 15 percent slopes


muname:
Benco stony loam, 0 to 15 percent slopes


muname:
Burbank loamy fine sand, 5 to 15 percent slopes


muname:
Burbank very cobbly loamy sand, 0 to 15 percent slopes


muname:
Burbank stony loamy sand, 2 to 15 percent slopes


muname:
Adkins very fine sandy loam, 5 to 10 percent slopes


muname:
Burbank very bouldery loamy sand, 0 to 10 percent slopes


muname:
Chard very fine sandy loam, 5 to 15 percent slopes


muname:
Condon silt loam, 5 to 25 percent slopes


muname:
Ellisforde silt loam, 5 to 15 percent slopes


muname:
Entiat-Rock outcrop complex, 25 to 65 percent slopes


muname:
Adkins very fine sandy loam, 10 to 15 percent slopes


muname:
Ephrata fine sandy loam, 0 to 2 percent slopes


muname:
Ephrata fine sandy loam, 5 to 10 percent slopes


muname:
Ephrata gravelly sandy loam, 0 to 2 percent slopes


muname:
Ephrata gravelly sandy loam, 2 to 5 percent slopes


muname:
Ephrata-Malaga complex, 0 to 5 percent slopes


muname:
Ephrata-Malaga complex, 5 to 15 percent slopes


muname:
Farrell very fine sandy loam, 5 to 10 percent slopes


muname:
Adkins very fine sandy loam, 15 to 35 percent slopes


muname:
Finley-Taunton complex, 0 to 5 percent slopes


muname:
Finley-Taunton complex, 5 to 10 percent slopes


muname:
Hezel loamy fine sand, 0 to 10 percent slopes


muname:
Kennewick loamy fine sand, 0 to 5 percent slopes


muname:
Kennewick loamy fine sand, 5 to 10 percent slopes


muname:
Kennewick fine sandy loam, 0 to 2 percent slopes


muname:
Kennewick fine sandy loam, 2 to 5 percent slopes


muname:
Adkins very fine sandy loam, cemented substratum, 0 to 5 percent slopes


muname:
Kennewick fine sandy loam, 5 to 10 percent slopes


muname:
Kennewick fine sandy loam, 10 to 15 percent slopes


muname:
Kennewick silt loam, 10 to 25 percent slopes


muname:
Adkins very fine sandy loam, cemented substratum, 5 to 10 percent slopes


muname:
Magallon sandy loam, 0 to 5 percent slopes


muname:
Magallon sandy loam, 5 to 10 percent slopes


muname:
Malaga gravelly sandy loam, 0 to 5 percent slopes


muname:
Malaga gravelly sandy loam, 5 to 15 percent slopes


muname:
Malaga cobbly sandy loam, 15 to 35 percent slopes


muname:
Malaga stony sandy loam, 0 to 15 percent slopes


muname:
Malaga very stony sandy loam, 0 to 35 percent slopes


muname:
Malaga-Ephrata complex, 0 to 15 percent slopes


muname:
Adkins very fine sandy loam, cemented substratum, 10 to 15 percent slopes


muname:
Adkins very fine sandy loam, cemented substratum, 15 to 35 percent slopes


muname:
Prosser very fine sandy loam, 2 to 5 percent slopes


muname:
Prosser very fine sandy loam, 5 to 10 percent slopes


muname:
Prosser very fine sandy loam, 10 to 15 percent slopes


muname:
Prosser very fine sandy loam, 15 to 25 percent slopes


muname:
Prosser-Starbuck very fine sandy loams, 0 to 15 percent slopes


muname:
Quincy sand, 5 to 25 percent slopes, eroded


muname:
Quincy loamy fine sand, 15 to 35 percent slopes


muname:
Adkins loamy fine sand, 5 to 15 percent slopes


muname:
Quinton-Schawana complex, 5 to 20 percent slopes


muname:
Ralls stony silt loam, 3 to 25 percent slopes


muname:
Renslow silt loam, 0 to 5 percent slopes


muname:
Renslow silt loam, 25 to 35 percent slopes


muname:
Renslow-Willis silt loams, 0 to 15 percent slopes


muname:
Renslow-Willis silt loams, 15 to 25 percent slopes


muname:
Anders silt loam, 0 to 10 percent slopes


muname:
Roloff silt loam, 0 to 25 percent slopes


muname:
Royal loamy fine sand, 10 to 25 percent slopes


muname:
Royal very fine sandy loam, cemented substratum, 2 to 5 percent slopes


muname:
Royal very fine sandy loam, cemented substratum, 5 to 10 percent slopes


muname:
Sagemoor silt loam, 5 to 10 percent slopes


muname:
Sagemoor silt loam, 10 to 15 percent slopes


muname:
Schawana cobbly loamy fine sand, 15 to 55 percent slopes


muname:
Scoon stony silt loam, 0 to 15 percent slopes


muname:
Shano silt loam, 15 to 35 percent slopes


muname:
Starbuck very fine sandy loam, 0 to 15 percent slopes


muname:
Starbuck stony silt loam, 0 to 30 percent slopes


muname:
Starbuck-Kiona stony silt loams, 30 to 65 percent slopes


muname:
Starbuck-Prosser complex, 0 to 25 percent slopes


muname:
Strat gravelly loam, 0 to 15 percent slopes


muname:
Strat-Stratford complex, 0 to 15 percent slopes


muname:
Taunton loamy fine sand, 0 to 10 percent slopes


muname:
Taunton fine sandy loam, 0 to 2 percent slopes


muname:
Taunton fine sandy loam, 5 to 10 percent slopes


muname:
Taunton silt loam, 0 to 2 percent slopes


muname:
Taunton silt loam, 2 to 5 percent slopes


muname:
Taunton silt loam, 10 to 15 percent slopes


muname:
Bagdad silt loam, 5 to 20 percent slopes


muname:
Taunton stony silt loam, 0 to 25 percent slopes


muname:
Beckley fine sandy loam, 25 to 55 percent slopes


muname:
Benco cobbly silt loam, 0 to 7 percent slopes


muname:
Broadax silt loam, 0 to 7 percent slopes


muname:
Broadax silt loam, 7 to 25 percent slopes


muname:
Broadax silt loam, 25 to 40 percent slopes


muname:
Broadax silt loam, low rainfall, 7 to 25 percent slopes


muname:
Anders gravelly silt loam, 0 to 15 percent slopes


muname:
Broadax-Lance silt loams, 7 to 25 percent slopes


muname:
Broadax-Lance silt loams, 25 to 40 percent slopes


muname:
Conconully very stony fine sandy loam, 25 to 55 percent slopes


muname:
Dragoon silt loam, 0 to 7 percent slopes


muname:
Dragoon silt loam, 7 to 25 percent slopes


muname:
Anders-Bakeoven-Rock outcrop complex, 0 to 15 percent slopes


muname:
Dragoon silt loam, 25 to 40 percent slopes


muname:
Dragoon very stony silt loam, 7 to 25 percent slopes


muname:
Endicott silt loam, 5 to 25 percent slopes


muname:
Ewall loamy sand, 0 to 15 percent slopes


muname:
Ewall loamy sand, 15 to 35 percent slopes


muname:
Ewall loamy sand, 35 to 55 percent slopes


muname:
Farrell fine sandy loam, 5 to 25 percent slopes


muname:
Badge-Bakeoven-Rock outcrop complex, very steep


muname:
Hanning silt loam, 0 to 7 percent slopes


muname:
Hanning silt loam, 7 to 25 percent slopes


muname:
Hesseltine silt loam, 0 to 15 percent slopes


muname:
Hesseltine very stony silt loam, 0 to 15 percent slopes


muname:
Kuhl cobbly silt loam, 0 to 15 percent slopes


muname:
Nespelem silt loam, 3 to 15 percent slopes


muname:
Nespelem silt loam, 15 to 35 percent slopes


muname:
Nespelem silt loam, 35 to 45 percent slopes


muname:
Phoebe sandy loam, 0 to 15 percent slopes


muname:
Reardan silt loam, 0 to 7 percent slopes


muname:
Reardan silt loam, 7 to 25 percent slopes


muname:
Reardan silt loam, 25 to 40 percent slopes


muname:
Renslow silt loam, 5 to 25 percent slopes


muname:
Ritzville silt loam, 5 to 25 percent slopes


muname:
Roloff-Bakeoven-Rock outcrop complex, 0 to 15 percent slopes


muname:
Speigle very stony silt loam, 25 to 55 percent slopes


muname:
Spens extremely gravelly loamy sand, 25 to 50 percent slopes


muname:
Bagdad silt loam, 7 to 25 percent slopes, eroded


muname:
Spokane very stony loam, 5 to 30 percent slopes


muname:
Spokane very stony loam, 30 to 55 percent slopes


muname:
Spokane-Rock outcrop complex, very steep


muname:
Springdale gravelly sandy loam, 0 to 7 percent slopes


muname:
Springdale cobbly sandy loam, 0 to 15 percent slopes


muname:
Starbuck cobbly silt loam, 0 to 20 percent slopes


muname:
Strat very cobbly silt loam, 3 to 25 percent slopes


muname:
Stratford gravelly silt loam, 0 to 15 percent slopes


muname:
Tucannon silt loam, 0 to 5 percent slopes


muname:
Tucannon-Rock outcrop complex, 0 to 15 percent slopes


muname:
Bagdad silt loam, 25 to 40 percent slopes


muname:
Willis silt loam, 5 to 25 percent slopes


muname:
Willis variant silt loam, 5 to 25 percent slopes


muname:
Bagdad-Endicott silt loams, 7 to 25 percent slopes


muname:
Caldwell-Latah complex, 0 to 3 percent slopes


muname:
Rock outcrop-Lithic Xerorthents complex, 0 to 30 percent slopes


muname:
Roloff cobbly silt loam, 0 to 15 percent slopes


muname:
Roloff-Starbuck complex, 0 to 30 percent slopes


muname:
Schumacher silt loam, 3 to 15 percent slopes


muname:
Schumacher silt loam, 15 to 25 percent slopes


muname:
Schumacher silt loam, 25 to 40 percent slopes


muname:
Athena silt loam, 7 to 25 percent slopes


muname:
Speigle-Rock outcrop complex, 3 to 30 percent slopes


muname:
Speigle-Rock outcrop complex, 30 to 65 percent slopes


muname:
Spofford silt loam, 0 to 15 percent slopes


muname:
Staley silt loam, 7 to 25 percent slopes


muname:
Bakeoven-Tucannon complex, 0 to 30 percent slopes


muname:
Beckley sandy loam, 0 to 20 percent slopes


muname:
Beckley sandy loam, 20 to 40 percent slopes


muname:
Almota silt loam, 25 to 65 percent slopes


muname:
Calouse silt loam, 3 to 7 percent slopes


muname:
Calouse silt loam, 7 to 25 percent slopes


muname:
Calouse silt loam, 5 to 25 percent slopes, eroded


muname:
Calouse silt loam, 25 to 40 percent slopes


muname:
Calouse silt loam, 25 to 40 percent slopes, eroded


muname:
Chard silt loam, 15 to 25 percent slopes


muname:
Alpowa cobbly silt loam, 30 to 65 percent slopes


muname:
Cheney very cobbly silt loam, 0 to 20 percent slopes


muname:
Endicott silt loam, 3 to 15 percent slopes


muname:
Farrell very fine sandy loam, 0 to 7 percent slopes


muname:
Farrell very fine sandy loam, 7 to 25 percent slopes


muname:
Garfield silty clay loam, 3 to 25 percent slopes


muname:
Gwin-Linville complex, 30 to 65 percent slopes


muname:
Anders silt loam, 3 to 15 percent slopes


muname:
Gwin-Tucannon complex, 3 to 30 percent slopes


muname:
Hesseltine cobbly silt loam, 0 to 30 percent slopes


muname:
Kuhl-Alpowa complex, 30 to 65 percent slopes


muname:
Kuhl-Anders complex, 3 to 15 percent slopes


muname:
Kuhl-Asotin complex, 7 to 30 percent slopes


muname:
Lance silt loam, 25 to 40 percent slopes


muname:
Anders-Kuhl complex, 3 to 15 percent slopes


muname:
Larkin silt loam, 3 to 15 percent slopes


muname:
Larkin silt loam, 15 to 25 percent slopes


muname:
Larkin silt loam, 25 to 40 percent slopes


muname:
Athena silt loam, 40 to 55 percent slopes


muname:
Palouse-Thatuna silt loams, 7 to 25 percent slopes


muname:
Palouse-Thatuna silt loams, 25 to 40 percent slopes


muname:
Palouse-Thatuna silt loams, 40 to 55 percent slopes


muname:
Reardan silt loam, 3 to 15 percent slopes


muname:
Risbeck silt loam, 15 to 40 percent slopes


muname:
Ritzville silt loam, 3 to 30 percent slopes


muname:
Starbuck-Alpowa complex, 30 to 65 percent slopes


muname:
Stratford very cobbly loam, 0 to 15 percent slopes


muname:
Tekoa silt loam, 25 to 40 percent slopes


muname:
Almota silt loam, 7 to 25 percent slopes


muname:
Athena silt loam, 7 to 25 percent slopes, eroded


muname:
Tekoa gravelly silt loam, 25 to 55 percent slopes


muname:
Tekoa gravelly silt loam, deep, 25 to 55 percent slopes


muname:
Tekoa stony silt loam, 25 to 40 percent slopes


muname:
Thatuna silt loam, 3 to 7 percent slopes


muname:
Thatuna silt loam, 7 to 25 percent slopes


muname:
Thatuna silt loam, 25 to 40 percent slopes


muname:
Thatuna silt loam, 40 to 55 percent slopes


muname:
Thatuna-Tilma silt loams, 7 to 25 percent slopes


muname:
Thatuna-Tilma silt loams, 25 to 40 percent slopes


muname:
Thatuna-Naff silt loams, 7 to 25 percent slopes


muname:
Athena silt loam, 25 to 40 percent slopes


muname:
Tilma silt loam, 25 to 40 percent slopes


muname:
Tucannon silt loam, 7 to 25 percent slopes


muname:
Tucannon-Bakeoven complex, 0 to 30 percent slopes


muname:
Walla Walla silt loam, 3 to 7 percent slopes


muname:
Walla Walla silt loam, 7 to 25 percent slopes


muname:
Walla Walla silt loam, 15 to 30 percent slopes, eroded


muname:
Walla Walla silt loam, 25 to 40 percent slopes


muname:
Athena silt loam, 25 to 40 percent slopes, eroded


muname:
Walla Walla silt loam, 40 to 55 percent slopes


muname:
Walvan silt loam, 7 to 25 percent slopes


muname:
Larkin silt loam, 40 to 55 percent slopes


muname:
Linville silt loam, 30 to 65 percent slopes


muname:
Magallon sandy loam, 20 to 40 percent slopes


muname:
Asotin silt loam, 7 to 25 percent slopes


muname:
Naff-Garfield complex, 3 to 25 percent slopes


muname:
Palouse silt loam, 3 to 7 percent slopes


muname:
Palouse silt loam, 7 to 25 percent slopes


muname:
Palouse silt loam, 7 to 25 percent slopes, eroded


muname:
Palouse silt loam, 25 to 40 percent slopes


muname:
Palouse silt loam, 25 to 40 percent slopes, eroded


muname:
Palouse silt loam, 40 to 55 percent slopes


muname:
Asotin silt loam, 25 to 65 percent slopes


muname:
Palouse-Thatuna silt loams, 3 to 7 percent slopes


muname:
Ahtanum silt loam, 0 to 2 percent slopes


muname:
Ahtanum silt loam, 2 to 5 percent slopes


muname:
Ashue gravelly loam, 0 to 2 percent slopes


muname:
Ashue gravelly loam, 2 to 5 percent slopes


muname:
Quincy loamy fine sand, 0 to 2 percent slopes


muname:
Quincy loamy fine sand, 2 to 15 percent slopes


muname:
Ritzville silt loam, 5 to 8 percent slopes


muname:
Ritzville silt loam, 8 to 15 percent slopes


muname:
Ritzville silt loam, gravelly subsoil variant, 5 to 8 percent slopes


muname:
Ritzville silt loam, gravelly subsoil variant, 8 to 15 percent slopes


muname:
Rock Creek very stony loam, 0 to 20 percent slopes


muname:
Shano silt loam, 15 to 30 percent slopes


muname:
Stanfield silt loam, 0 to 2 percent slopes


muname:
Stanfield silt loam, 2 to 5 percent slopes


muname:
Toppenish silt loam, 0 to 2 percent slopes


muname:
Toppenish silt loam, 2 to 5 percent slopes


muname:
Warden fine sandy loam, 0 to 2 percent slopes


muname:
Warden fine sandy loam, 2 to 5 percent slopes


muname:
Warden fine sandy loam, 5 to 8 percent slopes


muname:
Warden silt loam, 15 to 30 percent slopes


muname:
Weirman fine sandy loam, 0 to 2 percent slopes


muname:
Weirman fine sandy loam, 2 to 5 percent slopes


muname:
White Swan silt loam, 0 to 2 percent slopes


muname:
White Swan silt loam, 2 to 5 percent slopes


muname:
White Swan silt loam, 5 to 8 percent slopes


muname:
Argabak very cobbly loam, 3 to 15 percent slopes


muname:
Argabak very cobbly loam, 15 to 30 percent slopes


muname:
Argabak extremely cobbly loam, 3 to 15 percent slopes


muname:
Argabak extremely cobbly loam, 15 to 30 percent slopes


muname:
Argabak very stony loam, 3 to 15 percent slopes


muname:
Argabak very stony loam, 15 to 30 percent slopes


muname:
Argabak-Camaspatch complex, 3 to 15 percent slopes


muname:
Argabak-Horseflat complex, 3 to 15 percent slopes


muname:
Marlic-Zen-Laric complex, 3 to 15 percent slopes


muname:
Meloza-Roza complex, 5 to 10 percent slopes


muname:
Meloza-Roza complex, 10 to 15 percent slopes


muname:
Meloza-Roza complex, 15 to 30 percent slopes


muname:
Nack-Opnish complex, 0 to 2 percent slopes


muname:
Neppel-Scoon complex, 10 to 15 percent slopes


muname:
Nevo extremely gravelly sandy loam, 3 to 15 percent slopes


muname:
Nevo-Fortyday complex, 3 to 15 percent slopes


muname:
Vantage very cobbly loams complex, 3 to 15 percent slopes


muname:
Vantage very stony loams complex, 3 to 15 percent slopes


muname:
Vantage very stony loams complex, 15 to 30 percent slopes


muname:
Wanapum cobbly loam, 2 to 5 percent slopes


muname:
Wanapum complex, 10 to 15 percent slopes


muname:
Blint-Windry complex, 15 to 30 percent slopes


muname:
Caliralls-Clerf complex, 30 to 45 percent slopes


muname:
Caliralls-Horseflat complex, 15 to 30 percent slopes


muname:
Camaspatch very cobbly loam, 3 to 15 percent slopes


muname:
Camaspatch very cobbly loam, 15 to 30 percent slopes


muname:
Camaspatch very cobbly loam, thin, 3 to 15 percent slopes


muname:
Camaspatch very cobbly loam, thin, 15 to 30 percent slopes


muname:
Camaspatch-Colockum complex, 15 to 30 percent slopes


muname:
Camaspatch-Tanksel complex, 30 to 45 percent slopes


muname:
Camaspatch-Tanksel-Lainand complex, 45 to 60 percent slopes


muname:
Camaspatch-Whiskeydick complex, 3 to 15 percent slopes


muname:
Brehm-Gorskel-Gorst complex, 10 to 15 percent slopes


muname:
Caliralls silt loam, 10 to 15 percent slopes


muname:
Caliralls silt loam, 15 to 30 percent slopes


muname:
Caliralls-Clerf complex, 15 to 30 percent slopes


muname:
Whiskeydick very cobbly loam, 15 to 30 percent slopes


muname:
Whiskeydick very cobbly loam, 30 to 45 percent slopes


muname:
Whiskeydick-Tronsen-Camaspatch complex, 15 to 30 percent slopes


muname:
Whiskeydick-Tronsen-Camaspatch complex, 30 to 45 percent slopes


muname:
Whiskeydick-Tronsen-Camaspatch complex, 45 to 60 percent slopes


muname:
Winchester-Sagehill-Burbank complex, 5 to 30 percent slopes


muname:
Camaspatch-Whiskeydick complex, 15 to 30 percent slopes


muname:
Camaspatch-Whiskeydick complex, 30 to 45 percent slopes


muname:
Camaspatch-Whiskeydick complex, 45 to 60 percent slopes


muname:
Clerf very cobbly loam, 15 to 30 percent slopes


muname:
Clerf very cobbly loam, 30 to 45 percent slopes


muname:
Colockum silt loam, 5 to 10 percent slopes


muname:
Colockum silt loam, 10 to 15 percent slopes


muname:
Colockum silt loam, 15 to 30 percent slopes


muname:
Colockum-Tronsen complex, 3 to 15 percent slopes


muname:
Disage very cobbly loam, 3 to 15 percent slopes


muname:
Disage very cobbly loam, 15 to 30 percent slopes


muname:
Drino cobbly loam, 15 to 30 percent slopes


muname:
Drino very stony loam, 15 to 30 percent slopes


muname:
Drino-Disage-Kiona complex, 30 to 45 percent slopes


muname:
Drino-Rubble land-Rock outcrop complex, 30 to 75 percent slopes


muname:
Drino-Rubble land-Rock outcrop complex, 30 to 75 percent north slopes


muname:
Drino-Sohappy-Fortyday complex, 30 to 45 percent slopes


muname:
Drino-Sohappy-Fortyday complex, 45 to 60 percent slopes


muname:
Disage very stony loam, 30 to 45 percent slopes


muname:
Disage-Clenage complex, 15 to 30 percent slopes


muname:
Wipple cobbly clay loam, 3 to 15 percent slopes


muname:
Wipple cobbly clay loam, 15 to 30 percent slopes


muname:
Wipple cobbly clay loam, 30 to 45 percent slopes


muname:
Wockum silt loam, 15 to 30 percent slopes


muname:
Wockum silt loam, 30 to 45 percent slopes


muname:
Wockum-Blint complex, 15 to 30 percent slopes


muname:
Wockum-Blilt-Windry complex, 45 to 60 percent slopes


muname:
Zen-Benwy-Laric complex, 3 to 15 percent slopes


muname:
Zen-Marlic-Laric complex, 3 to 15 percent slopes


muname:
Argabak-Horseflat complex, 15 to 30 percent slopes


muname:
Argabak-Vantage complex, 3 to 15 percent slopes


muname:
Argabak-Whiskeydick complex, 3 to 15 percent slopes


muname:
Argabak-Whiskeydick complex, 15 to 30 percent slopes


muname:
Argabak-Windry complex, 3 to 15 percent slopes


muname:
Argabak-Zen-Grinrod complex, 3 to 15 percent slopes


muname:
Argabak-Zen-Grinrod complex, 15 to 30 percent slopes


muname:
Haploxerolls complex, 3 to 5 percent slopes


muname:
Benwy silt loam, 10 to 15 percent slopes


muname:
Benwy silt loam, 15 to 30 percent slopes


muname:
Benwy-Vantage-Argabak complex, 3 to 15 percent slopes


muname:
Benwy-Vantage-Argabak complex, 15 to 30 percent slopes


muname:
Blint very cobbly loam, 15 to 30 percent slopes


muname:
Blint very cobbly loam, 45 to 60 percent slopes


muname:
Niben-Vantage-Benwy complex, 15 to 30 percent slopes


muname:
Norod-Horseflat complex, 15 to 30 percent slopes


muname:
Norod-Horseflat complex, 30 to 45 percent slopes


muname:
Norod-Horseflat complex, 45 to 60 percent slopes


muname:
Norod-Ralock-Horseflat complex, 15 to 30 percent slopes


muname:
Norod-Ralock-Horseflat complex, 30 to 45 percent slopes


muname:
Norod-Ralock-Horseflat complex, 45 to 60 percent slopes


muname:
Norod-Rubble land complex, 30 to 75 percent slopes


muname:
Nosser-Levnik complex, 3 to 15 percent slopes


muname:
Nosser-Levnik complex, 15 to 30 percent slopes


muname:
Palerf-Ralock-Vantage complex, 15 to 30 percent slopes


muname:
Palerf-Vantage complex, 15 to 30 percent slopes


muname:
Palexerolls-Patron complex, 15 to 30 percent slopes


muname:
Patron-Camaspatch complex, 15 to 30 percent slopes


muname:
Prosser silt loam, 10 to 15 percent slopes


muname:
Prosser-Nevo complex, 3 to 15 percent slopes


muname:
Ralock silt loam, 15 to 30 percent slopes


muname:
Ralock silt loam, 30 to 45 percent slopes


muname:
Ralock-Horseflat complex, 15 to 30 percent slopes


muname:
Ralock-Palerf complex, 15 to 30 percent slopes


muname:
Ralock-Palerf complex, 30 to 45 percent slopes


muname:
Rollinger silt loam, 5 to 10 percent slopes


muname:
Rollinger silt loam, 10 to 15 percent slopes


muname:
Rollinger silt loam, 15 to 30 percent slopes


muname:
Rollinger silt loam, 30 to 45 percent slopes


muname:
Rollinger silt loam, 45 to 60 percent slopes


muname:
Rubble land-Rock outcrop complex, 60 to 120 percent slopes


muname:
Rubble land-Rock outcrop-Kiona complex, 60 to 120 percent slopes


muname:
Sagehill-Burbank-Malaga complex, 30 to 60 percent slopes


muname:
Selah silt loam, 10 to 15 percent slopes


muname:
Selah silt loam, 15 to 30 percent slopes


muname:
Sohappy-Fortyday complex, 3 to 15 percent slopes


muname:
Sohappy-Fortyday complex, 15 to 30 percent slopes


muname:
Sohappy-Fortyday complex, 30 to 45 percent slopes


muname:
Starbuck-Rock outcrop complex, 3 to 15 percent slopes


muname:
Tanskel-Patron-Camaspatch complex, 15 to 30 percent slopes


muname:
Tanksel-Patron-Camaspatch complex, 30 to 45 percent slopes


muname:
Tanksel-Wockum complex, 15 to 30 percent slopes


muname:
Tanksel-Wockum complex, 30 to 45 percent slopes


muname:
Tanksel-Wockum complex, 45 to 65 percent slopes


muname:
Terlan gravelly loam, 2 to 5 percent slopes


muname:
Terlan gravelly loam, 5 to 10 percent slopes


muname:
Terlan-Durtash-Selah complex, 2 to 5 percent slopes


muname:
Terlan-Durtash-Selah complex, 5 to 15 percent slopes


muname:
Timmerman complex, 2 to 5 percent slopes


muname:
Tronsen stony loam, 3 to 15 percent slopes


muname:
Tronsen stony loam, 15 to 30 percent slopes


muname:
Vantage extremely gravelly loam, 3 to 15 percent slopes


muname:
Vantage very cobbly loam, 3 to 15 percent slopes


muname:
Vantage very cobbly loam, 15 to 30 percent slopes


muname:
Vantage very cobbly loam, thin, 3 to 15 percent slopes


muname:
Vantage very cobbly loam, thin, 15 to 30 percent slopes


muname:
Vantage-Benwy-Argabak complex, 3 to 15 percent slopes


muname:
Vantage-Benwy-Argabak complex, 15 to 30 percent slopes


muname:
Vantage-Clerf complex, 3 to 15 percent slopes


muname:
Vantage-Clerf complex, 15 to 30 percent slopes


muname:
Vantage clerf complex, 30 to 45 percent slopes


muname:
Vantage-Clerf-Rubble land complex, 30 to 45 percent slopes


muname:
Vantage-Niben-Clerf complex, 3 to 15 percent slopes


muname:
Esquatzel-Aquolls-Weirman complex, channeled, 0 to 5 percent slopes


muname:
Esquatzel-Weirman complex, channeled, 0 to 2 percent slopes


muname:
Fortyday-Drino-Nevo complex, 15 to 30 percent slopes


muname:
Fortyday-Drino-Nevo complex, 30 to 45 percent slopes


muname:
Fortyday-Drino-Sohappy complex, 30 to 45 percent slopes


muname:
Fortyday-Nevo-Rock outcrop, 3 to 15 percent slopes


muname:
Fortyday-Rubble land-Rock outcrop complex, 45 to 70 percent slopes


muname:
Frint-Hogranch-Gidwin complex, 45 to 70 percent slopes


muname:
Frint-Gidwin-Rubble land complex, 45 to 70 percent slopes


muname:
Frint-Hogranch complex, 45 to 70 percent slopes


muname:
Grinrod-Horseflat complex, 15 to 30 percent slopes


muname:
Grinrod-Horseflat complex, 45 to 60 percent slopes


muname:
Haploxerolls-Orthents-Aquolls complex, channeled, 0 to 5 percent slopes


muname:
Horseflat very cobbly loam, 3 to 15 pecent slopes


muname:
Horseflat very cobbly loam, 15 to 30 percent slopes


muname:
Kiona very stony loam, 45 to 60 percent slopes


muname:
Kiona-Rubble land complex, 30 to 75 percent slopes


muname:
Lainand-Tanksel complex, 30 to 45 percent slopes


muname:
Laric very gravelly loam, 3 to 15 percent slopes


muname:
Laric-Zen complex, 3 to 15 percent slopes


muname:
Levnik-Nosser-Nevo complex, 3 to 15 percent slopes


muname:
Malaga gravelly sandy loam, 5 to 10 percent slopes


muname:
Malaga cobbly sandy loam, 3 to 15 percent slopes


muname:
Manastash-Durtash complex, 5 to 10 percent slopes


muname:
Manastash-Durtash complex, 15 to 30 percent slopes


muname:
Manastash-Meloza-Durtash complex, 15 to 30 percent slopes


muname:
Manastash-Selah-Gorst complex, 15 to 30 percent slopes


muname:
Rock Creek very stony silt loam, 0 to 30 percent slopes


muname:
Kiona stony silt loam, 15 to 45 percent slopes


muname:
Lickskillet very stony silt loam, 5 to 45 percent slopes


muname:
Starbuck-Rock outcrop complex, 0 to 45 percent slopes


muname:
Starbuck-Rock outcrop complex, 45 to 60 percent slopes


muname:
Bakeoven very cobbly silt loam, 0 to 30 percent slopes


muname:
Ritzville silt loam, 30 to 60 percent slopes


muname:
Ritzville silt loam, basalt substratum, 0 to 5 percent slopes


muname:
Ritzville silt loam, basalt substratum, 5 to 15 percent slopes


muname:
Ritzville silt loam, basalt substratum, 15 to 30 percent slopes


muname:
Ritzville variant silt loam, 5 to 15 percent slopes


muname:
Ritzville variant cobbly silt loam, 5 to 15 percent slopes


muname:
Rock Creek-Clint-Simcoe complex, 0 to 45 percent slopes


muname:
Sapkin very stony loam, 10 to 45 percent slopes


muname:
Sapkin very stony loam, 45 to 75 percent slopes


muname:
Sapkin-Rubbleland complex, 30 to 75 percent slopes


muname:
Saydab cobbly loam, 0 to 5 percent slopes


muname:
Scoon silt loam, 15 to 30 percent slopes


muname:
Scooteney silt loam, 2 to 5 percent slopes


muname:
Scooteney silt loam, 5 to 15 percent slopes


muname:
Scooteney cobbly silt loam, 0 to 5 percent slopes


muname:
Simcoe silt loam, 5 to 15 percent slopes


muname:
Simcoe silt loam, 15 to 30 percent slopes


muname:
Sinloc fine sandy loam, 0 to 2 percent slopes


muname:
Carmack cobbly loam, 25 to 50 percent slopes


muname:
Starbuck silt loam, 2 to 15 percent slopes


muname:
Sutkin stony loam, 0 to 25 percent slopes


muname:
Sutkin stony loam, 25 to 45 percent slopes


muname:
Sutkin stony loam, 45 to 65 percent slopes


muname:
Sutkin stony loam, 25 to 45 percent south slopes


muname:
Sutkin-Rock outcrop complex, 25 to 75 percent slopes


muname:
Carmack cobbly loam, 50 to 75 percent slopes


muname:
Sutkin variant stony loam, 0 to 5 percent slopes


muname:
Cleman very fine sandy loam, 2 to 5 percent slopes


muname:
Bocker-Jumpe complex, 0 to 15 percent slopes


muname:
Logy cobbly silt loam, 0 to 5 percent slopes


muname:
Loneridge stony loam, 0 to 25 percent slopes


muname:
Loneridge stony loam, 25 to 45 percent slopes


muname:
Loneridge stony loam, 25 to 45 percent north slopes


muname:
McDaniel very stony loam, 5 to 30 percent slopes


muname:
McDaniel very stony loam, 30 to 65 percent slopes


muname:
McDaniel-Rock Creek complex, 5 to 30 percent slopes


muname:
Meystre stony loam, 15 to 45 percent slopes


muname:
Mikkalo silt loam, 0 to 5 percent slopes


muname:
Bocker-Sapkin complex, 0 to 25 percent slopes


muname:
Mikkalo silt loam, 5 to 15 percent slopes


muname:
Mikkalo silt loam, 15 to 30 percent slopes


muname:
Moxee silt loam, 15 to 30 percent slopes


muname:
Moxee cobbly silt loam, 0 to 30 percent slopes


muname:
Naxing stony loam, 25 to 45 percent slopes


muname:
Naxing stony loam, 45 to 65 percent slopes


muname:
Bocker-Sutkin complex, 0 to 7 percent slopes


muname:
Odo cobbly silt loam, 5 to 35 percent slopes


muname:
Prosser silt loam, 0 to 15 percent slopes


muname:
Quincy loamy fine sand, 0 to 10 percent slopes


muname:
Renslow silt loam, 5 to 15 percent slopes


muname:
Renslow silt loam, basalt substratum, 0 to 5 percent slopes


muname:
Renslow silt loam, basalt substratum, 5 to 15 percent slopes


muname:
Cleman very fine sandy loam, 5 to 8 percent slopes


muname:
Cleman very fine sandy loam, 8 to 15 percent slopes


muname:
Clint very stony loam, 15 to 45 percent slopes


muname:
Clint-Rubbleland complex, 8 to 75 percent slopes


muname:
Cowiche-Rock Creek complex, 5 to 15 percent slopes


muname:
Darland stony loam, 45 to 75 percent slopes


muname:
Darland-Rubble land complex, 45 to 75 percent


muname:
Finley fine sandy loam, 0 to 5 percent slopes


muname:
Finley cobbly fine sandy loam, 0 to 5 percent slopes


muname:
Finley silt loam, 8 to 15 percent slopes


muname:
Gorskel very stony loam, 0 to 25 percent slopes


muname:
Gorskel-Harwood complex, 0 to 25 percent slopes


muname:
Gorst cobbly loam, 0 to 25 percent slopes


muname:
Bickleton silt loam, 5 to 20 percent slopes


muname:
Harwood-Burke-Wiehl silt loams, 2 to 5 percent slopes


muname:
Harwood-Burke-Wiehl silt loams, 5 to 8 percent slopes


muname:
Harwood-Burke-Wiehl silt loams, 8 to 15 percent slopes


muname:
Harwood-Burke-Wiehl silt loams, 15 to 30 percent slopes


muname:
Harwood-Burke-Wiehl silt loams, 30 to 60 percent slopes


muname:
Harwood-Burke-Wiehl very stony silt loams, 15 to 30 percent slopes


muname:
Harwood-Gorst complex, 0 to 25 percent slopes


muname:
Jumpe stony loam, 5 to 25 percent slopes


muname:
Bocker very cobbly loam, 0 to 25 percent slopes


muname:
Jumpe stony loam, 25 to 45 percent slopes


muname:
Jumpe stony loam, 45 to 65 percent slopes


muname:
Jumpe stony loam, 25 to 45 percent north slopes


muname:
Jumpe stony loam, 45 to 65 percent north slopes


muname:
Jumpe-Rock outcrop complex, 40 to 80 percent slopes


muname:
Lickskillet silt loam, 5 to 30 percent slopes


muname:
Taneum-Rock Creek complex, 5 to 15 percent slopes


muname:
Tekison stony loam, 0 to 25 percent slopes


muname:
Tieton fine sandy loam, 2 to 5 percent slopes


muname:
Carmack cobbly loam, 25 to 50 percent north slopes


muname:
Tieton-Rock outcrop complex, 0 to 30 percent slopes


muname:
Tumac very stony sandy loam, 5 to 45 percent slopes


muname:
Tumac very stony sandy loam, 45 to 65 percent slopes


muname:
Carmack-Rock outcrop complex, 40 to 70 percent slopes


muname:
Umapine silt loam, drained, 2 to 5 percent slopes


muname:
Warden fine sandy loam, 8 to 15 percent slopes


muname:
Cleman very fine sandy loam, 0 to 2 percent slopes


muname:
Willis fine sandy loam, 2 to 5 percent slopes


muname:
Billett sandy loam, 0 to 2 percent slopes


muname:
Kranski loamy sand, 6 to 12 percent slopes


muname:
Kranski loamy sand, 12 to 20 percent slopes


muname:
Mecan loamy sand, 6 to 12 percent slopes


muname:
Mecan loamy sand, 12 to 20 percent slopes


muname:
Mecan sandy loam, 6 to 12 percent slopes


muname:
Mecan sandy loam, 12 to 20 percent slopes


muname:
Meehan loamy sand, 0 to 3 percent slopes


muname:
Meehan loamy sand, sandstone substratum, 0 to 3 percent slopes


muname:
Meehan loamy sand, red surface, 0 to 3 percent slopes


muname:
Meehan fine sandy loam, gravelly variant


muname:
Mosinee sandy loam, 2 to 6 percent slopes


muname:
Norgo silt loam, moderately deep variant, 2 to 6 percent slopes


muname:
Norgo silt loam, moderately deep variant, 6 to 12 percent slopes


muname:
Plainbo loamy sand, 2 to 6 percent slopes


muname:
Plainfield loamy sand, 0 to 2 percent slopes


muname:
Plainfield loamy sand, 2 to 6 percent slopes


muname:
Coloma loamy sand, 2 to 6 percent slopes


muname:
Coloma loamy sand, 6 to 12 percent slopes


muname:
Dunnville very fine sandy loam, 2 to 6 percent slopes


muname:
Dunnville very fine sandy loam, mottled subsoil variant, 1 to 3 percent slopes


muname:
Friendship loamy sand, 0 to 3 percent slopes


muname:
Kranski loamy sand, 2 to 6 percent slopes


muname:
Plainfield loamy sand, 6 to 12 percent slopes


muname:
Plainfield loamy sand, granite substratum, 2 to 6 percent slopes


muname:
Plainfield sandy loam, gravelly variant, 2 to 6 percent slopes


muname:
Richford loamy sand, 0 to 2 percent slopes


muname:
Richford loamy sand, 2 to 6 percent slopes


muname:
Richford loamy sand, 6 to 12 percent slopes


muname:
Richford loamy fine sand, 2 to 6 percent slopes


muname:
Rockers loamy sand, 1 to 3 percent slopes


muname:
Roscommon-Meehan complex, 0 to 3 percent slopes


muname:
Roscommon sandy loam, loamy variant, loamy substratum


muname:
Rosholt sandy loam, 0 to 2 percent slopes


muname:
Rosholt sandy loam, 2 to 6 percent slopes


muname:
Rosholt sandy loam, 6 to 12 percent slopes, eroded


muname:
Rosholt loam, 6 to 12 percent slopes, eroded


muname:
Rosholt loam, loamy substratum, 0 to 2 percent slopes


muname:
Rosholt complex, 12 to 20 percent slopes


muname:
Rosholt complex, 20 to 40 percent slopes


muname:
Wyocena sandy loam, 2 to 6 percent slopes


muname:
Wyocena sandy loam, 6 to 12 percent slopes


muname:
Wyocena sandy loam, 12 to 20 percent slopes


muname:
Wyocena sandy loam, 20 to 30 percent slopes


muname:
Absted-Arvada-Bone complex, 0 to 6 percent slopes


muname:
Aeric Haplaquepts, 0 to 3 percent slopes


muname:
Bahl-Savageton complex, 0 to 6 percent slopes


muname:
Cambria-Cushman complex, 0 to 6 percent slopes


muname:
Cambria-Cushman complex, 6 to 15 percent slopes


muname:
Shingle-Theedle-Cambria association, 6 to 30 percent slopes


muname:
Silhouette-Heldt association, 0 to 6 percent slopes


muname:
Tassel-Shingle complex, 2 to 30 percent slopes


muname:
Tassel-Terro-Rock outcrop complex, 15 to 30 percent slopes


muname:
Tassel-Tullock-Vonalee association, 6 to 30 percent slopes


muname:
Terro-Tullock-Orpha complex, 0 to 6 percent slopes


muname:
Terro-Tullock-Orpha complex, 6 to 15 percent slopes


muname:
Theedle-Kishona loams, 0 to 6 percent slopes


muname:
Theedle-Kishona loams, 6 to 15 percent slopes


muname:
Ulm-Bidman complex, 0 to 6 percent slopes


muname:
Ulm-Renohill complex, 0 to 6 percent slopes


muname:
Ulm-Renohill clay loams, 6 to 15 percent slopes


muname:
Ustic Torriorthents, reclaimed, 3 to 30 percent slopes


muname:
Vonalee-Terro complex, 0 to 6 percent slopes


muname:
Vonalee-Terro complex, 6 to 15 percent slopes


muname:
Wibaux-Rock outcrop-Shingle complex, 6 to 45 percent slopes


muname:
Worf-Shingle-Tassel complex, 3 to 30 percent slopes


muname:
Zigweid-Bahl association, 0 to 6 percent slopes


muname:
Zigweid-Cambria association, 0 to 6 percent slopes


muname:
Zigweid-Cambria-Theedle association, 6 to 15 percent slopes


muname:
Arvada, thick surface-Arvada-Slickspots complex, 0 to 6 percent slopes


muname:
Embry-Orpha complex, 3 to 15 percent slopes


muname:
Forkwood-Cushman loams, 6 to 15 percent slopes


muname:
Keeline-Tullock-Niobrara, dry, complex, 3 to 30 percent slopes


muname:
Forkwood-Ulm loams, 0 to 6 percent slopes


muname:
Hiland-Bowbac fine sandy loams, 6 to 15 percent slopes


muname:
Hilight-Wags-Badland complex, 3 to 45 percent slopes


muname:
Samday-Shingle-Badland complex, 10 to 45 percent slopes


muname:
Shingle-Taluce complex, 3 to 30 percent slopes


muname:
Theedle-Kishona-Shingle loams, 3 to 30 percent slopes


muname:
Wibaux-Wibaux, thin solum complex, 6 to 40 percent slopes


muname:
Wibaux-Shingle-Badland complex, 6 to 60 percent slopes


muname:
Theedle-Kishona loams, 6 to 20 percent slopes


muname:
Renohill-Worfka clay loams, 3 to 15 percent slopes


muname:
Renohill-Shingle-Worf complex, 3 to 15 percent slopes


muname:
Shingle-Worf loams, 3 to 30 percent slopes


muname:
Forkwood-Cambria loams, 0 to 6 percent slopes


muname:
Absted-Arvada complex, 0 to 3 percent slopes


muname:
Clarkelen fine sandy loam, overflow, 0 to 3 percent slopes


muname:
Cushman-Forkwood loams, 0 to 6 percent slopes


muname:
Endoaquolls-Torrifluvents complex, 0 to 3 percent slopes


muname:
Forkwood-Cambria-Cushman loams, 6 to 15 percent slopes


muname:
Haverdad loam, overflow, 0 to 4 percent slopes


muname:
Kishona-Cambria loams, 0 to 6 percent slopes


muname:
Kishona-Cambria-Theedle loams, 6 to 15 percent slopes


muname:
Taluce-Shingle complex, 3 to 20 percent slopes


muname:
Taluce-Tullock-Rock outcrop complex, 3 to 45 percent slopes


muname:
Taluce-Turnercrest-Keeline fine sandy loams, 3 to 20 percent slopes


muname:
Hiland-Bowbac associaton, 6 to 15 percent slopes


muname:
Arvada-Absted-Slickspots complex, 0 to 6 percent slopes


muname:
Hiland-Bowbac fine sandy loams, 0 to 6 percent slopes


muname:
Ulm-Renohill clay loams, 0 to 6 percent slopes


muname:
Orpha-Tullock loamy sands, 6 to 30 percent slopes


muname:
Cushman-Worf loams, 3 to 15 percent slopes


muname:
Savageton-Silhouette clay loams, 0 to 6 percent slopes


muname:
Hiland-Bowbac sandy loams, thick surface, 0 to 6 percent slopes


muname:
Hiland-Bowbac complex, 0 to 10 percent slopes


muname:
Lohmiller-Haverdad complex, 1 to 4 percent slopes


muname:
Absted-Bone complex, 0 to 6 percent slopes


muname:
Parmleed-Renohill complex, 0 to 6 percent slopes


muname:
Samday-Shingle-Worf complex, northeast, 3 to 15 percent slopes


muname:
Forkwood-Cambria-Cushman loams, 0 to 12 percent slopes


muname:
Cambria variant-Forkwood variant complex, 0 to 6 percent slopes


muname:
Clarkelen-Draknab complex, 0 to 3 percent slopes


muname:
Clarkelen-Dwyer-Orpha association, 0 to 10 percent slopes


muname:
Clarkelen-Haverdad-Bigwinder complex, 0 to 3 percent slopes


muname:
Cushman-Terro complex, 0 to 6 percent slopes


muname:
Cushman-Terro complex, 6 to 15 percent slopes


muname:
Cushman-Worf association, 6 to 15 percent slopes


muname:
Dwyer-Orpha loamy sands, 3 to 15 percent slopes


muname:
Forkwood-Cambria fine sandy loams, 0 to 6 percent slopes


muname:
Forkwood-Cambria-Cushman complex, 6 to 15 percent slopes


muname:
Forkwood-Ulm complex, 0 to 6 percent slopes


muname:
Forkwood-Ulm-Renohill complex, 6 to 15 percent slopes


muname:
Gateridge-Blacksheep association, 10 to 45 percent slopes


muname:
Haverdad-Lohmiller complex, 0 to 6 percent slopes


muname:
Hiland-Bowbac sandy loams, 0 to 6 percent slopes


muname:
Hiland-Bowbac complex, 6 to 15 percent slopes


muname:
Keeline-Tassel-Turnback complex, 6 to 15 percent slopes


muname:
Kishona-Dwyer-Orpha association, 0 to 10 percent slopes


muname:
Orella-Rock outcrop-Samday complex, 3 to 30 percent slopes


muname:
Renohill-Worfka-Shingle complex, 0 to 6 percent slopes


muname:
Renohill-Worfka-Shingle complex, 6 to 15 percent slopes


muname:
Samday-Shingle-Worf complex, 3 to 15 percent slopes


muname:
Sear-Wibaux complex, 0 to 15 percent slopes


muname:
Shingle-Badland-Samday complex, 10 to 30 percent slopes


muname:
Shingle, thin solum-Rock outcrop-Tassel,thin solum complex, cool, 6 to 45 percent slopes


muname:
Theedle-Shingle-Kishona complex, 6 to 40 percent slopes, gullied


muname:
Zigweid-Theedle loams, 3 to 15 percent slopes


muname:
Bayard fine sandy loam, 0 to 15 percent slopes


muname:
Blazon-Trimad complex, 15 to 45 percent slopes


muname:
Boyle, thin solum-Breece-Cathedral complex, 0 to 30 percent slopes


muname:
Poposhia-Blazon, thin solum-Rock outcrop complex, 5 to 35 percent slopes


muname:
Rock outcrop-Blazon, thin solum, complex, 30 to 60 percent slopes


muname:
Trimad-Evanston complex, 3 to 30 percent slopes


muname:
Trimad-Weed-Blazon association, 0 to 15 percent slopes


muname:
Valent loamy fine sand, moist, 0 to 6 percent slopes


muname:
Aberone-Cragola complex, 10 to 30 percent slopes


muname:
Alice-Bayard fine sandy loams, 0 to 6 percent slopes


muname:
Aberone gravelly sandy loam, 0 to 15 percent slopes


muname:
Alice-Phiferson fine sandy loams, 3 to 10 percent slopes


muname:
Alice-Recluse-Cedak fine sandy loams, 0 to 6 percent slopes


muname:
Bayard-Phiferson-Treon, thin solum complex, 0 to 6 percent slopes


muname:
Bayard-Phiferson-Treon, thin solum complex, 3 to 45 percent slopes


muname:
Blackhall-Satanka-Rock outcrop complex, 5 to 20 percent slopes


muname:
Bonjea-Chugcreek-Rock outcrop complex, 3 to 15 percent slopes


muname:
Bonjea-Rock outcrop-Chugcreek complex, 15 to 40 percent slopes


muname:
Boyle-Boyle, thin solum gravelly loams, 3 to 6 percent slopes


muname:
Boyle-Lininger association, 1 to 15 percent slopes


muname:
Boyle-Rock outcrop complex, 5 to 25 percent slopes


muname:
Brown-Featherlegs-Recluse complex, 5 to 40 percent slopes


muname:
Byrnie-Byrnie, thin solum-Rock outcrop complex, 5 to 45 percent slopes


muname:
Byrnie-Coocreek-Byrnie, thin solum complex, 0 to 15 percent slopes


muname:
Cascajo-Taluce-Rock outcrop complex, 6 to 40 percent slopes


muname:
Cathedral-Spinekop-Rock outcrop complex, 0 to 40 percent slopes


muname:
Cedak-Bayard-Treon, thin solum, complex, 0 to 6 percent slopes


muname:
Mitchell very fine sandy loam, 0 to 6 percent slopes


muname:
Mitchell very fine sandy loam, 6 to 10 percent slopes


muname:
Moskee sandy loam, 0 to 6 percent slopes


muname:
Taluce-Rock outcrop-Turnercrest complex, moist, 6 to 50 percent slopes


muname:
Taluce-Taluce, thin solum-Rock outcrop complex, 3 to 30 percent slopes


muname:
Taluce-Turnercrest sandy loams, 0 to 6 percent slopes


muname:
Treon-Alice-Phiferson complex, 0 to 6 percent slopes


muname:
Treon-Rock outcrop complex, 6 to 60 percent slopes


muname:
Treon, thin solum-Phiferson-Keeline fine sandy loams, 0 to 6 percent slopes


muname:
Trimad-Blazon-Rock outcrop complex, 3 to 40 percent slopes


muname:
Turnercrest-Phiferson-Taluce complex, 0 to 6 percent slopes


muname:
Typic Calciaquolls-Whetsoon fine sandy loams, 0 to 3 percent slopes


muname:
Tyzak-Tyzak, thin solum-Rock outcrop complex, 8 to 50 percent slopes


muname:
Vetal fine sandy loam, 3 to 9 percent slopes


muname:
Vetal-Julesburg fine sandy loams, 0 to 6 percent slopes


muname:
Orpha-Tullock loamy fine sands, 6 to 20 percent slopes


muname:
Phiferson-Alice, bedrock substratum, very fine sandy loams, 0 to 6 percent slopes


muname:
Phiferson-Mainter fine sandy loams, 0 to 6 percent slopes


muname:
Phiferson-Treon complex, 0 to 6 percent slopes


muname:
Poposhia-Chaperton association, 6 to 12 percent slopes


muname:
Poposhia-Forelle complex, 1 to 8 percent slopes


muname:
Quarterback, thick surface-Albinas complex, 0 to 3 percent slopes


muname:
Recluse fine sandy loam, 3 to 6 percent slopes


muname:
Recluse-Albinas-Treon, thin solum, complex, 0 to 6 percent slopes


muname:
Recluse-Cedak loams, 0 to 6 percent slopes


muname:
Recluse-Cedak loams, 6 to 10 percent slopes


muname:
Recluse-Graystone very fine sandy loams, 0 to 6 percent slopes


muname:
Recluse-Nuncho loams, 0 to 10 percent slopes


muname:
Rentsac-Brownsto-Ipson complex, 10 to 45 percent slopes


muname:
Rock outcrop-Bonjea complex, 40 to 60 percent slopes


muname:
Rock outcrop-Cathedral complex, 20 to 40 percent slopes


muname:
Rock outcrop-Cathedral-Alderon complex, 25 to 50 percent slopes


muname:
Selpats fine sandy loam, 0 to 3 percent slopes


muname:
Selpats-Forkwood loams, 0 to 3 percent slopes


muname:
Selpats-Hiland complex, 0 to 6 percent slopes


muname:
Snilloc-Chugcity complex, 0 to 6 percent slopes


muname:
Snilloc-Recluse complex, 0 to 6 percent slopes


muname:
Spearfish-Sixmile-Rock outcrop complex, 5 to 45 percent slopes


muname:
Storsun-Sunup-Rock outcrop complex, 3 to 50 percent slopes


muname:
Sunup-Rock outcrop complex, 10 to 40 percent slopes


muname:
Sunup-Snavee-Rock outcrop complex, 0 to 30 percent slopes


muname:
Sweatbee fine sandy loam, 0 to 3 percent slopes


muname:
Sweatbee fine sandy loam, wet, 0 to 3 percent slopes


muname:
Sweatbee-Numa sandy clay loams, 0 to 3 percent slopes


muname:
Taluce, thin solum-Rock outcrop complex, 10 to 60 percent slopes


muname:
Taluce, thin solum-Keeline complex, 6 to 50 percent slopes


muname:
Taluce, thin solum-Rock outcrop-Turnercrest complex, 6 to 50 percent slopes


muname:
Taluce-Rock outcrop-Turnercrest complex, 6 to 50 percent slopes


muname:
Cedak-Recluse very fine sandy loams, 0 to 6 percent slopes


muname:
Cedak-Recluse-Treon very fine sandy loams, 0 to 6 percent slopes


muname:
Cedak-Treon fine sandy loams, 0 to 6 percent slopes


muname:
Chaperton, moderately saline-Blazon complex, 8 to 20 percent slopes


muname:
Claprych gravelly fine sandy loam, 0 to 3 percent slopes


muname:
Claprych-Luman very gravelly sandy loams, 0 to 10 percent slopes


muname:
Claprych-Selpats sandy clay loams, 0 to 3 percent slopes


muname:
Claprych-Sweatbee complex, 3 to 20 percent slopes


muname:
Clarkelen-Quarterback very fine sandy loams, 0 to 3 percent slopes


muname:
Clarkelen, wet-Anvil loams, 0 to 3 percent slopes


muname:
Coaliams-Haverdad complex, 0 to 3 percent slopes


muname:
Creighton very fine sandy loam, 0 to 6 percent slopes


muname:
Curabith very cobbly sandy loam, 0 to 6 percent slopes


muname:
Cushool-Cutback complex, 2 to 10 percent slopes


muname:
Dalecreek-Kovich complex, 0 to 9 percent slopes


muname:
Deight-Thirtynine-Glendo very fine sandy loams, 0 to 6 percent slopes


muname:
Diamonkit-Stylite sandy loams, 3 to 15 percent slopes


muname:
Embry loamy fine sand, 2 to 10 percent slopes


muname:
Evanston-Ipson complex, 0 to 20 percent slopes


muname:
Evanston-Ipson-Brownsto complex, 15 to 45 percent slopes


muname:
Featherlegs fine sandy loam, wet, 0 to 3 percent slopes


muname:
Featherlegs-Bayard fine sandy loams, 0 to 6 percent slopes


muname:
Featherlegs-Curabith fine sandy loams, 0 to 3 percent slopes


muname:
Featherlegs-Greenhope-Curabith fine sandy loams, 3 to 15 percent slopes


muname:
Featherlegs-Recluse loams, 0 to 3 percent slopes


muname:
Featherlegs-Recluse loams, 3 to 6 percent slopes


muname:
Cowestglen fine sandy loam, 0 to 3 percent slopes


muname:
Evanston-Weed complex, 3 to 35 percent slopes


muname:
Evanston-Weed-Trimad loams, 3 to 15 percent slopes


muname:
Ipson-Evanston-Rock outcrop complex, 0 to 30 percent slopes


muname:
Poposhia silt loam, 0 to 6 percent slopes


muname:
Poposhia-Blazon silt loams, 3 to 30 percent slopes


muname:
Vetal-Treon-Phiferson complex, 3 to 20 percent slopes


muname:
Vonalee fine sandy loam, 0 to 6 percent slopes


muname:
Wendover-Rock outcrop complex, 10 to 60 percent slopes


muname:
Wagonhound-Selpats complex, 3 to 20 percent slopes


muname:
Taluce-Taluce, thin solum-Turnercrest fine sandy loams, 3 to 15 percent slopes


muname:
Taluce-Treon complex, thin solums, 6 to 10 percent slopes


muname:
Moskee fine sandy loam, 0 to 3 percent slopes


muname:
Featherlegs-Recluse loams, 3 to 15 percent slopes


muname:
Fluvaquentic Endoaquolls-Whetsoon complex, 0 to 3 percent slopes


muname:
Forelle-Diamondville association, 3 to 15 percent slopes


muname:
Forkwood fine sandy loam, 0 to 3 percent slopes


muname:
Forkwood loam, wet, 0 to 3 percent slopes


muname:
Graystone-Alice fine sandy loams, 0 to 6 percent slopes


muname:
Graystone-Greenhope-Bayard fine sandy loams, 0 to 10 percent slopes


muname:
Graystone-Mainter fine sandy loams, 0 to 6 percent slopes


muname:
Graystone-Phiferson-Treon very fine sandy loams, 0 to 6 percent slopes


muname:
Greenhope-Featherlegs complex, 0 to 6 percent slopes


muname:
Hiland fine sandy loam, 0 to 3 percent slopes


muname:
Hiland-Cambria sandy loams, 0 to 6 percent slopes


muname:
Jayem-Mainter-Moskee fine sandy loams, 0 to 6 percent slopes


muname:
Julesburg-Jayem-Phiferson fine sandy loams, 0 to 6 percent slopes


muname:
Keeline fine sandy loam, 0 to 3 percent slopes


muname:
Keeline fine sandy loam, 3 to 6 percent slopes


muname:
Keeline fine sandy loam, 6 to 10 percent slopes


muname:
Keeline-Mainter very fine sandy loams, 0 to 6 percent slopes


muname:
Keeline-Nidix-Taluce complex, 10 to 60 percent slopes


muname:
Keeline-Taluce-Turnercrest fine sandy loams, 3 to 40 percent slopes


muname:
Keeline-Turnercrest fine sandy loams, 0 to 6 percent slopes


muname:
Keeline-Turnercrest fine sandy loams, 6 to 10 percent slopes


muname:
Kishona clay loam, 0 to 6 percent slopes


muname:
Livan-Clarkelen complex, 0 to 3 percent slopes


muname:
Livan-Riverwash complex, 0 to 3 percent slopes


muname:
Mainter fine sandy loam, 0 to 6 percent slopes


muname:
Mainter fine sandy loam, wet, 0 to 3 percent slopes


muname:
Mainter-Keeline fine sandy loams, 6 to 10 percent slopes


muname:
McFadden gravelly fine sandy loam, 1 to 6 percent slopes


muname:
MORTON-CHAMA SILT LOAMS, SLOPING, ERODED


muname:
MORTON AND FARLAND CLAY LOAMS, GENTLY SLOPING


muname:
MORTON AND FARLAND SILT LOAMS, GENTLY SLOPING


muname:
REGENT-MOREAU SILTY CLAY LOAMS, GENTLY SLOPING


muname:
RHOADES AND BELFIELD SOILS, GENTLY SLOPING


muname:
VEBAR-FLASHER FINE SANDY LOAMS, STRONGLY SLOPING


muname:
VEBAR-PARSHALL FINE SANDY LOAMS, UNDULATING


muname:
VEBAR-PARSHALL FINE SANDY LOAMS, SLOPING


muname:
BELFIELD-RHOADES SILTY CLAY LOAMS, LEVEL


muname:
BELFIELD-RHOADES SILTY CLAY LOAMS, GENTLY SLOPING


muname:
FARLAND, ARNEGARD AND GRAIL SILT LOAMS, LEVEL


muname:
GRAIL-RHOADES SILTY CLAY LOAMS, GENTLY SLOPING


muname:
LEFOR FINE SANDY LOAM, UNDULATING, ERODED


muname:
LITTLE HORN AND DUNCOM SOILS, GENTLY SLOPING


muname:
MOREAU-MIDWAY SILTY CLAYS, STRONGLY SLOPING


muname:
HAMERLY, VALLERS, AND COLVIN SOILS, SALINE, 0 TO 3 PERCENT SLOPES


muname:
HAMERLY-WYARD LOAMS, 0 TO 3 PERCENT SLOPES


muname:
HAMERLY-SVEA LOAMS, 0 TO 3 PERCENT SLOPES


muname:
CAVOUR-MIRANDA LOAMS, 0 TO 3 PERCENT SLOPES


muname:
MINNEWAUKAN LOAMY SAND, LOAMY SUBSTRATUM, 0 TO 3 PERCENT SLOPES


muname:
OVERLY-BEARDEN SILTY CLAY LOAMS, 0 TO 3 PERCENT SLOPES


muname:
GREAT BEND-OVERLY SILTY CLAY LOAMS, 3 TO 6 PERCENT SLOPES


muname:
SINAI SILTY CLAY LOAM, 0 TO 6 PERCENT SLOPES


muname:
SEELYEVILLE MUCKY PEAT, 0 TO 9 PERCENT SLOPES


muname:
LA PRAIRIE SILT LOAM, 0 TO 3 PERCENT SLOPES


muname:
BARNES-SVEA LOAMS, 3 TO 6 PERCENT SLOPES


muname:
BARNES-BUSE LOAMS, 6 TO 9 PERCENT SLOPES


muname:
BARNES-BUSE LOAMS, 9 TO 15 PERCENT SLOPES


muname:
BUSE-SVEA LOAMS, 15 TO 50 PERCENT SLOPES


muname:
SVEA-BARNES LOAMS, 0 TO 3 PERCENT SLOPES


muname:
BARNES-SVEA-BUSE LOAMS, 9 TO 25 PERCENT SLOPES


muname:
BARNES-BUSE-PARNELL COMPLEX, 0 TO 35 PERCENT SLOPES


muname:
SIOUX-BARNES LOAMS, 9 TO 30 PERCENT SLOPES


muname:
KLOTEN-BUSE LOAMS, 9 TO 50 PERCENT SLOPES


muname:
HAMERLY-PARNELL COMPLEX, 0 TO 3 PERCENT SLOPES


muname:
DIVIDE-MARYSLAND LOAMS, 0 TO 3 PERCENT SLOPES


muname:
FORDVILLE-RENSHAW LOAMS, 0 TO 3 PERCENT SLOPES


muname:
FORDVILLE-RENSHAW LOAMS, 3 TO 6 PERCENT SLOPES


muname:
ARVILLA-SIOUX SANDY LOAMS, 0 TO 3 PERCENT SLOPES


muname:
SIOUX-ARVILLA SANDY LOAMS, 1 TO 9 PERCENT SLOPES


muname:
SIOUX-ARVILLA SANDY LOAMS, 9 TO 35 PERCENT SLOPES


muname:
RENSHAW-SIOUX LOAMS, 0 TO 6 PERCENT SLOPES


muname:
MADDOCK LOAMY FINE SAND, 0 TO 6 PERCENT SLOPES


muname:
MADDOCK LOAMY FINE SAND, 6 TO 15 PERCENT SLOPES


muname:
WYNDMERE FINE SANDY LOAM, 0 TO 3 PERCENT SLOPES


muname:
HAMERLY-TONKA COMPLEX, 0 TO 3 PERCENT SLOPES


muname:
HECLA-ULEN COMPLEX, 0 TO 3 PERCENT SLOPES


muname:
HECLA-TOWNER LOAMY FINE SANDS, 1 TO 6 PERCENT SLOPES


muname:
TOWNER LOAMY FINE SAND, 0 TO 3 PERCENT SLOPES


muname:
SWENODA FINE SANDY LOAM, 0 TO 3 PERCENT SLOPES


muname:
SWENODA-BUSE COMPLEX, 3 TO 6 PERCENT SLOPES


muname:
SWENODA-BUSE COMPLEX, 6 TO 9 PERCENT SLOPES


muname:
EMBDEN FINE SANDY LOAM, 0 TO 6 PERCENT SLOPES


muname:
CLONTARF FINE SANDY LOAM, 0 TO 6 PERCENT SLOPES


muname:
HAMERLY-CRESBARD LOAMS, 0 TO 3 PERCENT SLOPES


muname:
SWENODA-LARSON FINE SANDY LOAMS, 1 TO 6 PERCENT SLOPES


muname:
SVEA-CRESBARD LOAMS, 0 TO 3 PERCENT SLOPES


muname:
BARNES-CRESBARD LOAMS, 3 TO 6 PERCENT SLOPES


muname:
CRESBARD-CAVOUR LOAMS, 0 TO 3 PERCENT SLOPES


muname:
Christianburg clay, 3 to 5 percent slopes


muname:
Christianburg sandy loam, 0 to 3 percent slopes


muname:
Eastonville loamy sand, 0 to 3 percent slopes


muname:
Eastonville loamy sand, 3 to 5 percent slopes


muname:
Kutch clay, 5 to 15 percent slopes, severely eroded


muname:
Nunn loam, 3 to 5 percent slopes, severely eroded


muname:
Platner-Ascalon sandy loams, 0 to 3 percent slopes


muname:
Platner-Ascalon sandy loams, 3 to 5 percent slopes


muname:
Renohill complex, 3 to 15 percent slopes, eroded


muname:
Slickspot-Kutch complex, 3 to 9 percent slopes


muname:
Slickspot-Kutch complex, 3 to 9 percent slopes, severely eroded


muname:
Stoneham sandy loam, 1 to 5 percent slopes


muname:
Stoneham sandy loam, 5 to 18 percent slopes


muname:
Stoneham complex, 1 to 5 percent slopes, eroded


muname:
Terry fine sandy loam, 5 to 20 percent slopes


muname:
Terry-Vebar-Tullock complex, 5 to 25 percent slopes


muname:
Truckton sandy loam, 1 to 3 percent slopes


muname:
Truckton sandy loam, 3 to 5 percent slopes


muname:
Truckton sandy loam, 5 to 20 percent slopes


muname:
Truckton, Bresser, and Blakeland soils, 5 to 20 percent slopes, eroded


muname:
Ulm loam, 5 to 12 percent slopes, severely eroded


muname:
Ulm-Beckton complex, 3 to 9 percent slopes


muname:
Ulm-Beckton complex, 9 to 15 percent slopes, severely eroded


muname:
Vebar loamy fine sand, 3 to 5 percent slopes


muname:
Vebar loamy fine sand, 5 to 20 percent slopes


muname:
Wiley and Colby soils, 3 to 5 percent slopes


muname:
Wiley and Colby soils, 5 to 18 percent slopes


muname:
Arvada complex, 0 to 3 percent slopes, eroded


muname:
Ascalon sandy loam, 9 to 15 percent slopes


muname:
Ascalon complex, 1 to 3 percent slopes, eroded


muname:
Ascalon complex, 3 to 5 percent slopes, eroded


muname:
Baca complex, 5 to 15 percent slopes, eroded


muname:
Bresser sandy loam, 1 to 3 percent slopes


muname:
Bresser sandy loam, 3 to 5 percent slopes


muname:
Bresser sandy loam, 5 to 9 percent slopes


muname:
Bresser sandy loam, 9 to 15 percent slopes


muname:
Bresser complex, 3 to 5 percent slopes, eroded


muname:
Bresser-Truckton-Blakeland complex, 3 to 9 percent slopes


muname:
Christianburg clay, 0 to 3 percent slopes


muname:
Christianburg clay, 0 to 3 percent slopes, severely eroded


muname:
Adena-Colby fine sandy loams, 1 to 5 percent slopes


muname:
Adena-Colby fine sandy loams, 5 to 9 percent slopes


muname:
Adena-Colby silt loams, 1 to 5 percent slopes


muname:
Adena-Colby silt loams, 5 to 9 percent slopes


muname:
Baca-Thedalund loams, 3 to 9 percent slopes


muname:
Bijou sandy loam, wet, 0 to 3 percent slopes


muname:
Blakeland loamy sand, 1 to 9 percent slopes, eroded


muname:
Blakeland loamy sand, 1 to 20 percent slopes


muname:
Bresser loamy sand, terrace, 0 to 3 percent slopes


muname:
Bresser sandy loam, terrace, 0 to 3 percent slopes


muname:
Bresser loam, gravelly subsoil variant, 1 to 3 percent slopes


muname:
Bresser-Stapleton sandy loams, 3 to 9 percent slopes


muname:
Bresser-Stapleton sandy loams, 9 to 20 percent slopes


muname:
Bresser-Truckton sandy loams, 3 to 5 percent slopes


muname:
Bresser-Truckton sandy loams, 5 to 20 percent slopes


muname:
Bresser and Truckton soil, 3 to 9 slopes, eroded


muname:
Colby and Adena soils, 1 to 9 percent slopes, eroded


muname:
Fondis-Ascalon, gravelly subsoil variant, complex, 1 to 9 percent slopes


muname:
Fondis-Colby silt loams, 3 to 5 percent slopes


muname:
Heldt clay, saline, 0 to 3 percent slopes


muname:
Litle silty clay loam, 1 to 9 percent slopes


muname:
Litle-Samsil, gypsum, silty clay loams, 3 to 9 percent slopes


muname:
Nunn-Bresser-Ascalon complex, 0 to 3 percent slopes


muname:
Olney fine sandy loam, 5 to 9 percent slopes


muname:
Renohill loam,reddish variant, 5 to 20 percent slopes


muname:
Renohill-Buick loams, 3 to 9 percent slopes


muname:
Renohill-Buick loams, 9 to 20 percent slopes


muname:
Renohill-Buick complex, 5 to 20 percent slopes, eroded


muname:
Renohill-Litle clay loams, 3 to 9 percent slopes


muname:
Renohill-Litle-Thedalund complex, 9 to 30 percent slopes


muname:
Samsil clay, gypsum, 5 to 20 percent slopes


muname:
Samsil-Litle stony clays, 20 to 50 percent slopes


muname:
Samsil-Renohill clay loams, 3 to 20 percent slopes


muname:
Stapleton sandy loam, 9 to 30 percent slopes


muname:
Terry-Olney-Thedalund sandy loams, 5 to 20 percent slopes


muname:
Thedalund clay loam, 9 to 20 percent slopes


muname:
Thedalund clay loam, 9 to 20 percent slopes, eroded


muname:
Truckton loamy sand, 1 to 5 percent slopes


muname:
Truckton loamy sand, 5 to 20 percent slopes


muname:
Weld fine sandy loam, 1 to 5 percent slopes


muname:
Weld-Deertrail silt loams, 0 to 3 percent slopes


muname:
Stoneham-Harvey loams, 0 to 5 percent slopes


muname:
Vona-Otero sandy loams, 3 to 9 percent slopes


muname:
Bead fine sandy loam, 10 to 50 percent slopes


muname:
Glenberg sandy loam, 0 to 1 percent slopes


muname:
Kornman sandy clay loam, clay substratum variant, 0 to 1 percent slopes


muname:
Kornman sandy clay loam, clay substratum, 1 to 3 percent slopes


muname:
Limon clay, alkali, 0 to 1 percent slopes


muname:
Limon clay, alkali, 1 to 3 percent slopes


muname:
Litle-Ordway clays, 1 to 5 percent slopes


muname:
Manzanola clay loam, 0 to 1 percent slopes


muname:
Neesopah sandy clay loam, 0 to 1 percent slopes


muname:
Neesopah sandy clay loam, 1 to 3 percent slopes


muname:
Neesopah sandy clay loam, wet, 1 to 3 percent slopes


muname:
Nepesta loam, clay substratum variant, 0 to 1 percent slopes


muname:
Olney soils, 0 to 3 percent slopes, eroded


muname:
Otero-Ordway sandy loams, 1 to 9 percent slopes


muname:
Rocky Ford clay loam, 0 to 2 percent slopes


muname:
Shingle silty clay loam, 0 to 5 percent slopes


muname:
Bosler sandy loam, 1 to 8 percent slopes


muname:
Carbol very rocky sandy loam, 15 to 60 percent slopes


muname:
Corpening fine sandy loam, 5 to 40 percent slopes


muname:
Curecanti gravelly loam, 1 to 8 percent slopes


muname:
Dollard silty clay loam, 5 to 30 percent slopes


muname:
Duffson-Corpening loams, 5 to 35 percent slopes


muname:
Duffson-Spring creek stony loams, 5 to 40 percent slopes


muname:
Fola cobbly sandy loam, 1 to 8 percent slopes


muname:
Gas Creek sandy loam, 0 to 1 percent slopes


muname:
Gas Creek sandy loam, 1 to 5 percent slopes


muname:
Gateview cobbly loam, 2 to 8 percent slopes


muname:
Gateview cobbly loam, 8 to 30 percent slopes


muname:
Gold Creek silty clay loam, 0 to 5 percent slopes


muname:
Kezar-Cathedral gravelly sandy loams, 5 to 35 percent slopes


muname:
Leaps silty clay loam, 5 to 30 percent slopes


muname:
Lucky-Cheadle gravelly sandy loams, 5 to 45 percent slopes


muname:
Meredith very stony loam, 8 to 50 percent slopes


muname:
Morop stony loam, 5 to 40 percent slopes


muname:
Nutras stony loam, 10 to 50 percent slopes


muname:
Parlin-Hopkins channery loams, 5 to 45 percent slopes


muname:
Parlin-Mergel gravelly loams. 5 to 45 percent slopes


muname:
Posant very rocky loam, 10 to 60 percent slopes


muname:
Redcloud channery loam, 3 to 30 percent slopes


muname:
Ruby gravelly sandy loam, 5 to 30 percent slopes


muname:
Ruby extremely rocky sandy loam, 5 to 40 percent slopes


muname:
Shule and sapinero loams, 10 to 50 percent slopes


muname:
Tongue River loam, 10 to 50 percent slopes


muname:
Uinta and tolvar soils, 10 to 50 percent slopes


muname:
Vulcan gravelly sandy loam, 10 to 35 percent slopes


muname:
Wetterhorn stony loam, 10 to 55 percent slopes


muname:
Woodhall extremely rocky loam, 5 to 50 percent slopes


muname:
Woosley very rocky loam, 10 to 60 percent slopes


muname:
Youman-Leaps loams, 5 to 35 percent slopes


muname:
Youman-Passar loams, 5 to 30 percent slopes


muname:
Falcon-Trag families complex, 5 to 40 percent slopes, extremely stony


muname:
Tecolote very gravelly sandy loam, 15 to 40 percent slopes


muname:
Herm family, 5 to 25 percent slopes, very stony


muname:
Ring family, 40 to 60 percent slopes, rubbly


muname:
Merino family-Rock outcrop complex, 40 to 150 percent slopes, extremely bouldery


muname:
Hechtman-Guffey families complex, 40 to 60 percent slopes, extremely bouldery


muname:
Cathedral family, moist-Rock outcrop complex, 40 to 150 percent slopes, rubbly


muname:
Hechtman-Ashcroft families complex, 5 to 25 percent slopes, extremely bouldery


muname:
Cascajo very gravelly sandy loam, 5 to 25 percent slopes


muname:
Cascajo-Shale outcrop complex, 5 to 30 percent slopes


muname:
Gilcrest sandy loam, 0 to 2 percent slopes


muname:
Gilcrest gravelly sandy loam, 3 to 9 percent slopes


muname:
Heldt silty clay loam, 2 to 6 percent slopes


muname:
Holderness silt loam, 3 to 9 percent slopes


muname:
Laporte channery loam, 3 to 25 percent slopes


muname:
Larkson stony loam, 5 to 20 percent slope


muname:
Limon silty clay loam, 0 to 2 percent slopes


muname:
Limon silty clay loam, 2 to 5 percent slopes


muname:
Limon silty clay, 0 to 5 percent slopes,gullied


muname:
Manzanola clay loam, 2 to 9 percent slopes


muname:
Manzanola silty clay loam, 0 to 2 percent slopes


muname:
Midway-Shale outcrop complex, 1 to 9 percent slopes


muname:
Nederland stony sandy loam, 9 to 25 percent slopes


muname:
Neville sandy loam, 3 to 9 percent slopes


muname:
Otero gravelly sandy loam, 3 to 9 percent slopes


muname:
Penrose-Minnequa complex, 1 to 15 percent slopes


muname:
Penrose-Rock outcrop complex, 25 to 65 percent slopes


muname:
Rocky Ford silty clay loam, 0 to 1 percent slopes


muname:
Rocky Ford silty clay loam, 1 to 3 percent slopes


muname:
Shingle silty clay loam, 1 to 9 percent slopes


muname:
Stroupe extremely stony loam, 9 to 25 percent slopes


muname:
Travessilla sandy loam, 1 to 9 percent slopes


muname:
Travessilla-Rock outcrop complex, 30 to 90 percent slopes


muname:
Vamer-Rock outcrop complex, 5 to 25 percent slopes


muname:
Akela very gravelly loam, 0 to 10 percent slopes


muname:
Akela very gravelly loam, 10 to 25 percent slopes


muname:
Bluepoint loamy sand, 3 to 10 percent slopes


muname:
Brenda gravelly clay loam, 10 to 25 percent slopes


muname:
Bluepoint loamy sand, 0 to 3 percent slopes


muname:
Bluepoint loamy sand, 0 to 3 percent slopes, hummocky


muname:
Eba very gravelly clay loam, 0 to 10 percent slopes


muname:
Graham cobbly clay loam, 10 to 25 percent slopes


muname:
Ledru gravelly clay loam, 10 to 25 percent slopes


muname:
Lehmans very rocky loam, 0 to 10 percent slopes


muname:
Lehmans extremely rocky loam, 10 to 25 percent slopes


muname:
Lozier extremely rocky loam, 0 to 10 percent slopes


muname:
Mohave sandy clay loam, 0 to 3 percent slopes


muname:
Mimbres silty clay loam, sandy subsoil variant


muname:
Mohave sandy loam, 0 to 1 percent slopes


muname:
Mohave sandy clay loam, 0 to 1 percent slopes


muname:
Nickel very gravelly sandy loam, 3 to 9 percent slopes


muname:
Simona loamy sand, 0 to 5 percent slopes


muname:
Stellar silty clay loam, 0 to 1 percent slopes


muname:
Tres Hermanos gravelly loam, 1 to 5 percent slopes


muname:
Upton gravelly sandy loam, 3 to 10 percent slopes


muname:
Upton gravelly loam, 0 to 10 percent slopes


muname:
Alamogordo very fine sandy loam, 0 to 3 percent slopes


muname:
Alamogordo silt loam, 0 to 1 percent slopes


muname:
Alamogordo-Aztec complex, 1 to 3 percent slopes


muname:
Alamogordo-Gypsum land complex, 0 to 5 percent slopes


muname:
Alamogordo-Gypsum land-Aztec complex, 15 to 50 percent slopes


muname:
Alamogordo-McCullough sandy loams, hummocky, 0 to 3 percent slopes


muname:
Alamogordo variant very fine sandy loam, 0 to 1 percent slopes


muname:
Armesa very fine sandy loam, 0 to 5 percent slopes


muname:
Aztec gravelly fine sandy loam, 3 to 12 percent slopes


muname:
Aztec-Alamogordo complex, hummocky, 1 to 3 percent slopes


muname:
Aztec-Rock outcrop-Lozier complex, 20 to 65 percent slopes


muname:
Borrego cobbly loam, 15 to 40 percent slopes


muname:
Crowflats silt loam, 0 to 2 percent slopes


muname:
Deama gravelly loam, 0 to 5 percent slopes


muname:
Deama gravelly loam, 5 to 30 percent slopes


muname:
Deama-Rock outcrop complex, 20 to 50 percent slopes


muname:
Deama-Rock outcrop complex, 50 to 150 percent slopes


muname:
Deama-Rock outcrop-Holloman variant complex, 15 to 65 percent slopes


muname:
Dona Ana-Berino association, gently sloping


muname:
Dye-Encierro complex, 5 to 30 percent slopes


muname:
Ector-Rock outcrop complex, 20 to 50 percent slopes


muname:
Espy-Shanta variant association, gently sloping


muname:
Gypsum land-Holloman complex, 0 to 5 percent slopes


muname:
Holloman very fine sandy loam, 0 to 1 percent slopes


muname:
Holloman-Gypsum land complex, 0 to 1 percent slopes


muname:
Holloman-Gypsum land-Yesum complex, 0 to 5 percent slopes


muname:
Largo very fine sandy loam, thick surface, 0 to 1 percent slopes


muname:
Largo silt loam, 1 to 3 percent slopes, eroded


muname:
Largo silt loam, frequent overflow, 0 to 1 percent slopes


muname:
Largo-Ogral complex, 1 to 3 percent slopes


muname:
Largo-Ogral complex, 0 to 5 percent slopes


muname:
Lozier-Rock outcrop complex, 0 to 5 percent slopes


muname:
Lozier-Rock outcrop complex, 5 to 20 percent slopes


muname:
McCullough sandy loam, 1 to 3 percent slopes


muname:
McCullough variant very fine sandy loam, 0 to 1 percent slopes


muname:
Mead silty clay loam, 0 to 1 percent slopes


muname:
Nickel-Aztec gravelly sandy loams, 2 to 8 percent slopes


muname:
Pena-Aztec variant association, strongly sloping


muname:
Pena variant-Rock outcrop association, steep


muname:
Philder very fine sandy loam, 0 to 9 percent slopes


muname:
Pintura-Dona Ana complex, 0 to 5 percent slopes


muname:
Pintura-Tome-Dona Ana complex, 0 to 5 percent slopes


muname:
Prelo fine sandy loam, 0 to 1 percent slopes


muname:
Prelo sandy loam, hummocky, 0 to 1 percent slopes


muname:
Prelo silt loam, 1 to 3 percent slopes, eroded


muname:
Prelo silt loam, hummocky, 0 to 1 percent slopes


muname:
Prelo silt loam, frequent overflow, 0 to 1 percent slopes


muname:
Prelo-Prelo variant complex, 0 to 3 percent slopes


muname:
Reeves very fine sandy loam, 0 to 1 percent slopes


muname:
Reeves very fine sandy loam, 0 to 2 percent slopes, eroded


muname:
Reeves very fine sandy loam, frequent overflow, 0 to 1 percent slopes


muname:
Reeves variant-Shanta association, gently sloping


muname:
Rock outcrop-Deama complex, 40 to 150 percent slopes


muname:
Rock outcrop-Lozier complex, 20 to 65 percent slopes


muname:
Rock outcrop-Tortugas-Ustifluvents complex, 0 to 80 percent slopes


muname:
Tencee very gravelly silt loam, 0 to 10 percent slopes


muname:
Tome very fine sandy loam, 0 to 1 percent slopes


muname:
Tome very fine sandy loam, 1 to 3 percent slopes, eroded


muname:
Tome silt loam, frequent overflow, 1 to 3 percent slopes


muname:
Tome-Emot complex, 0 to 3 percent slopes


muname:
Tortugas cobbly loam, 5 to 30 percent slopes


muname:
Ustic Torriorthents, frequent overflow, 0 to 1 percent slopes


muname:
Apache cobbly clay loam, 1 to 3 percent slopes


muname:
Kim fine sandy loam, 3 to 5 percent slopes


muname:
Dalhart fine sandy loam, 0 to 3 percent slopes, eroded


muname:
Dalhart loamy fine sand, 0 to 3 percent slopes


muname:
Dalhart loamy fine sand, 0 to 3 percent slopes, eroded


muname:
Corlena loamy fine sand, 0 to 1 percent slopes, occasionally flooded


muname:
Conlen fine sandy loam, 3 to 5 percent slopes


muname:
Conlen-Dalhart complex, 1 to 3 percent slopes


muname:
Conlen-Plack complex, 3 to 12 percent slopes


muname:
Otero loamy fine sand, 1 to 5 percent slopes


muname:
Plack-Kerrick complex, 1 to 3 percent slopes


muname:
Rickmore fine sandy loam, 0 to 1 percent slopes


muname:
Travessilla-Rock outcrop complex, 10 to 50 percent slopes


muname:
Manzano clay loam, 0 to 1 percent slopes, occasionally flooded


muname:
Dalupe fine sandy loam, 0 to 1 percent slopes, occasionally flooded


muname:
Travessilla stony loam, 3 to 12 percent slopes


muname:
Glenrio clay loam, 1 to 5 percent slopes


muname:
Vona-Valent complex, 3 to 5 percent slopes


muname:
Paymaster fine sandy loam, 0 to 1 percent slopes, rarely flooded


muname:
Perico-Ulysses complex, 0 to 1 percent slopes


muname:
Perico-Ulysses complex, 1 to 3 percent slopes


muname:
Perico-Ulysses complex, 3 to 5 percent slopes


muname:
Happyditch loamy fine sand, 0 to 1 percent slopes, occasionally flooded


muname:
Conlen clay loam, 3 to 8 percent slopes, severely eroded


muname:
Otero fine sandy loam, 3 to 8 percent slopes


muname:
Otero-Vona complex, 3 to 12 percent slopes


muname:
Plack-Rock outcrop complex, 5 to 20 percent slopes


muname:
Lesho silty clay loam, 0 to 1 percent slopes, occasionally flooded


muname:
Valent fine sand, 12 to 30 percent slopes


muname:
Ulysses clay loam, 0 to 1 percent slopes


muname:
Ulysses clay loam, 1 to 3 percent slopes


muname:
Quinlan-Rock outcrop complex, 5 to 30 percent slopes


muname:
Vona loamy fine sand, 0 to 3 percent slopes


muname:
Vona loamy fine sand, 3 to 8 percent slopes


muname:
Vona, otero, and plack soils, 3 to 20 percent slopes


# SYSTEM - Geomorphic Feature

geomfdesc:
A unit of folded strata that is convex upward and whose core contains the stratigraphically oldest rocks, and occurs at the earth's surface.  In a single anticline, beds forming the opposing limbs of the fold dip away from its axial plane.  Compare - monocline, syncline, fold.  SW & HP


geomfdesc:
(not preferred - see pyroclastic flow, pyroclastic surge)  A highly heated mixture of volcanic gases and ash, traveling down the flank of a volcano or along the surface of the ground; produced by the explosive disintegration of viscous lava in a volcanic crater, or by the explosive emission of gas-charged ash from a fissure or group of fissures.  The solid materials contained in a typical ash flow are generally unsorted and ordinarily include volcanic dust, pumice, scoria, and blocks in addition to ash.  (Also called a pyroclastic flow.)  Compare - nue ardente, lahar, pyroclastic.  GG


geomfdesc:
A coral reef appearing in plan view as roughly circular, and surmounted by a chain of closely spaced, low coral islets that encircle or nearly encircle a shallow lagoon in which there is no land or islands of non-coral origin; the reef is surrounded by open sea.  GG


geomfdesc:
The central, channel-like corridor, scar, or depression along which an avalanche has moved.  An eroded surface marked by pits, scratches, and grooves.  GG


geomfdesc:
The upper or inner, usually dry, zone of the shore or beach, lying between the high-water line of mean spring tides and the upper limit of shore-zone processes; it is acted upon by waves or covered by water only during exceptionally severe storms or unusually high tides.  It is essentially horizontal or slopes gently landward, and is divided from the foreshore by the crest of the most seaward berm.  Compare - washover fan.  GG


geomfdesc:
(colloquial: southwestern U.S.A.) A broad, gently inclined alluvial piedmont slope extending from the base of a mountain range out into a basin, and formed by the lateral coalescence of a series of alluvial fans.  Typically it has a broadly undulating transverse profile, parallel to the mountain front, resulting from the convexities of component fans.  The term is generally restricted to constructional slopes of intermontane basins.  Synonym - coalescent fan piedmont.  Compare - colluvial apron.  HP & SW


geomfdesc:
(colloquial: western U.S.A.) A rounded, dome-shaped hill, formed either by erosion or uplift.  GG


geomfdesc:
A long, narrow, sandy island, representing a broadened barrier beach that is above high tide and parallel to the shore, and that commonly has dunes, vegetated zones, and swampy terrains extending lagoonward from the beach.  Also a long series of barrier beaches.  Compare - barrier beach. GG


geomfdesc:
A thin accumulation of stone blocks, typically angular, with only coarse fragments in the upper part, over solid or weathered bedrock, colluvium, or alluvium, without a cliff or ledge above as an apparent source.  Block fields occur on high mountain slopes above tree-line, or in polar or paleo-periglacial regions; they are most extensive along slopes parallel to the contour; and they generally occur on slopes of less than 5%.  Synonym - felsenmeer.  Compare - block stream, talus, scree.  GG


geomfdesc:
An accumulation of boulders or angular blocks, with no fine sizes in the upper part, overlying solid or weathered bedrock, colluvium, or alluvium, and lying below a cliff or ledge from which coarse fragments originate.  Block streams usually occur at the heads of ravines as narrow bodies that are more extensive downslope than along the slope.  They may exist on any slope angle, but ordinarily not steeper than 90 percent slope (approx. 40 degrees).  Compare - block field.  GG


geomfdesc:
A saucer-, cup-, or trough-shaped hollow or depression formed by wind erosion, on a pre-existing dune or other sand deposit, especially in an area of shifting sand, loose soil, or where protective vegetation is disturbed or destroyed; the adjoining accumulation of sand derived from the depression, where recognizable, is commonly included.  Commonly small, but some blowouts may be many kilometers in diameter.  Compare - deflation basin.  GG


geomfdesc:
A channel or stream with multiple channels that interweave as a result of repeated bifurcation and convergence of flow around inter-channel bars, resembling (in plan view) the strands of a complex braid.  Braiding is generally confined to broad, shallow streams of low sinuosity, high bedload, non-cohesive bank material, and a steep gradient.  At a given bank-full discharge, braided streams have steeper slopes and shallower, broader, and less stable channel cross sections than meandering streams.  Compare - meandering channel, flood-plain landforms.  HP


geomfdesc:
A large, more or less circular depression, formed by explosion and/or collapse, which surrounds a volcanic vent or vents, and whose diameter is many times greater than that of the included vent, or vents.  Compare - crater.  GG


geomfdesc:
A long, deep, narrow, very steep-sided valley cut primarily in bedrock with high and precipitous walls in an area of high local relief (e.g., mountain or high plateau terrain), often with a perennial stream at the bottom; similar to but larger than a gorge.  Compare - gorge, box canyon, slot canyon.  SW, HP & GG


geomfdesc:
(a) [stream] The hollow bed where a natural body of surface water flows or may flow.  The deepest or central part of the bed of a stream, containing the main current and occupied more or less continuously by water.  (b) (colloquial: western U.S.A.) The bed of a single or braided watercourse that commonly is barren of vegetation and is formed of modern alluvium.  Channels may be enclosed by banks or splayed across and slightly mounded above a fan surface and include bars and mounds of cobbles and stones.  (c) [microfeature] Small, trough-like, arcuate or sinuous channels separated by small bars or ridges, caused by fluvial processes and common to floodplains and young alluvial terraces; a constituent part of bar & channel topography. GG, FFP, & SW


geomfdesc:
A long, narrow, vegetated marine beach ridge or sandy hummock, 1 to 6 m high, forming roughly parallel to a prograding shoreline, seaward of marsh and mud-flat deposits, enclosed on the seaward side by fine-grained sediments, and resting on foreshore or mud-flat deposits.  It is well drained, often supporting trees on higher areas.  Widths range from 45 - 450 m and lengths may exceed several tens of kilometers.  GG


geomfdesc:
A mud-rich strand plain, occupied by cheniers and intervening mud-flats with marsh and swamp vegetation.  Compare - chenier, strand plain.  GG


geomfdesc:
Any high, very steep to perpendicular or overhanging face of rock or earth; a precipice.  Compare - bluff. GG


geomfdesc:
A low, generally broad plain that has as its margin an oceanic shore and its strata horizontal or gently sloping toward the water, and generally represents a strip of recently prograded or emerged sea floor; e.g. the coastal plain of the southeastern U.S. which extends for 3000 km from New Jersey to Texas.  GG


geomfdesc:
A lakebed formed in a lake on glacial ice and subsequently "let down" or collapsed by the melting of underlying ice, resulting in contortion or folding or the lacustrine sediment and sedimentary structures.  These modified or distorted lacustrine sediments cap present-day topographic highs and generally lie at elevations higher than the surrounding disintegration moraine.  Compare - collapsed lake plain, collapsed ice-walled lakebed.  SW & CF


geomfdesc:
A lakebed that formed in a lake bounded by stagnant ice, but floored by solid ground, usually till.  Collapse features are limited to the lakebed margins.  Presently, these materials and sedimentary structures generally occur as roughly circular-shaped hills of till capped by lacustrine sediments, generally at elevations higher than surrounding disintegration moraine.  Compare - collapsed ice-floored lakebed, collapsed lake plain.  SW & CF


geomfdesc:
A lake plain formed on, and bounded by, glacial ice and subsequently "let down" or collapsed by the melting of underlying ice resulting in contortion or folding of the sediments and sedimentary structures.  Lacustrine sediments cap present topography.    Compare - lake plain.  SW & CF


geomfdesc:
An outwash plain which forms on glacial ice (inside the glacial margin), and is subsequently let down or collapsed when the underlying ice melts, resulting in contortion or folding of the sediments and sedimentary structures to the extent that little of the original plain or it's gradient remain.  Outwash sediments commonly cap present-day  topography.  Compare - collapsed lake plain, pitted outwash plain.  SW &  CF


geomfdesc:
The new and relatively short channel formed when a stream cuts through a narrow strip of land and thereby shortens the length of its channel.  GG


geomfdesc:
The process, associated sediments (debris flow deposit) or resultant landform characterized by a very rapid type of flow dominated by a sudden, downslope movement of a mass of rock, soil, and mud (more than 50% of the particles are >2 mm), and whether saturated or comparatively dry, behaves much as a viscous fluid.  Compare - lahar, mudflow, landslide.  SW


geomfdesc:
A topographic basin excavated and maintained by wind erosion which removes unconsolidated material and commonly leaves a rim of resistant material surrounding the depression.  Unlike a blowout, a deflation basin does not include adjacent deposits derived from the basin.  Compare - blowout.  GG


geomfdesc:
The level or nearly level surface composing the land-ward part of a large delta; strictly, a flood plain characterized by repeated channel bifurcation and divergence, multiple distributary channels, and interdistributary flood basins.  GG


geomfdesc:
A dome or anticlinal fold in which the overlying rocks or sediments have been ruptured by the squeezing-out of plastic core material.  Diapirs in sedimentary strata usually contain cores of salt or shale; igneous intrusions may also show diapiric structure.  GG


geomfdesc:
A tabular igneous intrusion that cuts across the bedding or foliation of the country rock.  Compare - sill.  GG


geomfdesc:
A slope of the land surface, roughly determined by and approximately conforming with the dip of underlying bedded rocks; (i.e. the long, gently inclined surface of a cuesta).  Compare - scarp slope.  HP


geomfdesc:
A drift topography characterized by chaotic mounds and pits, generally randomly oriented, developed in supraglacial drift by collapse and flow as the underlying stagnant ice melted.  Slopes may be steep and unstable and there will be used and unused stream courses and lake depressions interspersed with the morainic ridges.  Characteristically, there are numerous abrupt, lateral and vertical changes between unconsolidated materials of differing lithology.  SJ & SW


geomfdesc:
(a) The line of separation;  (b) The summit area, or narrow tract of higher ground that constitutes the watershed boundary between two adjacent drainage basins; it divides the surface waters that flow naturally in one direction from those that flow in the opposite direction.  Compare - interfluve  GG


geomfdesc:
(a) A general term for a course or channel along which water moves in draining an area.  GG;   (b) [soil survey] a term restricted to relatively small, roughly linear or arcuate depressions that move concentrated water at some time, and either lack a defined channel (e.g. head slope, swale) or have a small, defined channel (e.g. low order streams).  SW


geomfdesc:
The process, associated sediments (earthflow deposit) or resultant landform characterized by slow to rapid types of flow dominated by downslope movement of a mass of rock, soil, and mud (more than 50% of the particles are < 2 mm), and whether saturated or comparatively dry, behaves much as a viscous fluid.  Compare - debris flow (coarse, less fluid), mudflow (more fluid), landslide.  SW


geomfdesc:
A topographic feature that remains or is left standing above the general land surface after erosion has reduced the surrounding area; e.g., a monadnock, a butte, or a stack.  GG


geomfdesc:
(a) A category of mass movement processes, associated sediments (fall deposit), or resultant landforms (e.g., rockfall, debris fall, soil fall) characterized by very rapid movement of a mass of rock or earth that travels mostly through the air by free fall, leaping, bounding, or rolling, with little or no interaction between one moving unit and another.  Compare - topple, slide, lateral spread, flow, complex landslide, landslide.  SW & DV;   (b) The mass of material moved by a fall.  GG


geomfdesc:
(a) A gently sloping, fan-shaped mass of detritus forming a section of a low-angle cone commonly at a place where there is a notable decrease in gradient; specifically an alluvial fan (not preferred - use alluvial fan). Compare - alluvial fan, alluvial cone.  (b) A fan-shaped mass of congealed lava that formed on a steep slope by the continually changing direction of flow.  GG


geomfdesc:
A linear depression formed by a drainageway that is incised considerably below the surface of an alluvial fan.  GG


geomfdesc:
The most extensive landform on piedmont slopes, formed by (a) the lateral, downslope, coalescence of mountain-front alluvial fans into one generally smooth slope with or without the transverse undulations of the semi-conical alluvial fans, and (b) accretions of fan aprons.  FFP


geomfdesc:
A general term for landforms that are the remaining parts of older fan-landforms, such as alluvial fans, fan aprons, inset fans, and fan skirts, that either have been dissected (erosional fan-remnants) or partially buried (nonburied fan-remnants).  An erosional fan remnant must have a relatively flat summit that is a relict fan-surface.  A nonburied fan-remnant is a relict surface in its entirety.  Compare - eroded fan remnant, ballena.  FFP.


geomfdesc:
The zone of smooth, laterally-coalescing, small alluvial fans that issue from gullies cut into the fan piedmont of a basin or that are coalescing extensions of the inset fans of the fan piedmont, and that merge with the basin floor at their toeslopes.  These are generally younger fans which onlap older fan surfaces.  FFP


geomfdesc:
(a) A steep slope or cliff formed by differential erosion along a fault line, as by the more rapid erosion of soft rock on the side of a fault as compared to that of more resistant rock on the other side; e.g. the east face of the Sierra Nevada in California.  (b)  (not recommended) A fault scarp that has been modified by erosion.  This usage is not recommended because the scarp is usually not located on the fault line.  GG


geomfdesc:
[geomorphology] - (a) (adjective)  Said of an area characterized by a continuous surface or stretch of land that is smooth, even, or horizontal, or nearly so, and that lacks any significant curvature, slope, elevations, or depressions.  (b) (noun)  An informal, generic term for a level or nearly level surface or small area of land marked by little or no local relief.  Compare - mud flat.  (c) (not recommended) A nearly level region that visibly displays less relief than its surroundings.  GG.

[lake] (not recommended)  (a) The low-lying, exposed, flat land of a lake delta or of a lake bottom. Compare - lake plain.  (b) The flat bottom of a desiccated lake in the arid parts of western USA.  Compare - playa, pluvial lake.


geomfdesc:
A fan-shaped deposit or other outspread deposit formed where an overloaded stream breaks through a levee (natural or artificial) and deposits its material (often coarse-grained) on the flood plain.  Compare - crevasse.  GG


geomfdesc:
An essentially flat, terrace-like alluvial surface within a valley that is frequently covered by flood water from the present stream (e.g., below the 100 year flood level); any approximately horizontal surface still actively modified by fluvial scour and/or deposition (i.e., cut and fill and/or scour and fill processes).  May occur individually or as a series of steps.  Compare - stream terrace.  SW & RR


geomfdesc:
A lineation or streamlined groove and ridge parallel to the direction of ice movement, formed in newly deposited till or older drift.  They range in height from a few centimeters to 25 m, and in length from a few meters to 20 km.  GG


geomfdesc:
A long, narrow depression or troughlike hollow between the edge of a retreating glacier and the wall of its valley, or between the front of a moraine and its outwash plain.  GG


geomfdesc:
The part of a hillside or mountainside consisting of an outcrop of bare rock (scarp or cliff) that sheds colluvium to slopes below and commonly stands more steeply than the angle of repose of the colluvial slope (e.g. talus slope) immediately below. SW &  GG


geomfdesc:
A sharp break or opening in a mountain ridge, or a short pass through a mountain range; e.g., a wind gap.  GG


geomfdesc:
A ripple that is more than 30 m in length; e.g., the jokulhlaup derived giant ripples in Camas Prairie, MT.; it usually exhibits superimposed megaripples.  Compare - ripple mark.  GG


geomfdesc:
A channel formed by an ice-marginal, englacial, or subglacial stream during glaciation.  GG


geomfdesc:
An area formerly occupied by a glacial lake.  GG


geomfdesc:
An elongated trough or basin bounded on both sides by high-angle, normal faults that dip towards the interior of the trough.  It is a structural form that may or may not be geomorphically expressed as a rift valley.  Compare - horst.  GG


geomfdesc:
(colloquial:  western U.S.A.; not preferred - refer to ravine)  A small stream channel, narrow and steep-sided in cross section, and larger than a gully, cut in unconsolidated materials.  General synonym - ravine.  Compare - arroyo, draw, gully, wash. HP


geomfdesc:
(colloquial: U.S. Virgin Islands, Caribbean Basin)  A gully, ravine, small valley, or narrow passage on land. GG


geomfdesc:
A steep slope at the head of a valley; e.g. the rock cliff at the back of a cirque.  Compare - cirque headwall. GG


geomfdesc:
A bog, often on the uplands, whose surface is covered by sphagnum mosses which, because of their high degree of water retention, make the bog more dependent upon precipitation than on the water table.  The bog often occurs as a raised peat bog or blanket bog.  Compare - lowmoor bog, raised bog.  GG


geomfdesc:
A semi-conical type of alluvial fan with very steep slopes; it is higher, narrower, and steeper (e.g., > 40% slopes) than a fan, and composed of coarser, and thicker layers of material deposited by a combination of alluvial episodes and to a much lesser degree, landslides (e.g., debris flow).  Compare - alluvial fan, talus cone.  SW


geomfdesc:
A low, outspread mass of loose materials and/or rock material, commonly with gentle slopes, shaped like an open fan or a segment of a cone, deposited by a stream (best expressed in semiarid regions) at the place where it issues from a narrow mountain or upland valley; or where a tributary stream is near or at its junction with the main stream.  It is steepest near its apex which points upstream and slopes gently and convexly outward (downstream) with a gradual decrease in gradient.  GG


geomfdesc:
(a) (colloquial: western U.S.A.)  A nearly level, graded, alluvial surface in bolsons and semi-bolsons which commonly does not manifest traceable channels, terraces or floodplain levels.  Compare - flood-plain step, terrace, valley flat.  FFP, GG, & SW.  (b) (not preferred) A general term for a small flood plain bordering a river, on which alluvium is deposited during floods.  GG


geomfdesc:
A narrow, jagged mountain crest, often above the snowline, sculptured by alpine glaciers and formed by backward erosion of adjoining cirque walls.  HP


geomfdesc:
(not recommended as a landform term - use avalanche chute).  The path formed by an avalanche.  It may take the form of an open path in a forest, with bent and broken trees, or an eroded surface marked by pits, scratches, and grooves.  Compare - avalanche chute  GG


geomfdesc:
The channel of a flat-floored, ephemeral stream, commonly with very steep to vertical banks cut in unconsolidated material, sometimes called a wash.  It is usually dry but can be transformed into a temporary watercourse or short-lived torrent after heavy rain within the watershed.  Where arroyos intersect zones of ground-water discharge, they are more properly classed as intermittent stream channels.  HP


geomfdesc:
(refer to berm.)  A low, impermanent, nearly horizontal or landward-sloping shelf, ledge, or narrow terrace on the backshore of a beach, formed of material thrown up and deposited by storm waves; it is generally bounded on one side or the other by a beach ridge or beach scarp.  Some beaches have no berms, others have one or several.  GG


geomfdesc:
A narrow, elongate, coarse-textured ridge rising slightly above high-tide level and generally parallel with the shore, but separated from it by a lagoon or marsh; it is rarely more than several kilometers long.  Compare - barrier island.   Synonym, offshore barrier, offshore beach, bar beach.  Compare - bar [coast], barrier island.  GG and FFP


geomfdesc:
A general term for the nearly level, lower-most part of intermontane basins (i.e. bolsons, semi-bolsons).  The floor includes all of the alluvial, eolian, and erosional landforms below the piedmont slope.  Compare - basin, piedmont slope.  FFP


geomfdesc:
(colloquial:  western U.S.A.)  A relatively flat, erosional remnant of any former landform of a basin floor that has been dissected following the incision of an axial stream.  FFP


geomfdesc:
a) A gently sloping zone, typically with a concave profile, of unconsolidated material extending landward from the low-water line to the place where there is a definite change in material or physiographic form (such as a cliff) or to the line of permanent vegetation (usually the effective limit of the highest storm waves); a shore of a body of water, formed and washed by waves or tides, usually covered by sand or gravel; (b) the relatively thick and temporary accumulation of loose water-borne material (usually well-sorted sand and pebbles) accompanied by mud, cobbles, boulders, and smoothed rock and shell fragments, that is in active transit along, or deposited on, the shore zone between the limits of low water and high water.  GG


geomfdesc:
A relatively flat area, often occupied by pools of water, separating the exposed or seaward edge of a barrier beach or barrier island from the lagoon behind it.  GG


geomfdesc:
A low, essentially continuous mound of beach or beach-and-dune material heaped up by the action of waves and currents on the backshore of a beach, beyond the present limit of storm waves or the reach of ordinary tides, and occurring singly or as one of a series of approximately parallel deposits.  The ridges are roughly parallel to the shoreline and represent successive positions of an advancing shoreline.  GG


geomfdesc:
A platform-like, nearly level to gently inclined erosional surface developed on resistant strata in areas where valleys are cut in alternating strong and weak layers with an essentially horizontal attitude.  Structural benches are bedrock controlled, and in contrast to stream terraces, have no geomorphic implication of former, partial erosion cycles and base-level controls, nor do they represent a stage of flood-plain development following an episode of valley trenching.  Compare - ledge; see scarp.  HP


geomfdesc:
An abrupt change or inflection in a slope or profile.  Compare - knickpoint, shoulder, escarpment.  (geomorphology)  A marked variation of topography, or a tract of land distinct from adjacent land, or an irregular or rough piece of ground.  Compare - breaks.  GG


geomfdesc:
(colloquial: western U.S.A.)  A fan remnant having a distinctively-rounded surface of fan alluvium.  The ballena's broadly-rounded shoulders meet from either side to form a narrow summit and merge smoothly with concave sideslopes and then concave, short pediments which form smoothly-rounded drainageways between adjacent ballenas.  A partial ballena is a fan remnant large enough to retain some relict fan surface on a remnant summit.  Compare - fan remnant.  SW & FFP.


geomfdesc:
[beach] A low, impermanent, nearly horizontal or landward-sloping shelf, ledge, or narrow terrace on the backshore of a beach, formed of material thrown up and deposited by storm waves; it is generally bounded on one side or the other by a beach ridge or beach scarp.  Some beaches have no berms, others have one or several.  GG


geomfdesc:
(a) A high bank or bold headland, with a broad, precipitous, sometimes rounded cliff face overlooking a plain or body of water, especially on the outside of a stream meander; ex. a river bluff.  (b) (not preferred) use cliff.  Any cliff with a steep, broad face.  GG


geomfdesc:
Waterlogged, spongy ground, consisting primarily of mosses, containing acidic, decaying vegetation such as sphagnum, sedges, and heaths, that may develop into peat.  Compare - fen, marsh, swamp.  GG


geomfdesc:
A continuous and level or undulating area formed by closely spaced successive embankments of wave-deposited beach material added more or less uniformly to a prograding shoreline, such as to a growing compound spit or to a cuspate foreland.  Compare - wave-built terrace, cheneir plain.  GG


geomfdesc:
A crescent-shaped dune with tips extending leeward (downwind), making this side concave and the windward (upwind) side convex.  Barchan dunes tend to be arranged in chains extending in the dominant wind direction.  Compare - parabolic dune.  HP


geomfdesc:
A general term for a ridge-like accumulation of sand, gravel, or other alluvial material formed in the channel, along the banks, or at the mouth of a stream where a decrease in velocity induces deposition; e.g. a channel bar or a meander bar.  [coast] - A generic term for any of various elongate offshore ridges, banks, or mounds of sand, gravel, or other unconsolidated material submerged at least at high tide, and built up by the action of waves or currents, especially at the mouth of a river or estuary, or at a slight distance offshore from the beach.  Compare - longshore bar.  GG & GSST


geomfdesc:
A flood-plain landform.  Extensive, marshy, or swampy, depressed areas of flood plains between natural levees and valley sides or terraces.  Compare - valley flat.  HP


geomfdesc:
(a) A landform that consists of a wave-cut scarp and wave-built terrace of well-sorted sand and gravel of marine and lacustrine origin. (b) (colloquial: western U.S.A.) relict shorelines from pluvial lakes, generally restricted to valley sides.  Compare - strandline, shoreline.  FFP


geomfdesc:
An isolated, generally flat-topped hill or mountain with relatively steep slopes and talus or precipitous cliffs and characterized by summit width that is less than the height of bounding escarpments, commonly topped by a caprock of resistant material and representing an erosion remnant carved from flat-lying rocks.  Compare - mesa, plateau, cuesta.  HP & GG


geomfdesc:
Any of various shallow, often oval or elliptical, generally marshy, closed depressions in the Atlantic coastal plain (from southern New Jersey to northeastern Florida, especially developed in the Carolinas) which share an approximately parallel orientation of their long axes.  They range from about 100 meters to many kilometers in length, are rich in humus, and under native conditions contain trees and shrubs different from those of the surrounding areas.  Also called Grady ponds (colloquial: Georgia and Alabama) and Delmarva Bays (colloquial: Maryland).    Compare - pocosin.  GG


geomfdesc:
(colloquial: northwest USA, and ND) A dry or intermittent stream valley or wash, especially a long, steep-walled gorge representing a Pleistocene overflow channel that carried meltwater from an ice sheet, e.g. the Grand Coulee in Washington State.  HP


geomfdesc:
A short, straight ridge of stratified sand and gravel believed to have been deposited in a crevasse of a wasting glacier and left standing after the ice melted; a variety of kame.  May also occur as long, sinuous ridges and linear complexes of till or drift.  GG


geomfdesc:
A conical hill formed by the accumulation of cinders and other pyroclastics, normally basaltic or andisitic composition.  Slopes generally exceed 20 percent.  GG


geomfdesc:
A high, narrow, sharp-edged pass or saddle through a divide or between two adjacent peaks in a mountain range; especially a deep pass formed by the headward erosion and intersection of two cirques.  Compare - gap, pass, saddle.  GG


geomfdesc:
(not recommended: obsolete) use shrub-coppice dune.


geomfdesc:
a) A walled and rounded or cirque-like opening at the head of a small steep valley.  b) (colloquial - southern Appalachians, USA) A smooth-floored, somewhat oval-shaped "valley" sheltered by hills or mountains; e.g., Cades Cove in eastern Tennessee.  GG


geomfdesc:
A steep-walled, half bowl-like recess or hollow, crescent-shaped or semicircular in plan, commonly situated at the head of a  glaciated mountain valley or high on the side of a mountain, and produced by the erosive activity of a mountain glacier.  It often contains a small round lake (tarn).  Compare - cirque floor, cirque platform, cirque wall.  SW & GG.


geomfdesc:
A basin-like, rimmed structure, usually at the summit of a volcanic cone.  It may be formed by collapse, by an explosive eruption or by the gradual accumulation of pyroclastic material into a surrounding rim.  Compare - caldera.   GG


geomfdesc:
An asymmetric, homoclinal ridge capped by resistant rock layers of slight to moderate dip (commonly less than 15 percent); produced by differential erosion of interbedded resistant and weak rocks.  A cuesta has a long, gentle slope on one side (dip slope), that roughly parallels the inclined beds, and on the other side has a relatively short and steep or cliff-like slope (scarp) that cuts through the tilted rocks.    Compare - hogback, mesa, dipslope, scarp slope, cuesta valley.  SW & HP


geomfdesc:
A body of alluvium, nearly flat and fan-shaped, deposited at or near the mouth of a river or stream where it enters a body of relatively quiet water, usually a sea or lake.  HP


geomfdesc:
A smoothly rounded landform of rock mass such as a rock-capped mountain summit, that roughly resembles the dome of a building.  (e.g. the rounded granite peaks of Yosemite, CA).  GG


geomfdesc:
Any relatively sunken part of the Earth's surface; especially a low-lying area surrounded by higher ground.  A closed depression has no natural outlet for surface drainage (e.g. a sinkhole).  An open depression has a natural outlet for surface drainage.  Compare - closed depression, open depression.   GG


geomfdesc:
A low, smooth, elongated oval hill, mound, or ridge of compact till that has a core of bedrock or drift.  It usually has a blunt nose facing the direction from which the ice approached and a gentler slope tapering in the other direction.  The longest axis is parallel to the general direction of glacier flow.  Drumlins are products of streamline (laminar) flow of glaciers, which molded the subglacial floor through a combination of erosion and deposition.  Compare - drumlinoid ridge.  SW,  HP, & GG


geomfdesc:
A low mound, ridge, bank or hill of loose, windblown, subaerially deposited, granular material (generally sand), either bare and capable of movement from place to place, or covered and stabilized with vegetation,  but always retaining its characteristic shape.  (See barchan dune, parabolic dune, parna dune, shrub-coppice dune, seif dune, transverse dune).  SW & GG


geomfdesc:
A small, natural watercourse cut in unconsolidated materials, generally more open with a broader floor and more gently sloping sides than an arroyo, ravine or gulch, and whose present stream channel may appear inadequate to have cut the drainageway that it occupies.  SW


geomfdesc:
A long, narrow, sinuous and steep-sided ridge composed of irregularly stratified sand and gravel  deposited as the bed of  a  stream flowing in an ice tunnel within or below the ice (subglacial) or between ice walls on top of the ice of a wasting glacier, and  left behind as high ground when the ice melted.  Eskers range in length from less than a kilometer to more than 160 kilometers, and in height from 3 to 30 meters.   Compare - glaciofluvial deposits, kame, crevasse filling, outwash.  SW


geomfdesc:
A ridge-like accumulation that is being or was produced at the outer margin of an actively flowing glacier at any given time; a moraine that has been deposited at the outer or lower end of a valley glacier.  Compare - terminal moraine, recessional moraine, ground moraine.  GG


geomfdesc:
A relatively continuous and steep slope or cliff produced by erosion or faulting and that topographically interrupts or breaks the general continuity of more gently sloping land surfaces .  The term is most commonly applied to cliffs produced by differential erosion.  Synonym: "scarp." SW & HP


geomfdesc:
A sheet-like mantle of relatively young alluvium and soils covering part of an older fan piedmont (and occasionally alluvial fan) surface, commonly thicker and further down slope (e.g., mid-fan or mid-fan piedmont) than a fan collar.  It somewhere buries an older soil that can be traced to the edge of the fan apron where the older soil emerges as the land surface, or relict soil.  No buried soils should occur within a fan-apron mantle itself.  Compare - fan collar.  FFP


geomfdesc:
A coastal dune or dune ridge oriented parallel to the shoreline, occurring at the landward margin of the beach, along the shoreward face of a beach ridge, or at the landward limit of the highest tide, and more or less stabilized by vegetation.  GG


geomfdesc:
A long, narrow, winding, U-shaped and steep-walled, generally deep inlet or arm of the sea between high rocky cliffs of slopes along a mountainous coast.  Typically it has a shallow sill or threshold of solid rock or earth material submerged near its mouth and becomes deeper far inland.  A fjord usually represents the seaward end of a deep, glacially excavated valley that is partially submerged by drowning after melting of the ice.  GG


geomfdesc:
Waterlogged, spongy ground containing alkaline decaying vegetation, characterized by reeds, that develops into peat.  It sometimes occurs in sinkholes of karst regions.  Compare - bog, marsh, swamp.  GG


geomfdesc:
The nearly level plain that borders a stream and is subject to inundation under flood-stage conditions unless protected artificially.  It is usually a constructional landform built of sediment deposited during overflow and lateral migration of the streams.  HP


geomfdesc:
The inverted V-shaped end of a ridge that has been truncated or steeply beveled by steam erosion (e.g. meander scar or bluff), glacial truncation, or fault scarp displacement.   Compare - spur.  HP


geomfdesc:
A landform consisting of very low gradient, broad, barren, axial-stream channel segments in an intermontane basin.  It floods broadly and shallowly and is veneered with barren fine-textured sediment that crusts.  Commonly, a flood-plain playa is segmented by transverse, narrow bands of vegetation, and it may alternate with ordinary narrow or braided channel segments.  FFP


geomfdesc:
(a) Commonly an extensive, low relief area of till, having an uneven or undulating surface, and commonly bounded on the distal end by a recessional or end moraine; (b) A layer of poorly sorted rock and mineral debris (till) dragged along, in, on, or beneath a glacier and deposited by processes including basal lodgement and release from downwasting stagnant ice by ablation.  Compare - end moraine, recessional ,moraine, terminal moraine.  SW


geomfdesc:
(a) A narrow, deep valley with nearly vertical, rocky walls, smaller than a canyon, and more steep-sided than a ravine; especially a restricted, steep-walled part of a canyon.  (b) A narrow defile or passage between hills or mountains.  GG


geomfdesc:
A small channel with steep sides caused by erosion and cut in unconsolidated materials by concentrated but intermittent flow of water usually during and immediately following heavy rains or after ice / snow melt.  A gully generally is an obstacle to wheeled vehicles and too deep (e.g., >  0.5 m) to be obliterated by ordinary tillage; (a rill is of lesser depth and can be smoothed over by ordinary tillage).  Compare - rill, ravine, arroyo, swale, draw.  HP & GSST


geomfdesc:
(a) An irregularity of land, especially of considerable height with a steep cliff face, jutting out from the coast into a large body of water (usually the sea or a lake); a bold promontory or a high cape.  (b) The high ground flanking a body of water, such as a cove.  (c) The steep crag or cliff face of a promontory.  GG


geomfdesc:
A sharp-crested, symmetric (homoclinal) ridge formed by highly tilted resistant rock layers; produced by differential erosion of interlayered resistant and weak rocks with dips greater than about 25o (45 percent).  Compare - cuesta.  HP


geomfdesc:
A high, rocky, sharp pointed, steep-sided, mountain peak with prominent faces and ridges, bounded by the intersecting walls of three or more cirques that have been cut back into the mountain by headward erosion of glaciers.  GG


geomfdesc:
(a) (not preferred - see hillock) An imprecise, general term for a rounded or conical mound or other small elevation.  (b) (not preferred) A slight rise of ground above a level surface.  GG.


geomfdesc:
A tributary valley whose floor at the lower end is notably higher than the floor of the main valley in the area of junction.  GG


geomfdesc:
A stream, or reach of a stream, that does not flow year-round  (commonly dry for 3 or more months out of 12) and whose channel is generally below the local water table; it flows only when a) it receives baseflow solely during wet periods, or b) it receives ground-water discharge or protracted contributions from melting snow or other erratic surface and shallow subsurface sources.  Compare - ephemeral stream.  HP


geomfdesc:
A low mound, knob, hummock, or short irregular ridge, composed of stratified sand and gravel deposited by a subglacial stream as a fan or delta at the margin of a melting glacier; by a supraglacial stream in a low place or hole on the surface of the glacier; or as a ponded deposit on the surface or at the margin of stagnant ice.  Compare - crevasse filling, kame moraine, kame terrace, esker, outwash.  GG


geomfdesc:
A steep-sided, bowl-shaped depression commonly without surface drainage (closed depression) in drift deposits, often containing a lake or swamp, and formed by the melting of a large, detached block of stagnant ice that had been wholly or partly buried in the drift.  Kettles range in depth from 1 to tens of meters, and with diameters up to 13 km.  Compare - pothole.  GG


geomfdesc:
A small, low, rounded hill rising above adjacent landforms.  HP


geomfdesc:
(a) A rounded eminence, a small hill or mountain; especially a prominent or isolated hill with steep sides, commonly found in the Southern United States.  (b) A peak or other projection from the top of a hill or mountain.  Also, a boulder or group of boulders or an area of resistant rocks protruding from the side of a hill or mountain.  GG


geomfdesc:
A terrace-like ridge consisting of stratified sand and gravel (a) deposited by a meltwater stream flowing between a melting glacier and a higher valley wall or lateral moraine, and (b) left standing after the disappearance of the ice.  It is commonly pitted with "kettles" and has an irregular ice-contact slope.  HP


geomfdesc:
(a) A narrow shelf or projection of rock, much longer than wide, formed on a rock wall or cliff face, as along a coast by differential wave action on softer rocks; erosion is by combined biological and chemical weathering.  (b) A rocky outcrop; solid rock.  (c) A shelf-like quarry exposure or natural rock outcrop.  Compare - structural bench.  GG


geomfdesc:
A ridge-like moraine carried on and deposited at the side margin of a valley glacier.  It is composed chiefly of rock fragments derived from valley walls by glacial abrasion and plucking, or colluvial accumulation from adjacent slopes.  GG


geomfdesc:
A narrow shelf, partly cut and partly built, produced along a lake shore in front of a scarp line of low cliffs and later exposed when the water level falls.  GG


geomfdesc:
An artificial or natural embankment built along the margin of a watercourse or an arm of the sea, to protect land from inundation or to confine streamflow to its channel.  Compare - artificial levee, natural levee.  GG


geomfdesc:
The flat, usually bare ground situated seaward of a salt marsh and regularly covered and uncovered by the tide; e.g., a mud flat.  GG


geomfdesc:
Periodically wet or continually flooded areas with the surface not deeply submerged.  Covered dominantly with sedges, cattails, rushes, or other hydrophytic plants.  Compare - salt marsh, swamp, bog, fen.  GSST


geomfdesc:
A broad, nearly flat-topped, and usually isolated landmass bounded by steep slopes or precipitous cliff and capped by layers of resistant, nearly horizontal, rocky summit width greater than the height of bounding escarpments.  (Colloquial: western USA; not preferred)  Also used to designate broad structural benches and alluvial terraces that occupy intermediate levels in stepped sequences of platforms bordering canyons and valleys.  Compare - butte, plateau, cuesta.  HP & GG


geomfdesc:
A relatively level area of fine grained material (e.g. silt) along a shore (as in a sheltered estuary) or around an island, alternately covered and uncovered by the tide or covered by shallow water, and barren of vegetation.  Compare - low marsh, tidal flat, tidal marsh.  GG


geomfdesc:
A term used for one of numerous low circular or oval domes composed of loose, unstratified, gravelly, silty, or sandy material.  The basal diameter varies from 3 meters to more than 30 meters, and the height from 30 centimeters to about 2 meters.  Compare - pimple mound, patterned ground, shrub-coppice dune.  GG


geomfdesc:
(not recommended) use disintegration moraine.


geomfdesc:
(a)  A crescent-shaped, concave or linear mark on the face of a bluff or valley wall, produced by the lateral erosion of a meandering stream which impinged upon and undercut the bluff; if it's no longer adjacent to the modern stream channel it indicates an abandoned route of the stream.  SW;  (b) (not recommended - refer to oxbow)  An abandoned meander, commonly filled in by deposition and vegetation, but still discernible.  GG


geomfdesc:
A constructional coastal strip, sloping gently seaward, veneered by marine deposits (typically silt, sand, fine gravel).  Compare - terrace, wave-built terrace.  GG


geomfdesc:
An isolated hill, knob, ridge, or peak of bedrock that projects prominently above the surface of a glacier and is completely surrounded by glacier ice.  Compare - inselberg, monadnock.  GG


geomfdesc:
An extensive lowland area of coarse textured, glaciofluvial material.  An outwash plain is commonly smooth; where pitted, due to melt-out of incorporated ice masses (pitted outwash plain), it is generally low in relief and largely retains it-s original gradient.  Compare - outwash, pitted outwash plain, kettles.  HP


geomfdesc:
A flat-topped bank of outwash with an abrupt outer face (scarp or riser) extending along a valley downstream from an outwash plain or terminal moraine; a valley train deposit.    Compare - kame terrace, valley train.  GG


geomfdesc:
A closely looping stream meander having an extreme curvature such that only a neck of land is left between the two parts of the stream.  (colloquial: northeastern U.S.A.) the land enclosed, or partly enclosed, within an oxbow.  Compare - meander belt, oxbow lake, bayou.  GG


geomfdesc:
A dune largely composed of silt and sand-sized aggregates of clay; sometimes called a clay dune or lunette.    Compare - parna.  HP


geomfdesc:
A gently sloping erosional surface developed at the foot of a receding hill or mountain slope.  The surface may be essentially bare, exposing earth material that extends beneath adjacent uplands; or it may be thinly mantled with alluvium and colluvium, ultimately in transit from upland front to basin or valley lowland.  In hill-foot slope terrain the mantle is designated "pedisediment."  The term has been used in several geomorphic contexts:  Pediments may be classed with respect to (a) landscape positions, for example, intermontane-basin piedmont or valley-border foot slope surfaces (respectively, apron and terrace pediments (Cooke and Warren, 1973)); (b) type of material eroded, bedrock or regolith; or (c) combinations of the above.  Compare - Piedmont slope.  HP


geomfdesc:
A general term for any ground surface exhibiting a discernibly ordered, more-or-less symmetrical, morphological pattern of ground and, where present, vegetation.  Patterned ground is characteristic of, but not confined to, permafrost regions or areas subjected to intense frost action; it also occurs in tropical, subtropical, and temperate areas.  Patterned ground is classified by type of pattern and presence or absence of sorting and includes nonsorted and sorted circles, net, polygons, steps and stripes, garlands, and solifluction features.  In permafrost regions, the most common macroform is the ice-wedge polygon and a common microform is the nonsorted circle.  Stone polygons generally form on slopes of less than 8 percent, while garlands and stripes occur on slopes of 8 to 15 percent and more than 15 percent, respectively.  NRC and HP


geomfdesc:
A type of  small pit or closed depression (1 to 15 meters deep), generally circular or elliptical, occurring in an outwash plain, a recessional moraine, or a till plain.  GG


geomfdesc:
A large frost mound; especially a relatively large conical mound of soil-covered ice (commonly 30 to 50 meters high and up to 400 meters in diameter) raised in part by hydrostatic pressure within and below the permafrost of Arctic regions, and of more than 1 year's duration.  GG


geomfdesc:
Sharp or rugged upward extension of a ridge chain, usually at the junction of two or more ridges; the prominent highest point of a summit area.  HP


geomfdesc:
The usually dry and nearly level lake plain that occupies the lowest parts of closed depressions, such as those occurring on intermontane basin floors.  Temporary flooding occurs primarily in response to precipitation-runoff events.  Playa deposits are fine grained and may or may not have high water table and saline conditions.  HP


geomfdesc:
(colloquial: southeastern U.S.A.)  A large wet area on broad, commonly a swamp, which occurs on nearly level interfluves in the Atlantic coastal plain with distinctive, native vegetation relative to adjacent areas.  Soils may be either mineral or organic.  A Native American term for "swamp on a hill."   Compare - raised bog.  RD


geomfdesc:
An area of acid, peaty soil, especially that developed from moss, in which the center is higher than the margins.  Compare - pocosin, Carolina Bay, moss peat.  [Note: raised peat bog (not preffered) - refer to highmoor bog].   GG


geomfdesc:
A long, narrow elevation of the land surface, usually sharp crested with steep sides and forming an extended upland between valleys.  The term is used in areas of both hill and mountain relief.  HP


geomfdesc:
An end or lateral moraine, built during a temporary but significant halt in the final retreat of a glacier.  Also, a moraine built during a minor readvance of the ice front during a period of general recession.  Compare - end moraine, ground moraine, terminal moraine.  GG


geomfdesc:
A small stream channel; narrow, steep-sided, commonly V-shaped in cross section and larger than a gully, cut in unconsolidated materials.  General synonym (not preferred) - gulch.  Compare - arroyo, draw, gully.  HP


geomfdesc:
A low point on a ridge or interfluve, generally a divide (pass, col) between the heads of streams flowing in opposite directions.  Compare - summit, crest.  HP


geomfdesc:
A platform-like, nearly level to gently inclined erosional surface developed on resistant strata in areas where valleys are cut in alternating strong and weak layers with an essentially horizontal attitude.  Structural benches are bedrock controlled, and in contrast to stream terraces, have no geomorphic implication of former, partial erosion cycles and base-level controls, nor do they represent a stage of flood-plain development following an episode of valley trenching.  Compare - pediment, ledge; see scarp.  HP


geomfdesc:
(a) A shallow, open depression in unconsolidated materials which lacks a defined channel but can funnel overland or subsurface flow into a drainageway.  Soils in swales tend to be more moist and thicker (cummulic) compared to surrounding soils.  SW  (b) A small, shallow, typically closed depression in an undulating ground moraine formed by uneven glacial deposition; Compare - swell-and-swale topography.  (c) (not preferred; refer to interdune)  A long, narrow, generally shallow, trough-like depression between two beach ridges, and aligned roughly parallel to the coastline.  GG


geomfdesc:
A large, sharp-crested, elongated, longitudinal (linear) dune or chain of sand dunes, oriented parallel, rather than transverse (perpendicular), to the prevailing wind.  If unmodified, the crest, in profile, commonly consists of a succession of curved slip faces produced by strong, but infrequent cross winds.  A seif dune may be as much as 200 m high and from 400 m to more than 100 km long.  Compare - longitudinal dune. GG and HP


geomfdesc:
(a) A small marsh, especially a marshy area lying in a local, shallow, closed depression on a piece of dry land, as on  the prairie of the midwestern U.S.A.  (b) A term used, especially in the Mississippi Valley, for a creek or sluggish body of water in a tidal flat, flood plain, or coastal marshland.  Compare - bayou, oxbow.  (c) A sluggish channel of water, such as a side channel of a river, in which water flows slowly through low, swampy ground, as along the Columbia River, or a section of an abandoned river channel which may contain stagnant water and occurs in a flood plain or delta.  (d) (not preferred) An area of soft, miry, muddy or waterlogged ground, a place of deep mud.  GG


geomfdesc:
Flat, poorly drained area that is subject to periodic or occasional overflow by salt water, containing water that is brackish to strongly saline, and usually covered with a thick mat of grassy halophytic plants; e.g., a coastal marsh periodically flooded by the sea, or an inland marsh, (or salina) in an arid region and subject to intermittent overflow by salty water.  Compare - tidal marsh, mud flat.  GG


geomfdesc:
An isolated tongue-shaped feature up to 25 m wide and 150 m or more long, formed by rapid solifluction on certain sections of a slope showing variations in gradient.  This feature commonly has a steep (e.g. 15-60 degrees) front and a relatively smooth upper surface.  NRC


geomfdesc:
(a) A small point or low tongue or narrow embankment of land, commonly consisting of sand or gravel deposited by longshore transport and having one end attached to the mainland and the other terminating in open water, usually the sea; a finger-like extension of the beach. (b) A relatively long, narrow shoal or reef extending from the shore into a body of water.  GG


geomfdesc:
An island-like area of older rock surrounded by a lava flow.  Compare - kipuka.  HP


geomfdesc:
An area of low, saturated ground, intermittently or permanently covered with water, and predominantly vegetated by shrubs and trees, with or without the accumulation of peat.  Compare - marsh, bog, fen.  GG


geomfdesc:
A very asymmetric sand dune elongated perpendicular to the prevailing wind direction, having a gentle windward slope and a steep leeward slope standing at or near the angle of repose of sand; it generally forms in areas of sparse vegetation. Compare - longitudinal dune. GG


geomfdesc:
A step-like surface, bordering a valley floor or shoreline, that represents the former position of a flood plain, or lake or sea shore.  The term is usually applied to both the relatively flat summit surface (tread), cut or built by stream or wave action, and the steeper descending slope (scarp, riser), graded to a lower base level of erosion.  Compare - stream terrace, flood-plain step.  HP.  [ soil survey] Practically, terraces are considered to be generally flat alluvial areas above the 100 yr. flood stage.  SW


geomfdesc:
An extensive, nearly horizontal, barren or sparsely vegetated tract of land that is alternately covered and uncovered by the tide, and consists of unconsolidated sediments (mostly clays, silts and/or sand).  It may form the top surface of a deltaic deposit. Compare - tidal marsh. GG


geomfdesc:
An extensive, nearly level marsh bordering a coast (as in a shallow lagoon, sheltered bay or estuary) and regularly inundated by high tides; formed mostly of unconsolidated sediments (e.g. clays, silts, and/or sands, and organic materials), and the resistant root mat of salt tolerant plants; a marshy tidal flat.  Compare - tidal flat.  GG


geomfdesc:
(a)  Any long, narrow depression in the earth's surface, such as one between hills or with no surface outlet for drainage.  (b)  (not preferred - see U-shaped valley,  mountain valley)  A broad, elongate U-shaped valley, such as a glacial trough.  Compare - U-shaped valley.  GG


geomfdesc:
A conical hill of lava and/or pyroclastics that is built up around a volcanic vent.  GG


geomfdesc:
The sloping to very steep surfaces between the valley floor and summits of adjacent uplands.  Well-defined, steep valley sides have been termed valley walls (not recommended).  Note:  Scale, relief, and perspective may require use of closely related terms such as hill slope or mountain slope.  HP


geomfdesc:
A long narrow body of outwash confined within a valley beyond a glacier; it may, or may not, emerge from the valley and join an outwash plain.  GG


geomfdesc:
A gently sloping surface produced by wave erosion, extending into the sea or lake from the base of the wave-cut cliff.  It represents both the wave-cut bench and the abrasion platform.  GG


geomfdesc:
A gently sloping coastal feature at the seaward or lakeward edge of a wave-cut platform, constructed by sediment brought by rivers or drifted along the shore or across the platform and deposited in the deeper water beyond.  Compare - beach plain, strand plain.  GG


geomfdesc:
A type of thermokarst depression with steep sides and a flat, grass-covered floor, found in thermokarst terrain, produced by thawing of extensive areas of very thick and exceedingly ice-rich permafrost.  Compare - thermokarst depression.  NRC and GG


geomfdesc:
A generic term for an elevated area of the land surface, rising at least 30 m (100 ft.) to as much as 300 meters (approx. 1000 ft.) above surrounding lowlands, usually with a nominal summit area relative to bounding slopes, a well-defined, rounded outline and slopes that generally exceed 15 percent.  A hill can occur as a single, isolated mass or in a group.  A hill can be further specified based on the magnitude of local relief: low hill (30 - 90 m) or high hill (90 - 300 m).  Informal distinctions between a hill and a mountain are often arbitrary and dependent on local convention. Compare - hillock, plateau, mountain, foothills, hills.  SW &  HP


geomfdesc:
An elongated block that is bounded on both sides by normal faults that dip away from the interior of the horst.  It is a structural form and may or may not be expressed geomorphically.  GG


geomfdesc:
A prominent, isolated, residual knob, hill, or small mountain, usually smoothed and rounded, rising abruptly from an extensive lowland erosion surface in a hot dry region; generally bare and rocky although the lower slopes are commonly buried by colluvium.  Compare - monadnock, nunatak.  GG


geomfdesc:
(colloquial; southwestern USA)  The flood plain of an ephemeral stream that is confined between the fan remnants, ballenas, basin-floor remnants, or closely-opposed fan toeslopes of a basin.  FF & SW.


geomfdesc:
The relatively flat surface, whether sand-free or sand-covered, between dunes;  GG


geomfdesc:
A landform composed of the relatively undissected upland or ridge between two adjacent valleys containing streams flowing in the same general direction.  An elevated area between two drainageways that sheds water to those drainageways.  Compare - divide.  GG & FFP


geomfdesc:
A generic term for wide structural depressions between mountain ranges that are partly filled with alluvium and called "valleys" in the vernacular.  Intermontane basins may be drained internally (bolsons) or externally (semi-bolson).  FFP


geomfdesc:
(a)  An end moraine that contains numerous kames.  (b)  A group of kames along the front of a stagnant glacier, commonly comprising the slumped or erosional remnants of a formerly continuous outwash plain built up over the foot of rapidly wasting or stagnant ice.  GG


geomfdesc:
The process, associated sediments or resultant landform characterized by a mudflow composed chiefly of volcaniclastic materials on or near the flank of a volcano.  The debris carried in the flow includes pyroclastic material, blocks from primary lava flows, and epiclastic material.  Thick flows can exhibit a crude (poorly sorted) upward-fining sediment sequence.  Compare - mudflow.  SW & GG


geomfdesc:
The flat to gently undulating ground underlain or composed of fine-grained sediments deposited in a former lake.


geomfdesc:
A nearly level surface marking the floor of an extinct lake filled by well-sorted, generally fine-textured, stratified deposits, commonly containing varves.  GG


geomfdesc:
The narrow strip of land in contact with or bordering a lake; especially the beach of a lake.  GG


geomfdesc:
A general, encompassing term for most types of mass movement landforms and processes involving the downslope transport and outward deposition of soil and rock materials, caused by gravitational forces and which may or may not involve saturated materials.  Names of landslide types generally reflect the dominant process and/or the resultant landform.  The main operational categories of mass movement are fall (rockfall, soil fall, topple), slide (rotational landslide, block glide, debris slide, lateral spread), flow [rock fragment flow, (especially rockfall avalanche), debris avalanche, debris flow (e.g., lahar), earthflow (creep, mudflow)], and complex landslides.  Compare - solifluction.  SW & DV


geomfdesc:
A broad area of nearly level land, that can be localized but is commonly hundreds of square kilometers in extent, covered by a relatively thin succession of primarily basaltic lava flows resulting from fissure eruptions.  Compare - lava plateau, lava field, volcanic field.  SW & GG


geomfdesc:
A broad elevated tableland or flat-topped highland, that may be localized but commonly is many hundreds or thousands of square kilometers in extent, underlain by a thick succession of basaltic lava flows resulting from fissure eruptions (e.g. Columbia River Plateau).  Compare - lava plain, lava field.  GG


geomfdesc:
A narrow, elongate, coarse-textured ridge that once rose near to, or barely above, a pluvial or glacial lake and extended generally parallel to the shore but was separated from it by an intervening trough or lagoon; both the bar and lagoon are now relict features.  GG


geomfdesc:
A hill or ridge composed  of a lava flow remnant that caps or is exposed in a tilted fault block and bounded by a dip slope.  Used as evidence of block faulting in Basin-and-Range terrain (western USA).  Compare - hogback.  GG


geomfdesc:
A bog that is at or only slightly above the water table, on which it depends for accumulation and preservation of peat (chiefly the remains of sedges, reeds, shrubs, and various mosses).  Compare - highmoor bog, raised bog.  GG


geomfdesc:
One of a series of regular freely developing sinuous curves, bends, loops, turns, or windings in the course of a stream.  GG.


geomfdesc:
The term "meandering" should be restricted to loops with channel length more than 1.5 to 2 times the meander wave length.  Meandering stream channels commonly have cross sections with low width-to-depth ratios, cohesive (fine-grained) bank materials, and low gradient.  At a given bank-full discharge, meandering streams have gentler slopes, and deeper narrower, and more stable channel cross sections than braided streams.  Compare - meander, braided stream, flood-plain landforms.  HP & RR


geomfdesc:
(a) One of a series of long, parallel, close fitting, crescent-shaped ridges and troughs formed along the inner bank of a stream meander as the channel migrated laterally down-valley and toward the outer bank.  Compare - meander belt, point bar.  (b) (not recommended; refer to oxbow lake) - A small, elongate lake on a flood plain in a well-defined part of an abandoned stream channel.  GG


geomfdesc:
(a) An elongate moraine carried in or upon the middle of a glacier and parallel to its sides, usually formed by the merging of adjacent and inner lateral moraines below the junction of two coalescing valley glaciers.  (b) A moraine formed by glacial abrasion of a rocky protuberance near the middle of a glacier and whose debris appears at the glacier surface in the ablation area.  (c) The irregular ridge left behind in the middle of a glacial valley, when the glacier on which it was formed has disappeared.  GG


geomfdesc:
An isolated hill or mountain of resistant rock rising conspicuously above the general level of a lower erosion surface in a temperate climate representing an isolated remnant of a former erosion cycle in an area that has largely been beveled to its base level.  Compare - inselberg, nunatak.  GG


geomfdesc:
A unit of folded strata that dips from the horizontal in one direction only, is not part of an anticline or syncline, and occurs at the earth's surface..  This structure is typically present in plateau areas where nearly flat strata locally assume steep dips caused by differential vertical movements without faulting.  Compare - anticline, syncline, fold.  SW & HP


geomfdesc:
A general term for a landform composed mainly of till that has been deposited by a glacier; a kame moraine is a type of  moraine similar in exterior form to other types of moraines but composed mainly of stratified outwash materials.  Types of moraine include: disintegration, end, ground, kame, lateral, recessional, and terminal.  SW


geomfdesc:
A generic term for an elevated area of the land surface, rising more than 300 meters above surrounding lowlands, usually with a nominal summit area relative to bounding slopes and generally with steep sides (greater than 25 percent slope) with or without considerable bare-rock exposed.  A mountain can occur as a single, isolated mass or in a group forming a chain or range.  Mountains are primarily formed by tectonic activity and/or volcanic action and secondarily by differential erosion.  Compare - hill, hillock, plateau, foothills, mountains. SW & HP


geomfdesc:
A part of a mountain between the summit and the foot.  Compare - mountainflank, hillslope.  GG


geomfdesc:
(a) Any small, externally drained V-shaped depression (in cross-section) cut or deepened by a stream and floored with alluvium, or a broader, U-shaped depression modified by an alpine glacier and floored with either till or alluvium, that occurs on a mountain or within mountains.  Several types of mountain valleys can be recognized based on their form and valley floor sediments (i.e., V-shaped valley, U-shaped valley).  Compare - valley.  SW (b) (colloquial: Basin and Range, USA)  A relatively small, structural depression within a mountain range that is partly filled with alluvium and commonly drains externally to an intermontane basin, bolson, or semi-bolson.  Compare - valley flat.  SW &  FFP


geomfdesc:
The process, associated sediments (mudflow deposit) or resultant landform characterized by a very rapid type of earthflow dominated by a sudden, downslope movement of a mass of rock, soil, and mud (more than 50% of the particles are < 2 mm), that behaves much as a viscous fluid when moving.  Compare - debris flow, flow, landslide.  SW


geomfdesc:
A bog, usually a sphagnum bog, frequently with grassy tussocks (hummocks), growing in wet, poorly drained boreal regions, with deep accumulations of organic material, often in areas of permafrost; a moss-covered muck or peat bog of boreal regions.  GG  and HP


geomfdesc:
A long, broad low ridge or embankment of sand and coarse silt, built by a stream on its flood plain and along both sides of its channel, especially in time of flood when water overflowing the normal banks is forced to deposit the coarsest part of its load. It has a gentle slope away from the river and toward the surrounding floodplain, and its highest elevation is closest to the river bank.  Compare - levee, artificial levee, meander belt.  GG


geomfdesc:
(a) (colloquial - northeast USA) A narrow passageway, or short defile between mountains; a deep, close pass.  Compare - gap.  (b) A breached opening in the rim of a volcanic crater.  GG


geomfdesc:
A fan-shaped accumulation of outwash deposited by meltwater streams in front of the end moraine of a glacier.  Coalescing outwash fans form an outwash plain.  GG


geomfdesc:
The crescent-shaped, often ephemeral body of standing water situated by the side of a stream in the abandoned channel (oxbow) of a meander after the stream formed a neck cutoff and the ends of the original bend were silted up.  Compare - meander belt, oxbow.  GG


geomfdesc:
(colloquial: midwestern USA) Commonly an erosional remnant modified by depositional processes consisting of a low, elongated, rounded ridge or hill consisting mainly of drift, rock, or windblown sand, silt, or clay capped with a thick cover of loess; found especially in northeast Iowa.  Height varies between 10 and 30 m.  GG


geomfdesc:
A sand dune with a long, scoop-shaped form, convex in the downwind direction so that its horns point upwind, whose ground plan, when perfectly developed, approximates the form of a parabola.  GG


geomfdesc:
(not preferred) refer to ballena  - (colloquial: western U.S.A.)  A fan remnant having a distinctively-rounded surface of fan alluvium.  The ballena's broadly-rounded shoulders meet from either side to form a narrow summit and merge smoothly with concave sideslopes and then concave, short pediments which form smoothly-rounded drainageways between adjacent ballenas.  A partial ballena is a fan remnant large enough to retain some relict fan surface on a remnant summit.  Compare - fan remnant.  Modified from FFP


geomfdesc:
A generally flat-topped expanse of peat, elevated above the general surface of a peatland, and containing segregated ice that may or may not extend downward into the underlying mineral soil.  Controversy exists as to whether peat plateaus and palsen are morphological variations of the same feature.  NRC


geomfdesc:
An outwash plain marked by many irregular depressions such as kettles, shallow pits, and potholes which formed by melting of incorporated ice masses; much of the gradient and internal structures of the original plain remain intact; many are found in WI, MN, MI, and IN.  Compare - collapsed outwash plain, outwash, pitted outwash.  GG


geomfdesc:
A general term referring to any flat, lowland area, large or small, at a low elevation.  Specifically, any extensive region of comparatively smooth and level gently undulating land.  A plain has few or no prominent hills or valleys but sometimes has considerable slope, and usually occurs at low elevation relative to surrounding areas.  Where dissected, remnants of a plain can form the local uplands.  A plain may be forested or bare of trees and may be formed by deposition or erosion.  Compare - lowland, plateau.  GG


geomfdesc:
A comparatively flat area of great extent and elevation; specifically an extensive land region considerably elevated (more than 100 meters) above adjacent lower-lying terrain, and is commonly limited on at least one side by an abrupt descent, has a flat or nearly level surface.  A comparatively large part of a plateau surface is near summit level.  Compare - hill, foothill, mountain, mesa, plain.  GG


geomfdesc:
A volcanic dome characterized by an upheaved, consolidated conduit filling.  GG


geomfdesc:
A lake formed in a period of exceptionally heavy rainfall; a lake formed in the Pleistocene Epoch during a time of glacial advance, and now either extinct (relict) or existing as a remnant (lake); e.g., Lake Bonneville.  Compare - glacial lake, proglacial lake.  GG


geomfdesc:
One of a series of low, arcuate ridges of sand and gravel developed on the inside of a growing meander by the slow addition of individual accretions accompanying migration of the channel toward the outer bank.  Compare - meander scroll.  GG


geomfdesc:
An elongated uplift of the congealing crust of a lava flow, probably due to the pressure of the underlying, still-flowing lava; commonly < 5 m in height (but range up to 15 m) and < 100 m length (but can exceed 500 m).  Compare - tumulus.  SW, GG, & GS


geomfdesc:
An ancient (relict) beach occurring above the present shoreline and separated from the present beach, having been elevated above the high-water mark either by local crustal movements (uplift) or by lowering of sea level, and often bounded by inland cliffs.  GG


geomfdesc:
(a) A ridge-like or mound-like structure, layered or massive, built by sedentary calcareous organisms, especially corals, and consisting mostly of their remains; it is wave-resistant and stands above the surrounding contemporaneously deposited sediment.  Also, such a structure built in the geologic past and now enclosed in rock, commonly of differing lithology.  (b) A mass or ridge of rocks, especially coral and sometimes sand, gravel, or shells, rising above the surrounding sea or lake bottom to or nearly to the surface, and dangerous to navigation; specifically such a feature at 10 fathoms (18.3 m) or less, formerly 6 fathoms (11 m).  GG


geomfdesc:
A nutrient-rich wetland with a surface pattern of ridges and depressions.


geomfdesc:
The border, margin, edge, or face of a landform, such as the curved brim surrounding the top part of a crater or caldera; specifically the rimrock of a plateau or canyon.  GG


geomfdesc:
A small elongate protruding knob or hillock of bedrock, so sculptured by a large glacier as to have its long axis oriented in the direction of ice movement, an upstream (stoss or scour) side that is gently inclined, smoothly rounded, and striated, and a downstream (lee or pluck) side that is steep and rough.  It is usually a few meters in height, length, and breadth.  GG


geomfdesc:
A mass of poorly sorted angular boulders and fine material, with interstitial ice a meter or so below the surface (ice-cemented) or containing a buried ice glacier (ice-cored).  It occurs in a permafrost area, and is derived from a cirque wall or other steep cliff.  Rock glaciers have the general appearance and slow movement of small valley glaciers, ranging from a few hundred meters to several kilometers in length, and having a distal area marked by a series of transverse, arcuate ridges.  GG


geomfdesc:
A flow of wet sand, as along banks of noncohesive clean sand that is subject to scour and to repeated fluctuations in pore-water pressure due to rise and fall of the tide.  GG


geomfdesc:
A large, irregularly shaped, commonly thin, surficial mantle of eolian sand, lacking the discernible slip faces that are common on dunes.  GG


geomfdesc:
An escarpment, cliff, or steep slope of some extent along the margin of a plateau, mesa, terrace, or structural bench.  A scarp may be of any height.  Compare - escarpment.  GG


geomfdesc:
A cliff or slope produced by wave erosion, situated at the seaward edge of the coast or the landward side of the wave-cut platform.  It may vary from an inconspicuous slope to a high, steep escarpment.  GG


geomfdesc:
A surficial ridge, bank, or bar consisting of sand or other subaqueous deposit that has become permanently exposed by the retreat or lowering of a proglacial lake other body of water.  Compare - longshore bar [relict].  GG


geomfdesc:
The intersection of a specified plane of water with the beach; it migrates with changes of the tide or of the water level.  Compare - strand line, shore complex, beach, swash zone.   GG


geomfdesc:
A small, streamlined dune that forms around brush and clump vegetation.  GG


geomfdesc:
A closed, circular or elliptical depression, commonly funnel-shaped, characterized by subsurface drainage and formed either by dissolution of the surface of underlying bedrock (e.g., limestone, gypsum, salt) (solution sinkhole) or by collapse of underlying caves within bedrock (collapse sinkhole); diameters range from a few meters to as much as 1000 m.  Complexes of sinkholes in carbonate-rock terrain are the main components of karst topography.  Synonym (not preferred) - doline.  Compare - karst valley, interior valley, cockpit.  SW & WW


geomfdesc:
a) - A category of mass movement processes, associated sediments (slide deposit) or resultant landforms (e.g., rotational slide, translational slide, and snowslide) characterized by a failure of earth, snow, or rock under shear stress along one or several surfaces that are either visible or may reasonably be inferred.  The moving mass may or may not be greatly deformed, and movement may be rotational (rotational slide) or planar (translational slide).    A slide can result from lateral erosion, lateral pressure, weight of overlying material, accumulation of moisture, earthquakes, expansion owing to freeze-thaw of water in cracks, regional tilting, undermining, fire, and human agencies.  Compare -fall, topple, lateral spread, flow, complex landslide.  SW & DV  (b) The track of bare rock or furrowed earth left by a slide.  (c) The mass of material moved in or deposited by a slide.  Compare - fall, flow, complex landslide, landslide.  SW & GG


geomfdesc:
(a) (not preferred- refer to rotational slide) A generic, obsolete term for various types of landslides, especially rotational landslide; the process, associated sediments, or resultant landform characterized by a slide involving a shearing and rotary movement of a generally independent mass of rock or earth along a curved slip surface (concave upward) and about an axis parallel to the slope from which it descends, and by backward tilting of the mass with respect to that slope so that the slump surface often exhibits a reversed slope facing uphill.  Compare - rotational slide, slide, landslide.  SW, GG, & DV.  (b) (not recommended) refer to rotational slide.  An informal term for the landform or mass of material slipped down during, or produced by a landslide.  GG & DV


geomfdesc:
TheA mass of material torn away as a coherent unit during a landslide; a largely intact but displaced and commonly reoriented body of rock or soil.  SW & GG


geomfdesc:
A subordinate ridge or lesser elevation that projects sharply from the crest or side of a hill, mountain, or other prominent range of hills or mountains.  GG


geomfdesc:
A steep-sided mass of rock rising above its surroundings on all sides from a slope or hill.  GG


geomfdesc:
A prograded shore built seaward by waves and currents, and continuous for some distance along the coast.  It is characterized by subparallel beach ridges and swales, in places with associated dunes.  GG


geomfdesc:
A type of stream terrace, formed as an erosional surface cut on bedrock and thinly mantled with stream deposits (alluvium).


geomfdesc:
A volcano that is constructed of alternating layers of lava and pyroclastic deposits, along with abundant dikes and sills.  Viscous, acidic lava may flow from fissures radiating from a central vent, from which pyroclastics are ejected.  Compare - shield volcano.  GG


geomfdesc:
One or a series of platforms in a stream valley, flanking and more or less parallel to the stream channel, originally formed near the level of the stream, and representing the remnants of an abandoned flood plain, stream bed, or valley floor produced during a former state of fluvial erosion or deposition (i.e., currently very rarely or never floods; inactive cut and fill and/or scour and fill processes).  Erosional surfaces cut into bedrock and thinly mantled with stream deposits (alluvium) are called "strath terraces."  Remnants of constructional valley floors thickly mantled with alluvium are called alluvial terraces.  Compare - alluvial terrace, flood-plain step, strath terrace, terrace.  HP & SW


geomfdesc:
A peatland with rough parallel narrow ridges of peat dominated by peat vegetation interspersed with slight depressions, many of which contain shallow pools.  The ridges are at right angles to low < 2o slopes.  They are typically 1 to 3 m wide, up to 1 m high and may be over 1 km long.  The ridges are slightly elevated and are better drained allowing shrubs and trees to grow.  They are best developed in areas of discontinuous permafrost.  NRC


geomfdesc:
A unit of folded strata that is concave upward.  In a simple syncline, beds forming the opposing limbs of the fold dip toward its axial plane.  Compare - anticline, monocline.  HP


geomfdesc:
An end moraine that marks the farthest advance of a glacier and usually has the form of a massive arcuate or concentric ridge, or complex of ridges, underlain by till and other drift types.  Compare - end moraine, recessional moraine, ground moraine.  HP and GG


geomfdesc:
A hollow in the ground resulting from subsidence following the local melting of ground ice in a permafrost region.  GG


geomfdesc:
An extensive, flat to gently undulating area underlain predominantly by till and bounded on the distal end by subordinate recessional or end moraines.  Compare - till, ground moraine.  SW


geomfdesc:
A sand or gravel bar or barrier that connects an island with the mainland or with another island.  GG


geomfdesc:
A high, isolated pinnacle, or rocky peak; or a pile of rocks, much-jointed and usually granitic, exposed to intense weathering, and often assuming peculiar or fantastic shapes.  GG


geomfdesc:
A category of mass movement processes, associated sediments (translational slide deposit) or resultant landforms characterized by the extremely slow to moderately rapid downslope displacement of comparatively dry soil-rock material on a surface (slip face) that is roughly parallel to the general ground surface, in contrast to falls topples, and rotational slides.  The term includes such diverse slide types as translational debris slides, translational earth slide, translational rock slide, block glides, and slab or flake slides. .  Compare - rotational slide, slide, landslide.  SW, DV, GG


geomfdesc:
A relatively shallow trench or depression cut into drift and other loose material, or in bedrock, by a subglacial stream not loaded with coarse sediment that may or may not be part of the present day drainage pattern.  GG


geomfdesc:
A valley having a pronounced parabolic cross profile suggesting the form of a broad letter "U", with steep walls and a broad, nearly flat floor; specifically a valley carved by glacial erosion.  Compare - V-shaped valley.  GG


geomfdesc:
An elongate, relatively large, externally drained depression of the Earth's surface that is primarily developed by stream erosion or glacial activity.  Compare - basin.  HP


geomfdesc:
A generic term for the low or relatively level ground lying between valley walls and bordering a stream channel; especially the small plain at the bottom of a narrow, steep-sided valley.  The term can be generally applied noncommittally to a flat surface that cannot be identified with certainty as a floodplain or terrace.  Compare - backswamp, meander belt.  GG


geomfdesc:
A general term for the nearly level to gently sloping, lowest surface of a valley.  Landforms include axial stream channels, the flood plain, flood-plain steps, and, in some areas, low terrace surfaces.  Compare - flood-plain landforms, meander, braided channel, valley side.  HP


geomfdesc:
A steep-sided, rounded extrusion of highly viscous lava squeezed out from a volcano, and forming a dome-shaped or bulbous mass of congealed lava above and around the volcanic vent.  GG


geomfdesc:
(a) A vent in the surface of the Earth through which magma and associated gases and ash erupt; also, the form or structure, usually conical, that is produced by the ejected material.  (b) Any eruption of material, e.g. mud, that resembles a magmatic volcano.  GG '87


geomfdesc:
A valley having a pronounced cross profile suggesting the form of the letter "V", characterized by steep sides and short tributaries; specifically a narrow valley resulting from downcutting by a stream.  The "V" becomes broader as the downcutting progresses.  Compare - U-shaped valley.  GG


geomfdesc:
(colloquial: western U.S.A.)  The broad, flat-flooded channel of an ephemeral stream, commonly with very steep to vertical banks cut in alluvium.  Note:  When channels reach intersect zones of ground-water discharge they are more properly classed as "intermittent stream" channels.  Synonym - arroyo.  Compare - gully.  HP


geomfdesc:
A fan-like deposit of sand washed over a barrier island during a storm.  GG


geomfdesc:
A valley, commonly in karst, that ends abruptly downstream at the point at which its stream disappears underground.  GG


geomfdesc:
A solidified body of rock formed from the lateral, surficial outpouring of molten lava from a vent or fissure, often lobate in form.  Compare - a'a lavaflow, pahoehoe lava flow. GG


geomfdesc:
A bluff composed of a thick deposit of coarse loess, formed immediately adjacent to the edges of flood plains, as along the Mississippi River valley or China.  Sometimes referred to as a bluff formation (not preferred).  Modified substantially from GG.


geomfdesc:
A hill composed of thick deposits of loess, as in IA, MO, NE and the Palouse hills of WA.  SW


geomfdesc:
The relatively steeper face of a cuesta, facing in a direction opposite to the dip of the strata.  Compare - dip slope.  GG


geomfdesc:
A closed depression or doline into which all or part of a stream disappears underground.  GG


geomfdesc:
[structural geology] A curve or bend of a planar structure such as rock strata, bedding planes, foliation, or cleavage.  GG


geomfdesc:
A tabular, igneous intrusion that parallels the bedding or foliation of the surrounding sedimentary or metamorphic rock.  Compare - dike.  GG


geomfdesc:
(a) Any terrestrial formation resembling a bay of the sea, as a recess or extension of lowland along a river valley or within a curve in a range of hills, or an arm of a prairie extending into, or partly surrounded by, a forest.  (b) A Carolina Bay.  GG & GSST.


geomfdesc:
A term applied to many local water features in the lower Mississippi River basin and in the Gulf Coast region of the U.S..  Its general meaning is a creek or secondary watercourse that is tributary to another body of water; especially a sluggish and stagnant stream that follows a winding course through alluvial lowlands, coastal swamps or river deltas. Compare - oxbow, slough.  GG


geomfdesc:
(a) A seaward end or the widened funnel-shaped tidal mouth of a river valley where fresh water comes into contact with seawater and where tidal effects are evident; e.g., a tidal river, or a partially enclosed coastal body of water where the tide meets the current of a stream.    (b) A portion of an ocean or an arm of the sea affected by fresh water; e.g., the Baltic Sea.     (c) A drowned river mouth formed by the subsidence of land near the coast or by the drowning of the lower portion of a nonglacial valley due to the rise of sea level.  GG


geomfdesc:
(a) A lake that derives much or all of its water from the melting of glacier ice, fed by meltwater, and lying outside the glacier margins (e.g. proglacial lake) or lying on a glacier (e.g. ice-walled lake, ice-floored lake) and due to differential melting.  (b) A lake occupying a basin produced by glacial deposition, such as one held in by a morainal dam.  (c) A lake occupying a basin produced in bedrock by glacial erosion (scouring, quarrying); e.g., cirque lake, fjord.  (d) A lake occupying a basin produced by collapse of outwash material surrounding masses of stagnant ice.   GG


geomfdesc:
A tidal stream connecting two larger waterways.  GG


geomfdesc:
[coast] A shallow stretch of salt or brackish water, partly or completely separated from a sea or lake by an offshore reef, barrier island, sand or spit.  GG.  [relict landform] A nearly level, filled trough or depression behind the longshore bar on a barrier beach and built by a receding pluvial or glacial lake.


geomfdesc:
An inland body of permanently standing water fresh or saline, occupying a depression on the Earth's surface, generally of appreciable size (larger than a pond) and too deep to permit vegetation (excluding subaqueous vegetation) to take not completely across the expanse of water.  GG


geomfdesc:
A shallow, intermittent lake in a arid or semi-arid region, covering or occupying a playa in the wet season but drying up in summer; an ephemeral lake that upon evaporation leaves or forms a playa.  GG


geomfdesc:
A shallow depression, generally less than 10 hectares in area, occurring on disintegration moraines and commonly containing an intermittent or seasonal pond or marsh.  GG


geomfdesc:
A type of glacial lake which formed just beyond the margin of an advancing or retreating glacier; generally in direct contact with the ice.  Compare - glacial lake, pluvial lake.  GG


geomfdesc:
A large or small body of salt water in a marsh or swamp along the seacoast.  GG


geomfdesc:
a) A relatively shallow place in a stream, lake, sea, or other body of water; a shallows.  (b) A submerged ridge, bank, or bar consisting of, or covered by, sand or other unconsolidated material, rising from the bed of a body of water to near the surface so as to constitute a danger to navigation.  It may be exposed at low water.  Compare - reef.  GG


geomfdesc:
A quiet part of, or a still body of water in a stream.  Compare - backswamp.  GG


geomfdesc:
Lake or pond produced in a permafrost region by melting of ground ice.  HP


geomfdesc:
The process, associated sediments (debris avalanche deposit) or resultant landform characterized by a very rapid to extremely rapid type of flow dominated by the sudden downslope movement of incoherent, unsorted mixtures of soil and weathered bedrock which, although comparatively dry, behave much as a viscous fluid.  Compare - debris flow, rock fragment flow, debris avalanche, earthflow, landslide.  SW


geomfdesc:
The flat to gently undulating ground underlain or composed of fine-grained sediments deposited in a former lake.  (b) The bottom of a lake; a lake basin.  GG


geomfdesc:
(refer to lake plain) (a) A imprecise term for a slight increase in slope and elevation of the land surface, usually with a broad summit and gently sloping sides.  GG (b) [soil survey] same as (a) but the term is restricted to microfeatures in areas of very low relief such as lake plains or coastal plains.  SW


geomfdesc:
Collapsed basins that are generally closed depressions which are the direct result of surficial subsidence associated with subsurface mining (e.g. long-wall mining).  SW


geomfdesc:
An artificial embankment constructed along the bank of a watercourse or an arm of the sea, to protect land from inundation or to confine streamflow to it's channel.  GG


geomfdesc:
A small human-made hill, composed either of debris accumulated during successive occupations of the site or of earth heaped up to mark a burial site. GG


geomfdesc:
An earthen embankment constructed across a slope for conducting water from above at a regulated flow to prevent accelerated erosion and to conserve water.  Compare - hillslope terrace.  SW & GSST


geomfdesc:
An open and usually unpaved (unlined), channel or trench excavated to convey water for drainage (removal) from a landscape; smaller than a canal; some ditches are modified natural waterways.  GG


geomfdesc:
A mound or stratum of refuse (broken pots, ashes, food remains, etc.) normally found on the site of an ancient settlement.  GG


geomfdesc:
a) A natural body of standing fresh water occupying a small surface depression, usually smaller than a lake and larger than a pool.  b) A small artificial body of water, used as a source of water.  Compare  - salt pond.  GG


geomfdesc:
The trace or track of a railroad route, commonly raised slightly above the adjacent land, and composed mostly of earthy material (gravel, rock fragments, etc.).  Abandoned or reclaimed beds may no longer be topographically or visually distinct, but the materials used to construct them may still be a significant portion of the soil zone.  SW


geomfdesc:
An anthropogenic, nearly level impoundment that is inundated for long periods typically for wetland rice production.  It is applied to areas that have been used in this fashion for a long enough period of time to significantly change the original soil morphology (especially redoximorphic features).  SW


geomfdesc:
The trace or track of a wheeled vehicle route that may or may not be raised slightly above the adjacent land, and may be composed mostly of earthy fill material (gravel, rock fragments, etc.) or local soil material.  Traffic can alter various soil properties primarily by compaction. Abandoned or reclaimed beds may no longer be topographically or visually distinct. However, materials used to construct beds or associated changes in soil properties may continue to have a significant impact upon soil management or plant growth.  SW


geomfdesc:
A linear or arcuate opening left in the soil after a plow or disk has opened a shallow channel at the soil surface.  A shallow channel cut in the soil surface, usually between planted rows for controlling surface water and soil loss, or for conveying irrigation water. GSST


geomfdesc:
A raised, generally horizontal strip of earth and/or rock bounded by a down-slope berm or retaining wall, constructed along a contour on a hillslope to make land suitable for tillage and to prevent accelerated erosion; common in steep terrain, both archaic (e.g. Peru) and modern (e.g. Nepal).  Compare - conservation terrace.  SW & GSST


geomfdesc:
A landscape which is intricately dissected and characterized by a very fine drainage network with high drainage densities and short, steep slopes with narrow interfluves.  Badlands develop on surfaces with little or no vegetative cover, overlying unconsolidated or poorly cemented materials (clays, silts, or in some cases sandstones) sometimes with soluble minerals such as gypsum or halite.  GG


geomfdesc:
(colloquial: southwestern U.S.A.) A broad, gently inclined alluvial piedmont slope extending from the base of a mountain range out into a basin and formed by the lateral coalescence of a series of alluvial fans.  Typically it has a broadly undulating transverse profile, parallel to the mountain front, resulting from the convexities of component fans.  The term is generally restricted to constructional slopes of intermontane basins.  Synonym - coalescent fan piedmont.  Compare - colluvial apron.  HP & SW


geomfdesc:
(a)  Drainage basin;  (b) A low area in the Earth's crust, of tectonic origin, in which sediments have accumulated.  GG  (c) (colloquial:  western USA)  A general term for the nearly level to gently sloping, bottom surface of an intermontane basin (bolson).  Landforms include playas, broad alluvial flats containing ephemeral drainageways, and relict alluvial and lacustrine surfaces that rarely, if ever, are subject to flooding.  Where through-drainage systems are well developed, flood plains are dominant and lake plains are absent or of limited extent.  Basin floors grade mountainward to distal parts of piedmont slopes.  FFP


geomfdesc:
(colloquial: western USA.)  A landscape term for an internally drained (closed) intermontane basin into which drainages from surrounding mountains converge inward toward a central depression.  Bolsons are often tectonically depressed areas and, according to Peterson, include alluvial flat, alluvial plain, beach plain, barrier beach, lake plain, sand sheets, dunes, and playa.  The piedmont slope includes slopes of erosional origin adjoining the mountain front (pediments) and complex construction surfaces (fans).  A semi-bolson is an externally drained (open) bolson.  Synonym - intermontane basin.  GG and FFP.


geomfdesc:
(colloquial:  western USA) A landscape or large tract of steep, rough or broken land dissected by ravines and gullies and marks a sudden change in topography as from an elevated plain to lower hilly terrain, or a line of irregular cliffs at the edge of  a mesa or a river (e.g., the Missouri River breaks).  SW & GG


geomfdesc:
A steeply sloping upland composed of hills with relief of  30 up to 300 meters and fringes a mountain range or high-plateau escarpment.    Compare - hill, mountain, plateau.  HP


geomfdesc:
(not preferred - use karst).  A landscape dominated by dissolution features (e.g., sinkhole, blind valley, closed depressions, underground drainage) formed in soluable rocks.  SW & GG


geomfdesc:
The zone within which migration of a meandering channel occurs; the flood-plain area included between two imaginary lines drawn tangential to the outer bends of active channel loops.  Landform components of the meander-belt surface are produced by a combination of gradual (lateral and down-valley) migration of meander loops and avulsive channel shifts causing abrupt cut-offs of loop segments.  Landforms flanking the sinuous stream channel include:  point bars, abandoned meanders, meander scrolls, oxbow lakes, natural levees, and flood-plain splays.  Meander belts may not exhibit prominent natural levee or splay forms.  Flood plains of broad valleys may contain one or more abandoned meander belts in addition to the zone flanking the active stream channel.  HP


geomfdesc:
A region or landscape characterized by mountains and their intervening valleys; a generic name for any group, cluster, or sequence of mountains or narrowly spaced mountain ridges, with or without peaks, closely related in position, orientation, direction, formation, or age, and whose summits commonly exceed 300 m  (approx. 1000 ft).  Compare - foothills, hills, mountain range, mountain system.    SW.


geomfdesc:
An area, plain, slope, glacier, or other feature at the base of a mountain; e.g., a foothill or a bajada.  In the United States, the Piedmont (noun) is a low plateau extending from New Jersey to Alabama and lying east of the Appalachian Mountains.  GG


geomfdesc:
An elongated depression of the Earth's surface; carved by a river during the course of it's development. GG


geomfdesc:
A region of semi-stabilized sand dunes or sandy hills, either covered with vegetation or bare, as in north-central Nebraska and the midlands of the Carolinas.  GG


geomfdesc:
An elevated, flat-lying, basalt-floored area, with little if any soil cover, sparse vegetation, and usually deep, dry channels scoured into the surface, especially by glacial meltwaters such as the channeled scablands of eastern Washington.  Compare - coulee.  GG


geomfdesc:
(colloquial: western USA) A wide desert basin or valley that is drained by an intermittent stream, an externally drained (open) intermontane basin.  Compare - bolson  GG


geomfdesc:
A general term for a broad upland mass with nearly level or undulating summit area of large extent and steep side slopes descending to surrounding lowlands.  Compare - plateau, mesa, cuesta.  HP


geomfdesc:
Karst-like topographic features produced in a permafrost region by local melting of ground ice and subsequent settling of the ground.  GG


geomfdesc:
An informal, general term for (a) the higher ground of a region, in contrast with a low-lying, adjacent land such as a valley or plain.  (b) Land at a higher elevation than the flood plain or low stream terrace; land above the footslope zone of the hillslope continuum.  Compare - lowland.  HP & GG


geomfdesc:
An elongated, relatively large, externally drained depression of the Earth's surface that is primarily developed by stream erosion or glacial activity.  Compare - basin.  HP


geomfdesc:
A local-scale topographic pattern of recurring, small, sinuous or arcuate ridges separated by shallow troughs irregularly spaced across low-relief flood plains(slopes generally 2 - 6 %); the effect is one of a subdued, sinuously undulating surface that is common on active, meandering flood plains.  Micro-elevational differences between bars and channels generally range from <0.5 to 2 m and are largely controlled by the competency of the stream.  The ridge-like bars often consist of somewhat coarser sediments compared to the finer textured sediments of the micro-low troughs.  Compare - meander scroll, meander belt.  SW


geomfdesc:
A form of patterned ground whose horizontal mesh is dominantly circular.  Compare - Nonsorted circle, patterned ground.  GG


geomfdesc:
A type of hummock consisting predominantly of a core of silty and clayey mineral soil and showing evidence of cryoturbation.  Earth hummocks are a type of nonsorted circle.  Compare - turf hummock, hummock [patterned ground], non-sorted circle, patterned ground.  NRC


geomfdesc:
A tall, conical column of unconsolidated to semi-consolidated earth materials (e.g. clay till, or landslide debris) produced by differential erosion and usually capped by a flat, hard rock fragment that shields the underlying, softer material from erosion.  It can measure up to 6-9 m in height, and its diameter is a function of the width of the protective boulder.  Compare - hoodoo.  GG


geomfdesc:
A small mound of fresh soil material formed by frost action.  A type of nonsorted circle commonly found in fine-grained sediment underlain by permafrost, or formed in areas affected by seasonal frost.  Compare - patterned ground.  NRC


geomfdesc:
A microfeature pattern of soils composed of a succession of microbasins and microknolls on level areas, or of microtroughs and microridges parallel to the slope on sloping areas, and produced by expansion / contraction and shear / thrust processes with changes in moisture.  Found in soils containing large amounts of smectitic clay that swell and shrink considerably with wetting and drying. Various types of gilgai can be recognized based on the dominant shape of micro-highs and micro-lows: circular gilgai, elliptical gilgai, and linear gilgai.  Also referred to, in part or in total, as crabhole, Bay of Biscay, or hushabye in older literature.  SW & GSST


geomfdesc:
A small channel with steep sides caused by erosion and cut in unconsolidated materials by concentrated but intermittent flow of water usually during and immediately following heavy rains or after ice / snow melt.  A gully generally is an obstacle to wheeled vehicles and too deep (e.g., >  0.5 m) to be obliterated by ordinary tillage; (a rill is of lesser depth and can be smoothed over by ordinary tillage).  Compare - rill, ravine, arroyo, swale, and draw.  HP & GSST


geomfdesc:
A polygon whose center is raised relative to its boundary.  Compare - low center polygon.  NRC


geomfdesc:
A small, irregular knob of earth (earth hummock) or turf (turf hummock).  Neither type of hummock is diagnostic of permafrost, but both are most common in subpolar or alpine regions.  Both require vegetative cover.  GG


geomfdesc:
Patterned ground in areas of ice wedges.  These polygons are commonly in poorly-drained areas and may be high-centered or low-centered.  NRC


geomfdesc:
A polygon whose center is depressed relative to its boundary.  Compare - high-center polygon.  NRC


geomfdesc:
(a) A low, rounded natural hill, of unspecified origin, generally less than 3 m high, composed of earthy material; Compare - hillock.  (b) A small, human-made hill, composed either of debris accumulated during successive occupations of the site (e.g. tell) or of earth heaped up to mark a burial site (e.g. burial mound).  (c) A structure built by colonial organisms (e.g. termite mound).  GG


geomfdesc:
A type of patterned ground whose mesh (shape) is dominantly circular and has a nonsorted appearance due to the absence of a boarder of coarse fragments.  Vegetation characteristically outlines the pattern by forming a boardering ridge.  Diameters commonly range from 0.5 to 3 m.  Nonsorted circles include mud boils, earth hummocks, turf hummocks, and frost boils.  Nonsorted circles have various origins.  Some, such as mud and earth hummocks and frost boils, involve cryoturbation activity and differential heave of frost-susceptible materials.  Others, such as mud boils, involve hydraulic pressures and diapir-like displacement of water-saturated sediments.  Compare - sorted circle, frost boil, patterned ground.  NRC and GG


geomfdesc:
An elliptical dome-like permafrost mound containing alternating layers of ice lenses and peat or mineral soil, commonly 3-10 m high and 2-25 m long, occurring in subarctic bogs of the tundra and often surrounded by water; pl. palsen.  NRC


geomfdesc:
(colloquial: Gulf Coast U.S.A.)  Low, flattened, approximately circular or elliptical features composed of sandy loam that is coarser than, and distinct from, the surrounding soil; the basal diameter ranges from 3 m to more than 30 m, and the height from 30 cm to more than 2 m.  Compare -  mima mound, patterned ground, shrub-coppice dune.  GG


geomfdesc:
A tall, slender, tapering tower or spire-shaped pillar of rock, either isolated, as on steep slopes or cliffs formed in karst or other massive rocks,  or at the summit of a hill or mountain.    Compare - erosional remnant, hoodoo.  GG


geomfdesc:
A type of patterned ground consisting of a closed, roughly equidimensional figure bounded by more or less straight sides; some sides may be irregular.  Refer to patterned ground.  Compare - High center polygon, low center polygon, ice wedge polygon, nonsorted polygon.  NRC


geomfdesc:
A small, natural body of standing water, usually fresh; e.g. a stagnant body of water in a marsh, or a transient puddle in a depression following a rain.  GG


geomfdesc:
[geomorghology] (not preferred) A generic, imprecise term for any pot-shaped pit or hole.

[glacial geology] A term applied to a small pit depression (1 to 15 meters deep), generally circular or elliptical, occurring in an outwash plain, a recessional moraine, or a till plain.

[lake] - A shallow depression, generally less than 10 hectares in area, occurring on disintegration moraines and commonly containing an intermittent or seasonal pond or marsh.  GG


geomfdesc:
An undulating surface of alternating, subparallel, small-scale ridges and depressions, commonly composed of loose sand.  It is produced on land by wind and under water by the agitation of water by currents or wave action, and generally tends at right angles or obliquely to the direction of flow of the moving fluid.  Compare - giant ripple mark.  GG


geomfdesc:
An accumulation of sand commonly in the form of a low mound, produced by the expulsion of liquified sand to the ground surface; sometimes called sand volcanoes (not preferred).  Examples are found on top of some landslide deposits (i.e. spreads) or on the upper surface of highly contorted layers of laminated sediments.  SW & GG


geomfdesc:
A place in a stream bed swept (scoured) by running water, generally leaving a gravel bottom.  GG


geomfdesc:
A broad deposit of nonsorted, water-saturated, locally derived material that is moving or has moved downslope, en masse.  Stripes are commonly associated with solifluction sheets.  Compare - stripe. NRC


geomfdesc:
A low step with a straight or lobate front, the latter reflecting local differences in rate of flow.  A solifluction terrace may have bare mineral soil on the upslope part and 'folded under' organic matter in both the seasonally thawed and the frozen soil.  NRC


geomfdesc:
A type of patterned ground whose mesh (shape) is largely circular and has a sorted appearance commonly due to a border of coarse fragments surrounding finer material, occurring either singly or in groups.  Diameters range from a few centimeters to more than 10 meters.  The coarse fragment border may be 35 cm high and 8 to 12 cm wide.  Compare - patterned ground.  GG and NRC


geomfdesc:
A type of patterned ground; one of the alternating bands of fine and coarse surface material, or of rock or soil and vegetation-covered ground, commonly found on steeper slopes.  It is usually straight, but may be sinuous or branching.  Compare - patterned ground.  GG


geomfdesc:
(colloquial: southwestern USA) A natural depression or cavity in impervious rocks in which water collects and remains for the greater part of the year.  GG


geomfdesc:
Small, irregular step-like forms on steep hillslopes, especially in pasture, formed by creep or erosion of surficial materials that may or may not be induced by trampling of livestock such as sheep or cattle.  Synonyms (not preferred) - catstep, sheep or cattle track.  HP


geomfdesc:
The small mound of debris sloughed from the root plate (ball) of a tipped-over tree.  Sometimes called a cradle knoll (not recommended).  Local soil horizons are commonly obliterated and result in heterogeneous strata.  Compare - tree-tip pit.  SW.  (Modified substantially from BHM).


geomfdesc:
The small pit or depression resulting from an area vacated by the root plate (ball) resulting from tree-tip ("tree-throw").  Such pits are commomly adjacent to small mounds composed of the displaced material.  Subsequent infilling commonly results in a heterogeneous soil matrix, that may or may not include a stone line that lines the depression.  Compare - tree-tip mound.  SW.  (Modified substantially from BHM).


geomfdesc:
A hummock consisting of vegetation and organic matter with or without a core of mineral soil or stones.  Compare - earth hummock, non-sorted circle, patterned ground.  NRC


geomfdesc:
An excavated area where borrow material has been removed typically for construction purposes offsite; also called barrow pit.  GG


geomfdesc:
A passage, incision, or space from which material has been excavated, such as a road cut or railroad cut.  GG


geomfdesc:
Excavation areas, open to the sky, usually for the extraction of stone.  GG


geomfdesc:
A depression, ditch or pit excavated to furnish sand for roads or other construction projects off-site; a type of borrow pit.  SW


geomfdesc:
Any artificial pond or other water-filled excavation for the natural oxidation of sewage or disposal of farm manure.  GG


geomfdesc:
Rock debris, banks, and earthy dump deposits resulting from the excavation of ditches and strip mines.  GSST


geomfdesc:
A depression, open to the sky, resulting from the surface extraction of earthy material (e.g. soil / fill) or bedrock material (e.g. coal).  Compare - borrow pit, openpit mine, quarry.  SW


geomfdesc:
A depression, ditch or pit excavated to furnish gravel for roads or other construction projects; a type of borrow pit.  SW


geomfdesc:
A land area where municipal solid waste is buried in a manner engineered to minimize environmental degradation.  Commonly the waste is compacted and ultimately covered with soil or other earthy material.  Compare - dump.  GG


geomfdesc:
A land area, usually a field, that has been mechanically flattened or smoothed to facilitate management practices such as flood irrigation; as a result the natural soil has been partially or completely modified (e.g., truncated or buried).  SW


geomfdesc:
A type of basaltic lava flow dominated by a'a lava and a characteristically rough, jagged, clinkery surface.  Compare - block lava flow, pahoehoe lava flow, pillow lava flow.  GG & MA


geomfdesc:
A volcano having the shape of a very broad, gently sloping dome, built by flows of very fluid basaltic lava or rhyolitic ash flows.  Compare - stratovolcano.   GG & MA


geomfdesc:
A low "island" of land surrounded by a younger (more recent) lava flow.  Compare - steptoe.  MA


geomfdesc:
A natural, hollow tunnel beneath the surface of a solidified lava flow through which the lava flow was fed; the tunnel was left empty when the molten lava drained out.  MA & GG


geomfdesc:
(a) Any body of running water that moves under gravity to progressively lower levels, in a relatively narrow but clearly defined channel on the ground surface, in a subterranean cavern, or beneath or in a glacier.  It is a mixture of water and dissolved, suspended, or entrained matter.  (b) A term used in quantitative geomorphology interchangeably with channel.  Compare - river.  GG


geomfdesc:
(colloquial: Hawaii) A natural surface channel commonly found near the middle of an a'a lava flow, formed by the surficial draining of molten lava rather than by erosion from running water; a type of lava trench.  Compare - lava tube.  MA


geomfdesc:
An erosional remnant of a terrace which retains the surface form and alluvial deposits of its origin but was not emplaced by, and commonly does not grade to a present-day stream or drainage network.  Compare - alluvial plain remnant.  SW


geomfdesc:
A watercourse that is generally dry but conducts flood waters that have overflowed the banks of a river, commonly from large storms, annual meltwater, or glacial meltwaters.  SW


geomfdesc:
A deeply and extensively dissected landscape composed predominantly of relatively narrow, steep-walled valleys with small flood plains or valley floors; commonly with considerable outcrops of hard bedrock on steep slopes, ledges, or cliffs, and with broader summits or interfluves than found in badlands.  Sideslopes exhibit extensive erosion, active back-wearing, and relatively sparse vegetation.  SW


geomfdesc:
An assemblage of moving and/or stabilized sand dunes, together with sand plains, interdune areas, and the pond, lakes, or swamps produced by the blocking of streams by the sand.  See dune lake.  SW.


geomfdesc:
Groups or clusters of closely spaced drumlins or drumlinoid ridges, distributed more or less en echelon, and commonly separated by small, marshy tracts or depressions (interdrumlins).  SW


geomfdesc:
A sand-covered plain which may originate by deflation of sand dunes, and who's lower limit of erosion is governed by the ground-water level.  Also spelled sandplain.  GG.


geomfdesc:
Generally a small stream, or upper reach of a stream, that flows only in direct response to precipitation.  It receives no protracted water supply from melting snow or other source, and its channel is, at all times, above the water table.  Compare - arroyo, intermittent stream, perennial stream.  HP


geomfdesc:
A stream or reach of a stream that flows continuously throughout the year and whose surface is generally lower than the water table adjacent to the region adjoining the stream.  Compare - Ephemeral stream, Intermittent stream.  GG


geomfdesc:
The process, associated sediments (rockfall avalanche deposit) or resultant landform characterized by an extremely rapid, large type of rock-fragment flow (a type of landslide) which starts as a rockfall but turns into a flow and characteristically deposits rock-dominated debris long distances from the failure face (such as 10-20 times the fall height); occurs only when huge rockfalls and rockslides involving millions of metric tons of material attain extremely rapid speeds; most common in a rugged mountainous area; ex: the 1903 Franks, Alberta, Canada avalanche.  Sometimes loosely referred to as a long run-out landslide.  Compare - rock fragment flow, flow, landslide.  SW


geomfdesc:
The process, associated sediments (rockfall deposit) or resultant landform characterized by a very rapid type of fall dominated by downslope movement of detached rock bodies which fall freely through the air or by leaps and bounds (lacks an underlying slip face); also spelled rock fall. Compare - debris fall, soil fall,  landslide.  SW


geomfdesc:
A portion of a hillslope or mountainslope mantled by talus and lying below a rockfall source (cliff).  Compare - scree slope, scree, talus.  SW


geomfdesc:
A category of processes, associated sediments (topple deposit) or resultant landforms characterized by a localized, very rapid type of fall in which large blocks of soil or rock literally fall over, rotating outward over a low pivot point.  Portions of the original material may remain intact, although reoriented, within the resulting debris pile. Types of topples can be specified based on the dominant particle size of sediments (i.e. debris topple, soil topple, rock topple.  Compare - fall, flow, slide, spread, complex landslide, landslide.  SW & DV


geomfdesc:
A landform produced in a region of limestone or sandstone by infrequent rains combined with wind action, and characterized by "a surface bristling with a fine lacework of sharp ridges pitted by corrosion".  GG


geomfdesc:
A long, shallow, round-bottomed groove, furrow, trough, or corridor excavated in the desert floor by wind abrasion, and separating two yardangs.  GG


geomfdesc:
A microfeature in the form of a long, irregular, sharp-crested, undercut ridge between two round-bottomed troughs, carved on a plateau or unsheltered plain in a desert region by wind erosion, and cut into soft but coherent deposits (such as clayey sand); it lies in the direction of the dominant wind, and may be up to 6 m high and 40 m wide.


geomfdesc:
a) A large assemblage of fluvial landforms (braided streams, terraces, etc.,) that form low gradient, regional ramps along the flanks of mountains and extend great distances from their sources (e.g., High Plains of North America.  SW   b) (not recommended, use flood plain.)  An general, informal term for a broad flood plain or a low-gradient delta.  Compare - alluvial flat.  FFP.


geomfdesc:
An erosional remnant of an alluvial plain which retains the surface form and alluvial deposits of its origin but was not emplaced by, and commonly does not grade to a present-day stream or drainage network.  Compare - alluvial plain, erosional remnant, paleoterrace.  SW


geomfdesc:
The process, associated sediments (block glide deposit) or resultant landform characterized by a slow type of slide, in which largely intact units (blocks) of rock or soil slide downslope along a relatively planar surface, such as a bedding plane, without any significant distortion of the original mass.  Compare - rotational landslide, debris slide, lateral spread, landslide.  SW & DV


geomfdesc:
A category of mass movement processes, associated sediments (complex landslide deposit) or resultant landforms characterized by a composite of several mass movement processes none of which dominates or leaves a prevailing landform.  Numerous types of complex landslides can be specified by naming the constituent processes evident (e.g. a complex earth spread - earth flow landslide).  Compare - fall, topple, slide, lateral spread, flow, landslide.  SW &  DV


geomfdesc:
A low relief, low angle, asymmetrical depression which lies parallel to the strike of underlying strata; a type of strike valley.  It's formed by the differential erosion of weaker strata interbedded with more resistant bedrock.  It may or may not contain a local drainage network and commonly lies above and is not connected to the regional drainage system.  Compare - cuesta, valley, trough, hanging valley.  SW


geomfdesc:
The process, associated sediments (debris slide deposit) or resultant landform characterized by a rapid type of slide, composed of comparatively dry and largely unconsolidated earthy material which slides or rolls downslope (does not exhibit backward rotation) and resulting in an irregular, hummocky deposit somewhat resembling a moraine.  Compare - rotational landlside, block glide, lateral spread, landslide.  SW  & GG


geomfdesc:
A category of mass movement processes, associated sediments (lateral spread deposit) or resultant landforms characterized by a very rapid spread dominated by lateral movement in a soil or fractured rock mass resulting from liquefaction or plastic flow of underlying materials; also called spread.  Types of lateral spreads can be specified based on the dominant particle size of sediments (i.e. debris spread, earth spread, rock spread.  Compare - fall, topple, slide, flow, complex landslide,landslide.  SW, DV & GG


geomfdesc:
Remnant features of a glacial lake that is now extinct which formed just beyond the margin of an advancing or retreating glacier; generally in direct contact with the ice.  Compare - proglacial lake, pluvial lake.  SW


geomfdesc:
(a) An area of land completely surrounded by water;  (b) An elevated area of land surrounded by swamp, or marsh, or isolated at high water or during floods.  Compare - barrier island.  GG


geomfdesc:
Generally a narrow, transverse area that parallels a coastline, commonly crossing cutting across diverse inland landforms, and dominated by landforms derived from active coastal processes which gives rise to beach ridges, overwash fans, beaches, dunes, wave-cut platforms, barrier islands, cliffs, stacks, etc.  SW


geomfdesc:
A type of basaltic lava flow with a characteristically smooth, billowy or rope-like surface.  Compare - a'a lava flow, block lava flow, pillow lava flow.  GG & MA


geomfdesc:
A relict glaciofluvial terrace that retains its original attitude, composed of undistorted outwash sediments and depositional structures and whose surface is pock-marked with numerous potholes or kettle depressions.  Compare - collapsed outwash plain.  SW


geomfdesc:
(a) A general term for a natural, freshwater surface stream of considerable volume and generally with a permanent baseflow, moving in a defined channel toward a lake, sea, or a larger river;  (b) (colloquial - New England, USA; not recommended)  A small watercourse which elsewhere in the USA is known as a creek.  Compare - stream.  GG


geomfdesc:
A portion of a hillslope or mountainslope mantled by scree and lacking an up-slope rockfall source (i.e. cliff).  Compare - talus slope, scree, talus.  SW


geomfdesc:
The narrow strip of land immediately bordering any body of water, esp. the sea or a large lake; specifically the zone over which the ground is alternately exposed and covered by tides or waves, or the zone between high water and low water.  GG


geomfdesc:
The process, associated sediments (soil fall deposit) or resultant landform characterized by a rapid type of fall involving the relatively free, downslope movement or collapse of detached, unconsolidated soil material which falls freely through the air (lacks an underlying slip face); sediments predominantly fine earth (< 2 mm); common along undercut stream banks.  Also called earth fall, and (not recommended) debris fall.  Compare - rock fall, debris fall, topple, landslide.  SW


geomfdesc:
Small, trough-like, arcuate or sinuous channels separated by small bars or ridges, caused by fluvial processes and common to floodplains and young alluvial terraces; a constituent part of bar & channel topography. GG, FFP, & SW


geomfdesc:
A small, sinuous or arcuate ridge-like lineation on a flood plain and separated from others like it by small channels or troughs; caused by fluvial processes and common to flood plains and young alluvial terraces, and is a constituent part of bar & channel topography.  Compare - meander scroll.  SW


geomfdesc:
A bizzarrely shaped column, pinnacle, or pillar of rock produced by differential weathering or erosion in a region of sporadically heavy rainfall.  Formation is facilitated by joints and layers of varying hardness.  Compare - earth pillar.  GG


geomfdesc:
A generic name for a small, low hill, generally between 3 - 30 m in height and slopes between 5 and 50% (e.g., bigger than a mound but smaller than a hill); commonly considered a microfeature.  Compare - mound, hill.  SW


geomfdesc:
A small, natural, narrow drainageway on high angle slopes which separate small, tertiary spur ridges or mini-interfluves and is a constituent part of rib & groove topography; common in well dissected uplands.  Compare - rib.  SW


geomfdesc:
A very small channel with steep sides caused by erosion and cut in unconsolidated materials by concentrated but intermittent flow of water, usually during and immediately following moderate rains or after ice / snow melt.  Generally, a rill is not an obstacle to wheeled vehicles and is shallow enough (e.g., < 0.5 m) to be obliterated by ordinary tillage.  Compare - gully.  SW & GSST


geomfdesc:
A small, high-angle, tertiary spur ridge or mini-interfluve that is a constituent part of rib & groove topography; (slopes generally 20 - 90 %, or more); common on the mid and lower hillslopes of well dissected uplands.  Compare - finger ridge, groove, rib and groove topography.  SW


geomfdesc:
An open and usually unpaved (unlined), channel or trench excavated to convey water for drainage (removal) or irrigation (addition) to or from a landscape; smaller than a canal; some ditches are modified natural waterways.  GG


geomfdesc:
An area of smooth or uneven accumulations or piles of waste rock, earthy material, or general refuse that without major reclamation are incapable of supporting plants.  Compare - sanitary landfill, fill.  GSST


geomfdesc:
(a)  Human-constructed deposits of natural earth materials (e.g. rock, soil, gravel) and waste materials (e.g. tailings or spoil from dredging) used to fill a depression, to extend shore land into a a body of water, or in building dams.  (b)  Soil or loose rock used to raise the surface level of low-lying land, such as an embankment to fill a hollow or ravine in road and railroad construction


geomfdesc:
- (a) A bank, mound, or other artificial accumulation composed of spoil;  e.g., An embankment of earthy material dredged from a channel and deposited alongside it.  (b) A pile of refuse material from an excavation or mining operation; e.g. a pile of dirt removed from, and stacked at the surface of a mine in a conical heap or in layers.  GG


geomfdesc:
Raised, linear mounds with subdued, convex slope cross-sections constructed by mounding and shaping spoil material dredged from adjacent drainage ditches and placed over natural soil.  The mounds serve as preferred, better-drained bedding areas for managed timber plantations; common in the lower coastal plains of the Atlantic and Gulf coasts, USA.  SW


geomfdesc:
Irregularly spaced, roughly linear to radial depressions or small mounds associated with shallow to deep soil disturbance caused by dragging logs across a slope from where they were cut down to a central processing area such as a log landing during timber harvest operations.  SW


geomfdesc:
A comparatively level area, usually with road access, constructed or cut into steeper slopes and used for sorting logs during timber harvest operations.  Compare - skid trail.  SW


geomfdesc:
(colloquial - Southern High Plains)  The convex, upper margin (shoulder) of a playa basin where the playa slope intersects the surrounding terrain.  Compare - playa slope.  SW


geomfdesc:
A small, permanent body of water in a semi-closed or closed depression formed by movement along a strike-slip fault or by mass movement (i.e., landslide) that ponds water from impounded drainage or surface runoff.  Also spelled sagpond.  SW & GG


geomfdesc:
(colloquial - Southern High Plains)  The relatively level or gently inclined "terrace-like" bench or toeslope within a large playa basin flanking and topographically higher than the playa floor and below the playa slope; a bench or step-like surface within a playa basin that breaks the continuity of the playa slope and modified by erosion and/or deposition.  Temporary ponding may occur in response to precipitation / runoff events.  Compare - playa slope.  SW


geomfdesc:
(colloquial - Southern High Plains)  The lowest extensive, flat to slightly concave surface within a playa basin, consisting of a dry lake bed or lake plain underlain by stratified clay, silt or sand, and commonly by soluble salts.  Compare - playa step.  SW


geomfdesc:
A small, partially or completely closed depression formed by movement along a strike-slip fault, or by mass movement (i.e., landslide) that may or may not temporarily pond water from impounded drainage or surface runoff.  For example, a closed depression formed between a scarp or headwall and an adjacent rotated slump block of a landslide.  SW


geomfdesc:
A natural, seasonal pond in a small closed depression (micro-low) which supports a semi-aquatic or aquatic ecosystem adapted to annual cycles of standing water in the springtime followed by drying in the summer / autumn; commonly recognized in CA.  SW


geomfdesc:
(colloquial - Southern High Plains)  The generally concave to slightly convex area within a playa basin that lies between the relatively level playa floor below (or playa step, if present) and the convex playa rim above.  Overland flow is typically parallel down slope.  Compare - playa step, playa rim.  SW


geomfdesc:
(colloquial - Southern High Plains)  A linear or curvilinear ridge of windblown, granular material (generally sand or parna) removed from the adjacent basin by wind erosion (deflation), and deposited on the leeward (prevailing downwind) margin of a playa, playa basin, or salina basin.  The dune may be barren or vegetated.  Compare - dune.  SW


geomfdesc:
One in a group of small, tertiary spur ridges that form crudely palmate extensions of erosional remnants along the flanks or nose of larger ridges.  Compare - ballena, rib.  SW


geomfdesc:
An extensive lowland area of coarse textured, glaciofluvial material.  An outwash plain is commonly smooth; where pitted, due to melt-out of incorporated ice masses (pitted outwash plain), it is generally low in relief and largely retains it's original gradient.  Compare - outwash, pitted outwash plain, collapsed outwash plain, kettles.  SW & HP


geomfdesc:
An assemblage of landforms constructed proximal to a relatively static, rapidly wasting continental glacial margin.  Constituent landforms can include fosse, head-of-outwash, ice-contact slope, ice-contact delta, kame, kame moraine, kettle, outwash fan, small outwash plain, glacial sluiceway, and small proglacial lake.  Moraines, if present, are of limited occurrence (except kame moraines which can be extensive).  Glaciofluvial sediments dominate but glaciolacustrine sediments, till, and diamictons can be present in minor amounts.  SW


geomfdesc:
A glacial lake occupying a portion of a tunnel valley.  GG


geomfdesc:
A subsequent valley eroded in, and developed parallel to the strike of, underlying weak strata; such as a cuesta; a valley that commonly, but not necessarily contains a strike valley.  SW & GG


geomfdesc:
An erosion surface of low relief, cut directly into and across bedrock and composed of either bare rock or thinly veneered pedisediment or residuum (e.g. < 1.5 m) over bedrock; it occurs along the flanks of mountain fronts, or at the base of mountains or high hills.  Its surface grades to the backwearing mountain slopes or hillslopes above, and generally grades down to and merges with a lower-lying alluvial plain, piedmont slope or valley floor below.  SW & FFP


geomfdesc:
(colloquial: Caribbean Basin)  An isolated, steep-sided, commonly asymmetrical hill or ridge composed of limestone, generally steeper on its leeward side (prevailing downwind side) and surrounded by nearly level to sloping coastal plain composed of marine and alluvial sediments; a type of karst tower.  They range in height from a few feet (< 1 m) to over 150 ft (50 m).  Most are isolated and cover small areas but some form clusters of hills or ridges rising out of the surrounding blanket deposits.  Mogotes are extensive in northern Puerto Rico.  SW, Monroe ( 1976, 1980), & WW.


geomfdesc:
A long, narrow sand dune, usually symmetrical in cross profile, oriented parallel to the prevailing wind direction ; it is wider and steeper on the windward side but tapers to a point on the lee side.  It commonly forms behind an obstacle in an area where sand is abundant and the wind is strong and constant.  Such dunes can be a few meters high and up to 100 km long.  Compare - seif dune, transverse dune.  GG


geomfdesc:
The concave to relatively flat bottomed, roughly linear depressions ranging from small saddles or swales to small valleys that separate drumlins or drumlinoid ridges in drumlin fields.  Streams, if present, have not had a dominant impact on the formation of the depression.  Compare - drumlin, drumlinoid ridge.  SW


geomfdesc:
A stream drainage along the side or front of a glacier.  Relict ice-marginal streams are used to trace the former position of a glacier; also called ice-marginal drainage.  SW & GG


geomfdesc:
A steep escarpment of predominantly glaciofluvial sediment that was deposited against a wall of glacier ice, marking the position of a relatively static ice-margin; an irregular scarp against which glacier ice once rested.  Compare - head-of-outwash.  SW & GG


geomfdesc:
A sloping and sometimes high relief landform composed predominantly of glaciofluvial sediment that delimits a former ice-margin of a relatively static, rapidly wasting glacier.  A steep ice-contact slope forms the ice-proximal face of the landform; a more gently sloping surface dips away on the distal slope, if not slumped.  Compare - ice-margin complex.  SW


geomfdesc:
The comparatively steep, glacially scoured, concave sides of a u-shaped, mountain valley mantled by colluvium with little or no till; (not preferred: colloquial - western USA) sometimes called a trough wall.  SW


geomfdesc:
The comparatively flat bottom of a mountain valley predominantly mantled by till but which can grade from glacial scour (scoured rock-outcrop) near it's head to a thick mantle of till, and ultimately merging with alluvium or colluvium further down valley.   Some glacial-valley floors descend downstream in a series of scour-derived steps which may contain sequential tarn lakes (pater noster lakes); (not preferred: colloquial - western USA) sometimes called a trough bottom.  SW


geomfdesc:
A rock drumlin or drift deposit whose form approaches but does not fully attain that of a classic drumlin, even though it seemingly results from similar processes of moving ice.  Compare - drumlin, interdrumlin.  SW & GG


geomfdesc:
(not preferred) refer to cirque headwall.


geomfdesc:
The comparatively level bottom of a cirque, thinly mantled with till and consisting of glacially-scoured knolls and hillocks separated by depressions, flat areas and small lakes (tarn); commonly it is bounded by a slightly elevated rock lip at its exit.  SW & HD


geomfdesc:
(a) The main stream of an intermontane valley, flowing in the deepest part of the valley and parallel to its longest dimension.  (b) A stream that follows the axis of a syncline or anticline.  GG


geomfdesc:
A relatively level or bench-like surface formed by the coalescence of several cirques.  GG & SW


geomfdesc:
a) A large-capacity channel constructed to divert floodwaters or excess streamflow from populous, flood-prone areas, such as a bypass route bounded by levees.  b) The part of the flood plain kept clear of encumbrances and reserved for emergency diversion of floodwaters.  GG


geomfdesc:
(colloquial: western U.S.A.) A wide, gently-sloping portion of a bolson floor comprising numerous, parallel, closely-spaced, relict longshore-bars and lagoons built by a receding pluvial lake.  Synonym, offshore barrier, offshore beach, bar beach.  Compare - bar [coast], barrier island.  GG and FFP


geomfdesc:
(a) A divergent stream flowing away from the main stream and not returning to it, as in a delta or on a flood plain.  It may be produced by stream deposition choking the original channel.  (b) One of the channels of a braided stream; a channel carrying the water of a stream distributary.  GG


geomfdesc:
(a) A lake occupying a deflation basin as in a blowout on a dune.  (b) A lake occupying a basin formed by the blocking of a stream by sand dunes migrating along a shore (e.g. Moses lake, WA).  GG


geomfdesc:
(not recommended - use meteorite crater)  A generally circular crater formed by the impact of an interplanetary body (projectile) on a planetary surface.  GG


geomfdesc:
An asymmetrical ridge of local, essentially non-glacial material (such as deformed bedrock, with some drift incorporated in it) that has been pressed up by the shearing action of an advancing glacier.  It is typically 10 - 60 m high, about 150 - 300 m wide, and as much as 5 km long.  Examples are common on the Great Plains where such ridges occur on the sides of escarpments formed of relatively incompetent rocks that face the direction from which the ice moved.  GG


geomfdesc:
The sloping part of the beach that is alternately covered and uncovered by the uprush of waves, and where longshore movement of water occurs in a zigzag (upslope-downslope) manner.  Compare - shoreline.  GG


geomfdesc:
a) A large mass of ice formed, at least in part, on land by the compaction and recrystallization of snow, moving slowly by creep downslope or outward in all directions due to the stress of its own weight, and surviving from year to year.  Included are small mountain glaciers as well as ice sheets continental in size, and ice shelves which float on the ocean but are fed in part by ice formed on land. b)  A stream-like landform having the appearance of, or moving like a glacier; e.g. a rock glacier.  Compare - snowfield, rock glacier.  GG


geomfdesc:
A generic term for the steeper part of a hill between its summit and the drainage line, valley flat, or depression floor at the base of the hill.  Compare - mountain slope. HP


geomfdesc:
An elongated depression of the Earth's surface; carved by a river during the course of it's development.  Compare - valley side, valley floor.  GG


geomfdesc:
A bank or slope portion of a cut excavated into unconsolidated material (regolith) or bedrock as in a roadcut, whose slope gradient has been mechanically reduced to a subdued angle (e.g. to < 33 %) to increase slope stability, reduce erosion, or to facilitate revegetation.  Compare - cut, cutbank, roadcut.  SW


geomfdesc:
A slope or wall portion of a cut excavated into unconsolidated material (regolith) or bedrock, as in a borrow pit.  It may stand nearly vertical resulting from collapse as the base is undercut during excavation or by erosion, or it may be reduced by subsequent erosion to a more subdued angle by slope wash.  Compare - cut, beveled cut, roadcut.  SW


geomfdesc:
A generally circular or elliptical depression formed by hypervelocity impact of an experimental projectile or ordinance into earthy or rock material.  Compare - caldera, crater, meteorite crater.  SW


geomfdesc:
a) A land area composed of earthy fill material that has been placed and shaped to approximate natural contours, commonly part of land-reclamation efforts after mining operations; b) A land area, commonly submerged in its native state, that has been protected by artificial structures (e.g. dikes) and drained for agricultural or other purposes (e.g. polder).  SW


geomfdesc:
a) A modified slope, feature, or land area where much or all of the natural soil has been mechanically removed (e.g. scraped off) due to construction or other management practices.  Compare - truncated soil.  b) A forest soil area where the ground vegetation and root mat have been removed to expose mineral soil in preparation for planting or seeding.  Compare - truncated soil.   SW


geomfdesc:
A generic name for any enclosed area that has no surface drainage outlet and from which water escapes only by evaporation or subsurface drainage; an area of lower ground indicated on a topographic map by a hachured contour line forming a closed loop.  Compare - open basin.  SW & GG


geomfdesc:
Small, tighly bunched, parallel ridges or corrugations of lava, commonly < 1 m in amplitude (high) and < 3 m in period (wide) on the surface of corded pahoehoe lava (ropy lava).  SW & GS


geomfdesc:
A dissolution groove or trench formed along vertical bedrock fractures beneath soil and usually buried beneath regolith with little or no ground surface expression, commonly wider than a solution fissure (widths commonly range from 0.5 to 3 meters) and tapering down to a crack or a bedrock floored trench; also called grike (not preferred), subsurface karren (not preferred).  Compare - karren, solution fissure, solution corridor.  SW & WW


geomfdesc:
A damp depression or trough between dunes in a dune field or dune ridges on a shore, caused by intersecting the capillary fringe of the local water table; a moist type of interdune.  Compare - interdune, dune lake.  SW & GG


geomfdesc:
A lineation or streamlined groove or ridge parallel to the direction of ice movement, formed in newly deposited till or older drift.  They range in height from a few centimeters to 25 m, and in length from a few meters to 20 km.  GG


geomfdesc:
The relatively flat surface, whether sand-free or sand-covered, between dunes.  GG


geomfdesc:
Repeating, surficial solution channels, grooves or other forms etched onto massive, bare limestone surfaces; types range in depth from a few millimeters to > 1 m and separated by ridges; the total complex (all varieties) of surficial solution forms found on compact, pure limestone.  Many types can be specified.  Compare - solution fissure.  SW & GG


geomfdesc:
A separate, distinct lobe of lava that issues from the main body of a lava flow; a specific outpouring of lava, a few centimeters to several meters thick and of variable lateral extent, that forms a subdivision within a single flow.  A series of overlapping lava flow-units together comprise a single lava flow.  Also called flow unit.  Compare - lava flow.  GS & GG


geomfdesc:
A natural surface channel in a lava flow that never had a roof, formed by the surficial draining of molten lava rather than by erosion from running water; also called lava channel.  Compare - mawae, lava tube.  SW


geomfdesc:
A shallow, non-cliffed depression or hollow on a mountain side permanently or intermittently occupied by a snow bank or snow patch and produced by nivation.  If the snow completely melts each summer the hollow is deepened; otherwise not; may be a cirque precursor if further enlarged and deepened by alpine glaciation.  GG


geomfdesc:
A generic name for any enclosed or low area that has a surface drainage outlet whereby surface water can leave the enclosure; an area of lower ground indicated on a topographic map by contour lines forming an incomplete loop or basin indicating at least one surface exit.  Compare - closed basin.  SW


geomfdesc:
The steeply sloping surface on the lee side of a dune, standing at or near the angle of repose of loose sand, and advancing downwind by a succession of slides wherever that angle is exceeded.  GG


geomfdesc:
A straight, open trench about 3 to 10 m wide in a karst area, formed by vertical and lateral solution zones developed along bedrock fractures; also called (not preferred) bogaz, zanjon (Puerto Rico).  Compare - solution fissure, karst valley.  SW & GG


geomfdesc:
One of a series of vertical open cracks commonly < 0.5 m wide dissolved along joints or fractures, separating limestone pavement (pavement karst) into blocks (clints); also called kluftkarren (not preferred).  Compare - solution corridor, karren.  SW, GG, & WW


geomfdesc:
A small, steep-sided cone (e.g., 3 - 15 m high, or more) built up on a lava flow, usually pahoehoe, composed of clots of lava ejected with escaping gases from a vent or fissure which spatters and congeals as it hits the ground to form a small cone; rougher lava clots than a spiracle.  Compare - spiracle.  SW


geomfdesc:
A small tubular opening or chimney formed by fluid lava congealing and mounding around a fumarolic vent in a basaltic lava flow, usually about 1 m in diameter and up to 5 m high, although in the northwestern USA where spiracles are common they generally are 10 m in diameter and 12 m high or more; formed by a gaseous explosion in lava that is still fluid, probably due to steam generated from underlying wet material; smoother lava clots and drapes than a spatter cone.   Compare - spatter cone.  SW, GS, & GG


geomfdesc:
(a) The shoreline, especially a former (relict) shoreline now elevated above the present water level, that commonly appears as a bench or line wrapping around the landscape at a common elevation.  SW  (b) A beach, especially one raised above the present sea or lake level.  GG


geomfdesc:
A relatively deep, steep-banked lake or pool occupying an ice-gouged rock basin amid glaciated mountains.  A cirque lake.  GG


geomfdesc:
A small dome or mound on the surface of a lava flow formed by the buckling of the congealing crust near the edge of a flow caused by differences in  flow rates of the cooler crust above and the hotter, more fluid lava below.  Dimensions commonly range from < 1 m to 5 m in height, 3 to 10 m in width and 30 to 40 m in length.  Some tumuli are hollow.  Compare - pressure ridge [volcanic].  SW, GG, and GS


geomfdesc:
(colloquial - Southern High Plains) The generally concave to slightly convex area within a playa basin that lies between the relatively level playa floor below (or playa step, if present) and the convex playa rim above.  Overland flow is typically parallel down slope.  Compare - playa step, playa rim.  SW


geomfdesc:
(colloquial - Southern High Plains) The relatively level or gently inclined "terrace-like" bench or toeslope within a large playa basin flanking and topographically higher than the playa floor and below the playa slope; a bench or step-like surface within a playa basin that breaks the continuity of the playa slope and modified by erosion and/or deposition.  Temporary ponding may occur in response to precipitation / runoff events.  Compare - playa slope.  SW


geomfdesc:
A karst landscape dominated by subsurface drainage and serrate or star-shaped depressions (cockpits) that range widely in size and density but typically are considerably larger than sinkholes (dolines), and are separated by intermediate residual hills with concave side slopes; a common type of tropical karst (e.g. Jamaica).  Compare - kegel karst, karst.  SW & WW


geomfdesc:
A glacier of considerable thickness completely covering a large part of a continent or an area of at least 50,000 square km, obscuring the underlying surface, such as the ice sheets covering Antarctica or Greenland.  Continental glaciers occupied northern portions of  the coterminous USA and Alaska in the past (e.g., Pleistocene) and usage commonly implies former continental glacier conditions.   Compare - alpine glacier.  SW & GG


geomfdesc:
A karst landscape dominated by both 1) karst features (deranged and subsurface drainage, blind valleys, swallow holes, large springs, closed depressions, and caves), generally limited to interfluve areas, and 2) surface drainage by large rivers, with associated fluvial features (adjacent stream terraces) and sediments (alluvium), that commonly maintain their surface courses and are fed by underground tributaries; the dominant karst in the eastern USA.  Compare - sinkhole karst, pavement karst, karst.  SW, WW, & GG


geomfdesc:
A general name used to describe several types of humid tropical karst landscapes characterized by numerous, closely spaced cone- (cone karst), hemispherical- (halbkugelkarst), or tower-shaped (tower karst) hills with vertical or near-vertical walls and having intervening closed depressions and narrow steep-walled karst valleys or passageways.  Compare - cockpit karst.  GG & SW


geomfdesc:
A kind of topography formed in limestone, gypsum, or other soluable rocks by dissolution, and that is characterized by closed depressions, sinkholes, caves, and underground drainage.  Various types of karst can be recognized depending upon the dominant surface features:  karst dominated by closed depressions (sinkhole karst - temperate climates; cockpit karst - humid tropical climates), closed depressions and large rivers (fluviokarst), bare rock dominated by dissolution joints (pavement karst), tropical cone-, tower- or domed-hills (kegel karst), etc.  SW & WW


geomfdesc:
An area covered primarily by lava flows whose terrain can be rough and broken or relatively smooth; it can include vent structures (e.g., small cinder cones, spatter cones, etc.), surface flow structures (e.g., pressure ridges, tumuli, etc.) and small, intermittent areas covered with pyroclastics.  Compare - lava plain, volcanic field.  SW


geomfdesc:
(a) An elongated body or stretch of land nearly surrounded by water (e.g., on three sides) and connected with a larger tract of land area, usually by a neck or an isthmus.  (b) A relatively large tract of land jutting out into the water, with or without a well-defined isthmus; e.g., the Italian peninsula.  GG


geomfdesc:
(colloquial - western USA) The dominant gentle slope at the foot of a mountain; generally used in terms of intermontane-basin terrain in arid to subhumid regions.  Main components include: (a) An erosional surface on bedrock adjacent to the receding mountain front (pediment, rock pediment); (b) A constructional surface comprising individual alluvial fans and interfan valleys, also near the mountain front; and (c) A distal complex of coalescent fans (bajada), and alluvial slopes without fan form.  Piedmont slopes grade to basin-floor depressions with alluvial and temporary lake plains or to surfaces associated with through drainage (e.g., axial streams).  Compare - bolson, fan piedmont.  HP


geomfdesc:
A valley that has developed along a long, narrow continental trough that has down-dropped and is bounded by normal faults; a graben of regional size.  It marks part of a zone along which the entire thickness of the lithosphere has ruptured under crustal extension.  SW & GG


geomfdesc:
A landscape dominated by subsurface drainage and sinkholes (dolines) that range widely in sizes and density; the most common type of karst in temperate regions (e.g. Highland Rim of TN, northern FL, southwestern MO, etc.); also called doline karst (not preferred).  Compare - fluviokarst, pavement karst, karst.  SW, WW, & GG


geomfdesc:
A more or less well defined area that is covered with volcanic rocks of much more diverse lithology and distribution than a lava field, or that is so modified by age and erosion that it's original topographic configuration, composition and extent is uncertain.  Compare - lava field, lava plain.  SW


geomfdesc:
a) Any glacier in a mountain range except an ice cap or ice sheet.  It usually originates in a cirque and may flow down into a valley previously carved by a stream.  Compare - continental glacier.  GG  b) (not preferred - refer to U-shaped valley): (relict) - landforms or sediments formed, modified or deposited by a glacier in or on mountains or high hills that has since melted away.  Compare - glacial-valley floor, glacial-valley wall.  SW


geomfdesc:
A lava flow dominated by block lava.  Compare - a'a lava flow, pahoehoe lava, pillow lava.  SW


geomfdesc:
(colloquial: southeastern USA)  A type of very wide, low gradient (level to nearly level) interfluve that lacks a well developed drainage network such that large portions of the local upland lack stream channels or other drainageways; extensive in lower coastal plains and some lake plains, till plains and alluvial plain remnants.  Compare - interfluve.  SW & RD


geomfdesc:
The glacially-scoured, steep and arcuate side or wall of a cirque, dominated by rock-outcrops, rubble, and colluvium.  Compare - headwall.  SW & HD


geomfdesc:
A dune formed by the piling-up of sand by wind against a cliff or mountain slope; very common in arid regions with substantial local relief and strong winds.  Compare - sand ramp.  GG & SW


geomfdesc:
A crudely star-shaped, closed depression (i.e. large sinkhole) in tropical karst having an inverted conical or slightly concave floor, with an irregular or serrate  perimeter formed by subsidiary solution channels and corridors into adjacent hills, and surrounded by residual hills with steep, concave side slopes; the dominant type of closed depression in cockpit karst.  Compare - sinkhole, kegel karst.  SW, WW & GG


geomfdesc:
A type of sinkhole that is formed by collapse of a cave within the underlying soluble bedrock (e.g., limestone, gypsum, salt).  Compare - solution sinkhole.  SS, WW, & GG


geomfdesc:
An elongated hill or ridge of subglacially streamlined drift, having at the stoss end (up-ice) a steep, often precipitous face or knob of ice-smoothed, resistant bedrock (the "crag") obstructing the movement of the glacier, and at the lee end (down-ice) a tapering, streamlined, gentle slope (the "tai;") of intact, weaker rock and / or drift protected by the crag; also called lee-side cone.  Compare - drumlin, drumlinoid ridge, flute, stoss and lee.  GG, SW, & GM


geomfdesc:
The process, associated sediments (debris fall deposit) or resultant landform characterized by a rapid type of fall involving the relatively free, downslope movement or collapse of detached, unconsolidated material which falls freely through the air (lacks an underlying slip face); sediments have substantial proportions of both fine earth and coarse fragments; common along undercut stream banks.  Compare - rock fall, soil fall, landslide.  SW


geomfdesc:
The process, associated sediments (debris spread deposit) or resultant landforms characterized by a very rapid type of spread dominated by lateral movement in a soil and rock mass resulting from liquefaction or plastic flow of underlying materials that may be extruded out between intact units; sediments have substantial proportions of both fine earth and coarse fragments.  Compare - earth spread, rock spread, landslide.  SW & DV


geomfdesc:
The process, associated sediments (debris topple deposit) or resultant landform characterized by a localized, very rapid type of topple in which large blocks of soil and rock material literally fall over, rotating outward over a low pivot point;  sediments have substantial proportions of both fine earth and coarse fragments.  Portions of the original material may remain intact, although reoriented, within the resulting debris pile.  Compare - earth topple, rock topple, landslide.  SW


geomfdesc:
The process, associated sediments (earth spread deposit) or resultant landforms characterized by a very rapid type of spread dominated by lateral movement in a soil mass resulting from liquefaction or plastic flow of underlying materials that may be extruded out between intact units.  Compare - debris spread, rock spread, landslide.  SW & DV


geomfdesc:
The process, associated sediments (earth topple deposit) or resultant landform characterized by a localized, very rapid type of topple in which large blocks of soil material literally fall over, rotating outward over a low pivot point; sediments < 2 mm predominate.  Portions of the original material may remain intact, although reoriented, within the resulting deposit.  Compare - debris topple, rock topple, landslide.  SW


geomfdesc:
All, or a portion of an alluvial fan that is much more extensively eroded and dissected than a fan remnant; sometimes called an erosional fan remnant (FFP).  It consists primarily of a) eroded and highly dissected sides (eroded fan-remnant sideslopes) dominated by hillslope positions (shoulder, backslope, etc.), and b) to a lesser extent an intact, relatively planar, relict alluvial fan "summit" area best described as a tread.  SW & FFP


geomfdesc:
A rough or broken margin of an eroded fan remnant highly dissected by ravines and gullies that can be just a fringe or make up a large part of an eroded alluvial fan; its bounding escarpments (risers), originally formed by inset channels, have become highly dissected and irregular such that terrace components (tread and riser) have been consumed or modified and replaced by hillslope positions and components (shoulder, backslope, footslope, etc.); sometimes referred to as fan remnant sideslopes (FFP).  Compare - eroded fan remnant.  SW & FFP


geomfdesc:
A landform comprised of a thin, short, relatively young mantle of alluvium along the very upper margin  (near the proximal end or apex) of a major alluvial fan.   The young mantle somewhere buries an older soil that can be traced to the edge of the collar where the older soil emerges at the land surface as a relict soil.  Compare - fan apron.  FFP


geomfdesc:
A category of mass movement processes, associated sediments (flow deposit) and landforms characterized by slow to very rapid downslope movement of unconsolidated material which, whether saturated or comparatively dry, behaves much as a viscous fluid as it moves. Types of flows can be specified based on the dominant particle size of sediments (i.e. debris flow (e.g., lahar), earth flow (creep, mudflow), rock fragment flow (e.g., rockfall avalanche), debris avalanche]. Compare - fall, topple, slide, lateral spread, complex landslide, landslide.  SW & DV


geomfdesc:
A type of hot spring that intermittently erupts jets of hot water and steam, the result of ground water coming in contact with rock or steam hot enough to create steam under conditions preventing free circulation; a type of intermittent spring.  Compare - mud pot, hot spring.  GG


geomfdesc:
A valley that contains numerous springs, geysers, and steam fissures fed by the same ground-water flow.  GG


geomfdesc:
A low hill or mound built up of siliceous sinter around the orifice of a geyser. GG


geomfdesc:
A generic name for an elevated, generally rounded land surface with high local relief, rising between 90 meters (approx. 300 ft.) to as much as 300 m (approx. 1000 ft.) above surrounding lowlands.  Compare - low hill, hill, hillock.  SW


geomfdesc:
A natural, geothermally heated spring whose temperature is above that of the human body.  Compare - geyser, mud pot.  GG


geomfdesc:
A large, flat-floored closed depression in a karst area whose drainage is ultimately subsurface and its floor is commonly covered by alluvium.  Some interior valleys may become ephemeral lakes during periods of heavy rainfall, when sinking streams that drain them cannot manage the runoff; also called polje (not preferred).  Compare - karst valley, sinkhole.  GG


geomfdesc:
A conically-shaped residual hill in karst with a rounded top and relatively steep, convex (e.g. parabolic) side slopes, commonly in tropical climates.  Compare - karst tower, mogote.  SW & WW


geomfdesc:
An isolated, separate hill or ridge in a karst region consisting of an erosional remnant of limestone or other sedimentary rocks with vertical or near-vertical, convex side slopes and commonly surrounded by an alluviated plain or deep rugged ravines.  Compare - mogote, karst cone.  SW


geomfdesc:
A closed depression formed by the coalescence of multiple sinkholes; an elongate, solutional valley.  Its drainage is subsurface, diameters range from several hundred meters to a few kilometers, and it usually has a scalloped margin inherited from the sinkholes.  It may have nominal, local channel flow (small streams), sequential sinkhole inlets (springs) and outlets (swallow hole, etc.); also called compound sinkhole (not preferred), uvala (not preferred).  Compare - sinkhole, interior valley.  SW & GG


geomfdesc:
A generic name for an elevated, generally rounded land surface with low local relief, rising between 30 meters (100 ft.) to as much as 90 m (approx. 300 ft.) above surrounding lowlands.  Compare - high hill, hill, hillock.  SW


geomfdesc:
An impact crater formed by the falling of a large meteorite onto the earth's surface; e.g., Barringer Crater (AZ).  Compare - crater, impact crater.  SW & GG


geomfdesc:
A type of hot spring containing boiling mud, usually sulfurous and often multicolored, as in a paint pot.  Mud pots are commonly associated with geysers and other hot springs in volcanic areas, especially in Yellowstone Natl. Park, WY.  Compare - geyser, hot spring.  GG


geomfdesc:
A vertical, pipe-like tower of solidified lava or consolidated fragmental igneous rock that represents a former volcanic vent whose surrounding material (e.g. tuff and tephra) has been largely removed by erosion.  Compare - volcanic plug.    SW, GG, & GS


geomfdesc:
A relict (inactive) delta composed of glaciofluvial sediments formed where a sediment laden outwash river emptied into an open lake, commonly a proglacial lake.  Sediment attributes include very gently dipping topset beds (coarser textures) and steeply dipping foreset beds (finer textures).  SW & GM


geomfdesc:
Areas of bare limestone, usually sculpted by solution erosion into karren of various types and where soils have been stripped off, commonly by glaciation in alpine areas (e.g. Rocky Mountains - USA) and high latitudes, and by water erosion in arid karst areas.  Compare - fluviokarst, sinkhole karst, karst.  SW & WW


geomfdesc:
A lava flow or body displaying pillow structure and considered to have formed in a subaqueous environment (underwater); usually basaltic or andesitic in composition.  Compare - a'a lava flow, block lava flow, pahoehoe lava flow.  SW & GS


geomfdesc:
The bottom of a shallow, extinct glacial lake composed of thin (e.g., < 2 m thick), fine-textured, reworked  lacustrine sediments that overlie outwash or till; original lacustrine sediments have been subsequently redistributed primarily by wave action (eroded and / or moved a short distance).  A distinctive lake plain topography is not always present.  It may include subdued, till-capped topographic highs, ringed by shores or strandlines, that were once emergent islands.  Common to MI, OH.  SW


geomfdesc:
The process, associated sediments (rock spread deposit) or resultant landforms characterized by a very rapid type of spread dominated by lateral movement in a rock mass resulting from liquefaction or plastic flow of underlying materials that may be extruded out between intact units; rock bodies predominate.  Compare - debris spread, earth spread, landslide.  SW & DV


geomfdesc:
The process, associated sediments (rock topple deposit) or resultant landform characterized by a localized, very rapid type of fall in which large blocks of rock material literally fall over, rotating outward over a low pivot point; rock bodies predominate (little fine earth).  Portions of the original material may remain intact, although reoriented, within the resulting deposit.  Compare - earth topple, debris topple, landslide.  SW


geomfdesc:
The process, associated sediments (rotational debris slide deposit) or resultant landform characterized by an extremely slow to moderately rapid type of slide, composed of comparatively dry and largely unconsolidated earthy material, portions of which remain largely intact and in which movement occurs along a well-defined, concave shear surface and resulting in a backward rotation of the displaced mass; sediments have substantial proportions of both fine earth and coarse fragments.  The landform may be single, successive (repeated up and down slope), or multiple (as the number of slide components increase).  Compare - rotational earth slide, rotational rock slide, translational slide, lateral spread, landslide.  SW & DV


geomfdesc:
The process, associated sediments (rotational earth slide deposit) or resultant landform characterized by an extremely slow to moderately rapid type of slide, composed of comparatively dry and largely unconsolidated earthy material, portions of which remain largely intact and in which movement occurs along a well-defined, concave shear surface and resulting in a backward rotation of the displaced mass; sediments predominantly fine earth (< 2 mm).  The landform may be single, successive (repeated up and down slope), or multiple (as the number of slide components increase).  Compare - rotational debris slide, rotational rock slide, translational slide, lateral spread, landslide.  SW & DV


geomfdesc:
The process, associated sediments (rotational rock slide deposit) or resultant landform characterized by an extremely slow to moderately rapid type of slide, composed of comparatively dry and largely consolidated rock bodies, portions of which remain largely intact but reoriented, and in which movement occurs along a well-defined, concave shear surface and resulting in a backward rotation of the displaced mass.  The landform may be single, successive (repeated up and down slope), or multiple (as the number of slide components increase).  Compare - rotational debris slide, rotational earth slide, translational slide, lateral spread, landslide.  SW & DV


geomfdesc:
A sand sheet blown up onto the lower slopes of a bedrock hill or mountain and forming an inclined plane, sometimes filling small mountain-side valleys and even crossing low passes.  Compare - climbing dune, sand sheet.  FFP & SW


geomfdesc:
a) A broad expanse of terrain covered with snow, relatively smooth and uniform in appearance, occurring usually at high latitudes or in mountainous regions above the snowline and persisting throughout year.  b)  A region of permanent snow cover, as at the head of a glacier; the accumulation area of a glacier.  Compare -  glacier.  GG


geomfdesc:
The most common type of sinkhole, caused by dissolution that forms fissures or a chimney and a depression in the bedrock surface which grows when closely spaced fissures underneath it enlarge and coalesce.  Compare - collapse sinkhole.  SW, WW, & GG


geomfdesc:
A large, isolated sand dune whose base, in plan view, resembles a star, with sharp-crested ridges converging from basal points to a central peak that may be as high as 100 m above the surrounding plain.  It tends to remain fixed for centuries in an area where the wind blows from all directions.  Compare - dune.  GG


geomfdesc:
An arrangement of small hills or prominent rocks, in a strongly glaciated area, having gentle slopes on the stoss ("up-ice") side and somewhat steeper, plucked slopes on the lee ("down-ice") side.  This arrangement is the opposite of crag and tail.  Compare - crag and tail, drumlin, drumlinoid ridge, flute.  GG


geomfdesc:
A small, steep, cone-shaped landform at the base of a cliff or escarpment, that heads in a relatively small declivity or ravine, and composed of poorly sorted rock and soil debris that has accumulated primarily by episodic rockfall or, to a lesser degree, by slope wash.  Not to be confused with an alluvial cone; a similar feature but of fluvial origin, composed of better stratified and more sorted material, and that tapers up into a more extensive drainageway.  Compare - alluvial cone, talus slope.  SW


geomfdesc:
Part of, or the entire floor of, an extinct glacial lake where a thin (e.g. < 2 m), often discontinuous veneer of lacustrine sediments overlies till.  Topography reflects the underlying, irregular or undulating till surface rather than a distinctive, flat, lake plain surface.  It may include subdued, till-capped topographic highs, ringed by shores or strandlines, that were once emergent islands.  SW


geomfdesc:
The process, associated sediments (translational debris slide deposit) or resultant landform characterized by an extremely slow to moderately rapid type of slide, composed of comparatively dry and largely unconsolidated earthy material, portions or blocks of which remain largely intact and in which movement occurs along a well-defined, planar slip face roughly parallel to the ground surface and resulting in lateral displacement but no rotation of the displaced mass; sediments have substantial proportions of both fine earth and coarse fragments.  The landform may be single, successive (repeated up and down slope), or multiple (as the number of slide components increase).  Compare - translational earth slide, translational rock slide, rotational slide lateral spread, landslide.  SW & DV


geomfdesc:
The process, associated sediments (translational earth slide deposit) or resultant landform characterized by an extremely slow to moderately rapid type of slide, composed of comparatively dry and largely unconsolidated earthy material, portions or blocks of which remain largely intact and in which movement occurs along a well-defined, planar slip face roughly parallel to the ground surface and resulting in lateral displacement but no rotation of the displaced mass; sediments predominantly fine earth (< 2 mm).  The landform may be single, successive (repeated up and down slope), or multiple (as the number of slide components increase).  Compare - translational debris slide, translational rock slide, rotational slide, lateral spread, landslide.  SW & DV


geomfdesc:
The process, associated sediments (translational rock slide deposit) or resultant landform characterized by an extremely slow to moderately rapid type of slide, composed of comparatively dry and largely consolidated rock bodies, portions or blocks of which remain largely intact and in which movement occurs along a well-defined, planar slip face roughly parallel to the ground surface and resulting in lateral displacement but no rotation of the displaced mass; sediments predominantly fine earth (< 2 mm).  The landform may be single, successive (repeated up and down slope), or multiple (as the number of slide components increase).  Compare - translational debris slide, translational earth slide, rotational slide, lateral spread, landslide.  SW & DV


geomfdesc:
A rugged, irregular wall of broken floating ice buckled upward by the lateral pressure of wind or current forcing or squeezing one floe against another, or against a shore; it may extend for kilometers in length and up to 30 m in height.  Along shores they are lower (< 10 m tall)  and  contribute to the temporary or permanent formation of a beach berm or a rim of boulders and stones.  SW & GG


geomfdesc:
The process, associated sediments (rotational landslide deposit) or resultant landforms characterized by an extremely slow to moderately rapid type of slide, composed of comparatively dry and largely soil-rock materials, portions of which remain largely intact and in which movement occurs along a well-defined, concave shear surface and resulting in a backward rotation of the displaced mass.  The landform may be single, successive (repeated up and down slope), or multiple (as the number of slide components increase).  Compare - rotational debris slide, rotational earth slide, rotational rock slide, translational slide, lateral spread, landslide.  SW & DV


geomfdesc:
A large, generally discordant plutonic rock body exposed at the land surface, with an aerial extent > 40 sq. mi. (100 km2) and no known bottom (e.g. Idaho batholith).  Compare - stock.  SW & GG


geomfdesc:
The lower portion of a canyon wall or escarpment marked by a sharp reduction in slope gradient from the precipitous cliff  above, and characteristically composed of thinly mantled colluvium (e.g. < 1 m) and / or carapaced with a thin surficial mantle of large rock fragments from above, which overly residuum of less resistant rock (e.g., shale) whose thin strata intermittently outcrop at the surface; a zone of erosion and transport common in the canyonlands of the semi-arid southwestern USA.  Compare - talus.  SW


geomfdesc:
An accumulation of sand that is formed as sand is blown off a mesa top or over a cliff face or steep slope, forming a solid wall, sloping at the angle of repose of dry sand, or a fan extending downward from a re-entrant in the mesa wall.  Compare - climbing dune, sand ramp.  GG


geomfdesc:
A fault that is expressed as a zone of numerous small fractures or of breccia or fault gouge.  A fault zone may be as wide as hundreds of meters.  Compare - fault, fault-scarp.  GG


geomfdesc:
A low relief, broad volcanic crater formed by multiple, shallow explosive eruptions.  It is surrounded by a crater ring in the form of low ramparts of gently dipping (i.e. < 25 degrees), well-bedded ejecta; may be filled by water.  SW & GG


geomfdesc:
A low density, dilute, turbulent pyroclastic flow, usually very hot, composed of a generally unsorted mixture of gases, ash, pumice and dense rock fragments that travels across the ground at high speed and less constrained by topography than a pyroclastic flow; several types of pyroclastic surges can be specified (e.g. base surge, ash-cloud-surge).  Compare - pyroclastic flow.  SW, SN, GG


geomfdesc:
A fast density current of pyroclastic material, usually very hot, composed of a mixture of gasses and a variety of pyroclastic particles (ash, pumice, scoria, lava fragments, etc.); produced by the explosive disintegration of viscous lava in a volcanic crater or by the explosive emission of gas-charged ash from a fissure and which tends to follow topographic lows (e.g. valleys) as it moves; used in a more general sense than ash flow.  Compare - pyroclastic surge, ash flow, nue ardente, lahar.  SW, SN, GG


geomfdesc:
A relatively small, concordant and / or discordant plutonic rock body exposed at the land surface, with an aerial extent < 40 sq. mi. (100 km2) and no known bottom.  Compare - batholith.  GG


geomfdesc:
A type of gilgai dominated by circular closed depressions (micro-lows) separated by low mounds (micro-highs); the prevailing type of gilgai on relatively level terrain (slopes < 3 %).  Distance from micro-high to the center of an adjacent microlow is generally 4 - 8 8 m.  Compare - elliptical gilgai, linear gilgai, gilgai.  SW


geomfdesc:
A type of gilgai dominated by elliptical, closed and semi-closed depressions (micro-lows) separated by low mounds or ridges (micro-highs); the prevailing type of gilgai on mildly sloping terrain (slopes 3 - 8%); as slope increases, basins become more eccentric and the occurrence of interconnected micro-lows increases.  Compare - circular gilgai, linear gilgai, gilgai.  SW


geomfdesc:
A nearly level area, including the lower part (footslope) of a micro-high, that is a transition zone between the slightly elevated micro-high (i.e. microknoll; mound in Russia) and the outer edge of an adjacent micro-low (i.e. microbasin, microtrough; depression in Russia) in gilgai.  Where present, it can make up a majority of the ground surface area in gilgai; called slope in Russia.  Compare - ephemeral stream.  HP


geomfdesc:
A type of gilgai dominated by parallel micro-low troughs separated by low ridges (micro-highs) and oriented perpendicular to the topographic contour (i.e., up and down slopes); the prevailing type of gilgai on sloping terrain (slopes > 8 %).  Compare - circular gilgai, elliptical gilgai, gilgai.  SW


geomfdesc:
A surface drape or exposure of  up-welled  substratum material forced to the surface and outcropping on a low mound or rim; the surface exposure of a chimney [gilgai]; a type of diapir composed of earthy material.  Compare - chimney, intermediate position [gilgai], gilgai.  SW


geomfdesc:
a) A narrow gorge or canyon containing an intermittent stream following a zig-zag course, characterized by high, steep rock walls and typically closed upstream by a similar wall, giving the impression, as viewed from its bottom, of being surrounded or "boxed-in" by almost vertical walls.  b) A steep-walled canyon heading against a cliff a dead-end canyon.  GG


geomfdesc:
An opening in earth's surface of a volcanic conduit in the form of a crack or fissure rather than a localized crater; a roughly linear crack or area along which lava, generally mafic and of low viscosity, wells up to the surface, usually without any explosive activity.  The results can be an extensive lava plateau (e.g. Columbia River Plateau).  Compare - crater [volcanic].  SW & GG


geomfdesc:
A long, narrow, deep and tortuous channel or drainageway with sheer rock walls eroded into sandstone or other sedimentary rocks, especially in the semi-arid western USA (e.g. Colorado Plateau); subject to flash flood events; depth to width ratios exceed 10:1 over most of its length and can approach 100:1; commonly containing unique ecological communities distinct from the adjacent, drier uplands.  SW


geomfdesc:
A steep surface on the displaced material of a landslide, produced by differential movements within the sliding mass.   Compare - main scarp, toe.  CV


geomfdesc:
The steep surface on undisturbed ground at the upper edge of a landslide, caused by movement of displaced material away from the undisturbed ground; it is visible a part of the surface of rupture (slip surface).  Compare - minor scarp, toe.  CV & SW


geomfdesc:
A relatively large depression resulting from the excavation of material and redistribution of overburden associated with surficial mining operations.  Compare - quarry, surface mine.  SW & GG


geomfdesc:
A group of mountain ranges exhibiting certain unifying features, such as similarity in form, structure and alignment, and presumably originating from the same general causes; especially a series of mountain ranges belonging to an orogenic belt.  Compare - mountain range, mountains.  GG


geomfdesc:
A single, large mass consisting of a succession of mountains or narrowly spaced mountain ridges, with or without peaks, closely related in position, direction, orientation, formation, and age; a component part of a mountain system.  Compare - mountain system, mountains.  GG


geomfdesc:
(a) An informal, generic term for low-lying land or an extensive region of low-lying land, especially near a coast and including the extended plains or country lying not far above tide level.  (b) (not preferred) A genericvague, imprecise term for a landscape of low, comparatively level ground of a region or local area, in contrast with the adjacent higher country.  (c) (not recommended use valley, bolson, etc.) A generic term for a large valley.  Compare - upland.  SW


geomfdesc:
The lowest, usually curved margin of displaced material of a landslide, most distant from the main scarp.  Commonly it has an irregular surface that has ripples and may be breached by radial cracks or gaps.  Compare - main scarp, minor scarp.  CV & SW


geomfdesc:
A constructional coastal strip, sloping gently seaward and/or down valley, veneered by or completely composed of unconsolidated sediments (typically silt, sand, fine gravel).  Sediments were deposited by both marine and fluvial processes, resulting from sea level flucuations and/or stream migration (e.g. materials deposited in a nearshore environment and reworked by fluvial processes as sea level fell, or visa versa as sea level rose).  Compare - terrace, stream terrace, marine terrace.


geomfdesc:
An extensive, nearly level tract of land that is alternately covered and uncovered by the tide, and composed of unconsolidated sediments (clays, silts and/or sand and organic materials) and a resistant root mat, and vegetated dominantly by hydrophytic (salt tolerant) plants.  The mineral sediments largely retain pedogenic horizonation and morphology (e.g. argillic horizons) developed under better drained, terrestrial conditions prior to submergence due to sea level rise; a type of tidal marsh.  Compare - tidal marsh.


# SYSTEM - Geomorphic Feature Type

geomftdesc:
Any physical, recognizable form or feature on the earth's surface, having a characteristic shape and range in composition, and produced by natural causes; it can span a wide range in size (e.g., dune encompasses both parabolic dune, which can be several tens-of-meters across, as well as seif dune which can be up to 100 kilometers long).  Landforms provide an empirical description of similar portions of the earth's surface.  SW & GG


geomftdesc:
An assemblage, group, or family of spatially related, natural landforms over a relatively large area; the land surface which the eye can comprehend in a single view.  SW & GSST


geomftdesc:
Small, local, natural forms (features) on the land surface that are too small to delineate on a topographic or soils map at commonly used map scales (e.g. 1:24,000 to 1:10,000).  Examples include earth pillars, patterned ground, frost boils.  Compare - microrelief.  SW


geomftdesc:
An artificial feature on the land surface, having a characteristic shape and range in composition, composed of unconsolidated earthy or organic materials, artificial materials, or rock, that is the direct result of human manipulation or activities; can be either constructional(e.g. artificial levee) or destructional(e.g. quarry).  SW


# SYSTEM - Help Text

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The purpose of this report is to provide a soil interpretation report that includes soil interpretations not available in any of the standard manuscript reports, or to be able to group soil interpretations differently from any grouping available in the standard manuscript reports.

You may select one, two or three soil interpretations to be included in the report.  When report generation is invoked, all selected interpretations must be consecutive, starting with the first interpretation.  The first selected interpretation will be the leftmost in the corresponding report.

When you select an interpretation, that interpretation’s name is copied into the corresponding interpretation column heading blank.  You can replace the default interpretation column heading with whatever you desire.  If you delete the default interpretation column heading, the original default interpretation column heading will be used.

You may specify a title for this report, which appears at the top of every page in the report.  You can replace the default report title with whatever you desire.  If you delete the default report title, the original default report title will be used.


# SYSTEM - Soil Reports

Report Name:
Acreage and Proportionate Extent of the Soils

Report Title:
Acreage and Proportionate Extent of the Soils

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Acreage and Proportionate Extent of the Soils


Report Name:
Acreage and Proportionate Extent of the Soils by County

Report Title:
Acreage and Proportionate Extent of the Soils by County

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Acreage and Proportionate Extent of the Soils by County

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Report Parameters - Counties or Parishes


Report Name:
Agricultural Disposal of Manure, Food-Processing Waste, and Sewage Sludge

Report Title:
Agricultural Disposal of Manure, Food-Processing Waste, and Sewage Sludge

Report Header Text:
[The information in this table indicates the dominant soil condition but does not eliminate the need for onsite investigation.  The numbers in the value columns range from 0.01 to 1.00.  The larger the value, the greater the potential limitation.  The table shows only the top five limitations for any given soil.  The soil may have additional limitations]

Access Report Name:
Template Interpretation Report - 2 Interpretations

Report Documentation:
Soil properties are important considerations in areas where soils are used as sites for the treatment and disposal of organic waste and wastewater. Selection of soils with properties that favor waste management can help to prevent environmental damage.

This table shows the degree and kind of soil limitations affecting the treatment of agricultural waste, including municipal and food-processing wastewater and effluent from lagoons or storage ponds. Municipal wastewater is the waste stream from a municipality. It contains domestic waste and may contain industrial waste. It may have received primary or secondary treatment. It is rarely untreated sewage. Food-processing wastewater results from the preparation of fruits, vegetables, milk, cheese, and meats for public consumption. In places it is high in content of sodium and chloride. In the context of these tables, the effluent in lagoons and storage ponds is from facilities used to treat or store food-processing wastewater or domestic or animal waste. Domestic and food-processing wastewater is very dilute, and the effluent from the facilities that treat or store it commonly is very low in content of carbonaceous and nitrogenous material; the content of nitrogen commonly ranges from 10 to 30 milligrams per liter. The wastewater from animal waste treatment lagoons or storage ponds, however, has much higher concentrations of these materials, mainly because the manure has not been diluted as much as the domestic waste. The content of nitrogen in this wastewater generally ranges from 50 to 2,000 milligrams per liter. When wastewater is applied, checks should be made to ensure that nitrogen, heavy metals, and salts are not added in excessive amounts.

The ratings in the table are for waste management systems that not only dispose of and treat organic waste or wastewater but also are beneficial to crops. The ratings are both verbal and numerical. Rating class terms indicate the extent to which the soils are limited by all of the soil features that affect agricultural waste management. Not limited indicates that the soil has features that are very favorable for the specified use. Good performance and very low maintenance can be expected. Somewhat limited indicates that the soil has features that are moderately favorable for the specified use. The limitations can be overcome or minimized by special planning, design, or installation. Fair performance and moderate maintenance can be expected. Very limited indicates that the soil has one or more features that are unfavorable for the specified use. The limitations generally cannot be overcome without major soil reclamation, special design, or expensive installation procedures. Poor performance and high maintenance can be expected.

Numerical ratings in the tables indicate the severity of individual limitations. The ratings are shown as decimal fractions ranging from 0.01 to 1.00. They indicate gradations between the point at which a soil feature has the greatest negative impact on the use (1.00) and the point at which the soil feature is not a limitation (0.00).

Application of manure and food-processing waste not only disposes of waste material but also can improve crop production by increasing the supply of nutrients in the soils where the material is applied. Manure is the excrement of livestock and poultry, and food-processing waste is damaged fruit and vegetables and the peelings, stems, leaves, pits, and soil particles removed in food preparation. The manure and food-processing waste are solid, slurry, or liquid. Their nitrogen content varies. A high content of nitrogen limits the application rate. Toxic or otherwise dangerous wastes, such as those mixed with the lye used in food processing, are not considered in the ratings.

The ratings are based on the soil properties that affect absorption, plant growth, microbial activity, erodibility, the rate at which the waste is applied, and the method by which the waste is applied. The properties that affect absorption include saturated hydraulic conductivity (Ksat), depth to a water table, ponding, the sodium adsorption ratio, depth to bedrock or a cemented pan, and available water capacity. The properties that affect plant growth and microbial activity include reaction, the sodium adsorption ratio, salinity, and bulk density. The wind erodibility group, the soil erodibility factor K, and slope are considered in estimating the likelihood that wind erosion or water erosion will transport the waste material from the application site. Stones, cobbles, a water table, ponding, and flooding can hinder the application of waste. Permanently frozen soils are unsuitable for waste treatment.

Application of sewage sludge not only disposes of waste material but also can improve crop production by increasing the supply of nutrients in the soils where the material is applied. In the context of this table, sewage sludge is the residual product of the treatment of municipal sewage. The solid component consists mainly of cell mass, primarily bacteria cells that developed during secondary treatment and have incorporated soluble organics into their own bodies. The sludge has small amounts of sand, silt, and other solid debris. The content of nitrogen varies. Some sludge has constituents that are toxic to plants or hazardous to the food chain, such as heavy metals and exotic organic compounds, and should be analyzed chemically prior to use.

The content of water in the sludge ranges from about 98 percent to less than 40 percent. The sludge is considered liquid if it is more than about 90 percent water, slurry if it is about 50 to 90 percent water, and solid if it is less than about 50 percent water.

The ratings in the table are based on the soil properties that affect absorption, plant growth, microbial activity, erodibility, the rate at which the sludge is applied, and the method by which the sludge is applied. The properties that affect absorption, plant growth, and microbial activity include Ksat, depth to a water table, ponding, the sodium adsorption ratio, depth to bedrock or a cemented pan, available water capacity, reaction, salinity, and bulk density. The wind erodibility group, the soil erodibility factor K, and slope are considered in estimating the likelihood that wind erosion or water erosion will transport the waste material from the application site. Stones, cobbles, a water table, ponding, and flooding can hinder the application of sludge. Permanently frozen soils are unsuitable for waste treatment.


Report Name:
Agricultural Disposal of Wastewater by Rapid Infiltration and Slow Rate Treatment

Report Title:
Agricultural Disposal of Wastewater by Rapid Infiltration and Slow Rate Treatment

Report Documentation:
Soil properties are important considerations in areas where soils are used as sites for the treatment and disposal of organic waste and wastewater. Selection of soils with properties that favor waste management can help to prevent environmental damage.

This table shows the degree and kind of soil limitations affecting the treatment of wastewater, including municipal and food-processing wastewater and effluent from lagoons or storage ponds. Municipal wastewater is the waste stream from a municipality. It contains domestic waste and may contain industrial waste. It may have received primary or secondary treatment. It is rarely untreated sewage. Food-processing wastewater results from the preparation of fruits, vegetables, milk, cheese, and meats for public consumption. In places it is high in content of sodium and chloride. In the context of these tables, the effluent in lagoons and storage ponds is from facilities used to treat or store food-processing wastewater or domestic or animal waste. Domestic and food-processing wastewater is very dilute, and the effluent from the facilities that treat or store it commonly is very low in content of carbonaceous and nitrogenous material; the content of nitrogen commonly ranges from 10 to 30 milligrams per liter. The wastewater from animal waste treatment lagoons or storage ponds, however, has much higher concentrations of these materials, mainly because the manure has not been diluted as much as the domestic waste. The content of nitrogen in this wastewater generally ranges from 50 to 2,000 milligrams per liter. When wastewater is applied, checks should be made to ensure that nitrogen, heavy metals, and salts are not added in excessive amounts.

The ratings in the table are for waste management systems that not only dispose of and treat wastewater but also are beneficial to crops.  The ratings are both verbal and numerical. Rating class terms indicate the extent to which the soils are limited by all of the soil features that affect agricultural waste management. Not limited indicates that the soil has features that are very favorable for the specified use. Good performance and very low maintenance can be expected. Somewhat limited indicates that the soil has features that are moderately favorable for the specified use. The limitations can be overcome or minimized by special planning, design, or installation. Fair performance and moderate maintenance can be expected. Very limited indicates that the soil has one or more features that are unfavorable for the specified use. The limitations generally cannot be overcome without major soil reclamation, special design, or expensive installation procedures. Poor performance and high maintenance can be expected.

Numerical ratings in the tables indicate the severity of individual limitations. The ratings are shown as decimal fractions ranging from 0.01 to 1.00. They indicate gradations between the point at which a soil feature has the greatest negative impact on the use (1.00) and the point at which the soil feature is not a limitation (0.00).

Rapid infiltration of wastewater is a process in which wastewater applied in a level basin at a rate of 4 to 120 inches per week percolates through the soil. The wastewater may eventually reach the ground water. The application rate commonly exceeds the rate needed for irrigation of cropland. Vegetation is not a necessary part of the treatment; hence, the basins may or may not be vegetated. The thickness of the soil material needed for proper treatment of the wastewater is more than 72 inches. As a result, geologic and hydrologic investigation is needed to ensure proper design and performance and to determine the risk of ground-water pollution.

The ratings in the table are based on the soil properties that affect the risk of pollution and the design, construction, and performance of the system. Depth to a water table, ponding, flooding, and depth to bedrock or a cemented pan affect the risk of pollution and the design and construction of the system. Slope, stones, and cobbles also affect design and construction. Ksat and reaction affect performance. Permanently frozen soils are unsuitable for waste treatment.

Slow rate treatment of wastewater is a process in which wastewater is applied to land at a rate normally between 0.5 inch and 4.0 inches per week. The application rate commonly exceeds the rate needed for irrigation of cropland. The applied wastewater is treated as it moves through the soil. Much of the treated water may percolate to the ground water, and some enters the atmosphere through evapotranspiration. The applied water generally is not allowed to run off the surface. Waterlogging is prevented either through control of the application rate or through the use of tile drains, or both.

The ratings in the table are based on the soil properties that affect absorption, plant growth, microbial activity, erodibility, and the application of waste. The properties that affect absorption include the sodium adsorption ratio, depth to a water table, ponding, available water capacity, Ksat, depth to bedrock or a cemented pan, reaction, the cation-exchange capacity, and slope. Reaction, the sodium adsorption ratio, salinity, and bulk density affect plant growth and microbial activity. The wind erodibility group, the soil erodibility factor K, and slope are considered in estimating the likelihood of wind erosion or water erosion. Stones, cobbles, a water table, ponding, and flooding can hinder the application of waste. Permanently frozen soils are unsuitable for waste treatment.


Report Name:
Irrigated and Nonirrigated Yields by Map Unit Component

Report Title:
Irrigated and Nonirrigated Yields by Map Unit Component

Report Header Text:
[Yields in the "N" columns are for nonirrigated areas; those in the "I" column are for irrigated areas.  Yields are those that can be expected under a high level of management.  Absence of a yield indicates that the soil is not suited to the crop or the crop generally is not grown on the soil]

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Irrigated and Nonirrigated Yields by Map Unit Component

Report Documentation:
The average yields per acre that can be expected of the principal crops under a high level of management are shown in the crop yield table. In any given year, yields may be higher or lower than those indicated in the table because of variations in rainfall and other climatic factors. The land capability classification of map units in the survey area also is shown in the table (United States Department of Agriculture, Soil Conservation Service. 1961).

The yields are based mainly on the experience and records of farmers, conservationists, and extension agents. Available yield data from nearby counties and results of field trials and demonstrations also are considered.

The management needed to obtain the indicated yields of the various crops depends on the kind of soil and the crop. Management can include drainage, erosion control, and protection from flooding; the proper planting and seeding rates; suitable high-yielding crop varieties; appropriate and timely tillage; control of weeds, plant diseases, and harmful insects; favorable soil reaction and optimum levels of nitrogen, phosphorus, potassium, and trace elements for each crop; effective use of crop residue, barnyard manure, and green manure crops; and harvesting that ensures the smallest possible loss.

If yields of irrigated crops are present, it is assumed that the irrigation system is adapted to the soils and to the crops grown, that good-quality irrigation water is uniformly applied as needed, and that tillage is kept to a minimum.

The estimated yields reflect the productive capacity of each soil for each of the principal crops. Yields are likely to increase as new production technology is developed. The productivity of a given soil compared with that of other soils, however, is not likely to change.

Crops other than those shown in the crop yield table are grown in the survey area, but estimated yields are not listed because the acreage of such crops is small. The local office of the Natural Resources Conservation Service or of the Cooperative Extension Service can provide information about the management and productivity of the soils for those crops.

Reference:
United States Department of Agriculture, Soil Conservation Service. 1961. Land capability classification. U.S. Department of Agriculture Handbook 210.


Report Name:
Irrigated and Nonirrigated Yields by Map Unit

Report Title:
Irrigated and Nonirrigated Yields by Map Unit

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Irrigated and Nonirrigated Yields by Map Unit


Report Name:
Nonirrigated Yields by Map Unit Component

Report Title:
Nonirrigated Yields by Map Unit Component

Report Header Text:
[Yields are those that can be expected under a high level of management. They are for nonirrigated areas.   Absence of a yield indicates that the soil is not suited to the crop or the crop generally is not grown on the soil]

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Nonirrigated Yields by Map Unit Component


Report Header Text:
[Yields are those that can be expected under a high level of management. They are for irrigated areas.   Absence of a yield indicates that the soil is not suited to the crop or the crop generally is not grown on the soil]


Report Header Text:
[Yields are those that can be expected under a high level of management.  They are for irrigated areas.  Absence of a yield indicates that the soil is not suited to the crop or the crop generally is not grown on the soil]


Report Header Text:
[Yields are those that can be expected under a high level of management.  They are for nonirrigated areas.  Absence of a yield indicates that the soil is not suited to the crop or the crop generally is not grown on the soil]


Report Header Text:
[Only the soils that support rangeland vegetation suitable for grazing are rated]

Report Documentation:
In areas that have similar climate and topography, differences in the kind and amount of vegetation produced on rangeland are closely related to the kind of soil. Effective management is based on the relationship between the soils and vegetation and water.

This table shows, for each soil that supports rangeland vegetation, the ecological site and the potential annual production of vegetation in favorable, normal, and unfavorable years. An explanation of the column headings in the table follows.

An ecological site is the product of all the environmental factors responsible for its development. It has characteristic soils that have developed over time throughout the soil development process; a characteristic hydrology, particularly infiltration and runoff, that has developed over time; and a characteristic plant community (kind and amount of vegetation). The hydrology of a site is influenced by development of the soil and plant community. The vegetation, soils, and hydrology are all interrelated. Each is influenced by the others and influences the development of the others. The plant community on an ecological site is typified by an association of species that differs from that of other ecological sites in the kind and/or proportion of species or in total production. Descriptions of ecological sites are provided in the Field Office Technical Guide, which is available in local offices of the Natural Resources Conservation Service (NRCS).

Total dry-weight production is the amount of vegetation that can be expected to grow annually on well managed rangeland that is supporting the potential natural plant community. It includes all vegetation, whether or not it is palatable to grazing animals. It includes the current year's growth of leaves, twigs, and fruits of woody plants. It does not include the increase in stem diameter of trees and shrubs. It is expressed in pounds per acre of air-dry vegetation for favorable, normal, and unfavorable years. In a favorable year, the amount and distribution of precipitation and the temperatures make growing conditions substantially better than average. In a normal year, growing conditions are about average. In an unfavorable year, growing conditions are well below average, generally because of low available soil moisture. Yields are adjusted to a common percent of air-dry moisture content.

Range management requires knowledge of the kinds of soil and of the potential natural plant community. It also requires an evaluation of the present range similarity index and rangeland trend. Range similarity index is determined by comparing the present plant community with the potential natural plant community on a particular rangeland ecological site. The more closely the existing community resembles the potential community, the higher the range similarity index. Rangeland trend is defined as the direction of change in an existing plant community relative to the potential natural plant community. Further information about the range similarity index and rangeland trend is available in chapter 4 of the "National Range and Pasture Handbook," which is available in local offices of NRCS or on the Internet.

The objective in range management is to control grazing so that the plants growing on a site are about the same in kind and amount as the potential natural plant community for that site. Such management generally results in the optimum production of vegetation, control of undesirable brush species, conservation of water, and control of erosion. Sometimes, however, an area with a range similarity index somewhat below the potential meets grazing needs, provides wildlife habitat, and protects soil and water resources.

Reference:
United States Department of Agriculture, Natural Resources Conservation Service. National range and pasture handbook. (http://www.nrcs.usda.gov/technical/range.html)


