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Fish Creek Soil Investigation <br />size control section. Lotex soils have hue of SYR or redder. Spliten and Udelope soils receive <br />most of their moisture in the winter and eazly spring. Taylow soils have a xeric moisture regime. <br />Tuggle soils have a pazalithic contact above the lithic contact. <br />GEOGRAPHIC SETTING: Splitro soils are on upland hillslopes, mountain slopes, structural <br />benches and ridges. Slope gradients range from 0 to 65 percent. These soils formed in medium <br />textured alluvium, residuum, and eolian materials derived dominantly from sandstone. In <br />Colorado some azeas are derived from basalt. Precipitation is 18 to 25 inches, with peak periods <br />of precipitation occumng in the spring and early summer. Mean annual temperature is 36 to 40 <br />degrees F. Elevation is 6,500 to 9,200 feet. The frost-free season is 60 to 90 days. <br />GEOGRAPHICALLY ASSOCIATED SOILS: These aze the Passcreek and Sawcreek soils. <br />Both of these soils aze moderately deep and occur on lowland hillslope positions and broad <br />summits. <br />DRAINAGE AND PERMEABILITY: Well drained; slow to rapid runoff; moderate to rapid <br />permeability. <br />USE AND VEGETATION: These soils aze used principally as native pastureland or for <br />recreational purposes. Native vegetation is green needlegrass,Idaho fescue, and yarrow. May <br />have scattered ponderosa pine and quaking aspen. <br />DISTRIBUTION AND EXTENT: The Bighorn Mountain areas ofnorth-central Wyoming and <br />the western slope of Colorado. The series is of moderate extent. <br />MLRA OFFICE RESPONSIBLE: Bozeman, Montana <br />SERIES ESTABLISHED: Lower Colorado Area, Colorado 1970. <br />REMARKS: Diagnostic horizons and features recognized in this pedon are: <br />mollic epipedon - 0 to 8 inches (A) <br />Iambic horizon - 8 to 16 inches (Bw) <br />lithic contact -16 inches (R) <br />MLRR- E <br />SIR- WY0062, WY0845, WY1390 <br />National Cooperative Soil Survey <br />U.S.A. <br /> <br />Habitat Management, Inc. A3-14 01/06/04 <br />