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PERMFILE107997
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PERMFILE107997
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Entry Properties
Last modified
8/24/2016 10:00:28 PM
Creation date
11/24/2007 4:07:20 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981019
IBM Index Class Name
Permit File
Doc Date
5/4/2007
Doc Name
Narrative Descriptions of NRCS Soil Map Units South Taylor/Lower Wilson Permit Expansion Area
Section_Exhibit Name
Exhibit 09 Item 5 -ST
Media Type
D
Archive
No
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I • Permeability of this Cochetopa soil is slow. Available water holding capacity is high. Effective <br />rooting depth is 60 inches or more. Runoff is slow, and the hazard of water erosion is moderate. <br />The hazard of soil blowing is slight. <br />This unit is used for livestock grazing and wildlife habitat <br />52 -Danavore-Waybe complex, 5-30% slopes <br />This unit is on narrow ridge crests and mountain sides. Elevation is 7,200 to 8,600 feet. The <br />average annual precipitation is 18 to 20 inches, the average annual air temperature is 37 to 40 <br />degrees F., and the average frost-free period is 50 to 75 days. <br />This unit is 45 percent Danavore soil and 30 percent Waybe soil. Included in this unit are small <br />areas of rock outcrop, and soils similaz to the Danavore soil but have dazk colored surface layers. <br />The Danavore soil is moderately deep and well drained. It formed in residuum derived from <br />interbedded sandstone and shale. Typically the surface layer is light yellowish brown very <br />cobbly sand loam and is 4 inches thick. The upper 4 inches of the underlying material is <br />yellowish brown extremely stony sandy loam. The next 9 inches is light yellowish brown <br />extremely channery loam. The lower part to a depth of 22 or more inches is very pale brown <br />calcareous extremely channery clay loam. Weakly consolidated sandstone bedrock is at a depth of <br />22 inches. Depth to weakly. consolidated sandstone bedrock ranges from 20 to 40 inches. <br />Permeability of the Danavore soil is moderately slow. Available water holding capacity is very <br />• low. Effective rooting depth is 20 to 40 inches. Runoff is rapid, and the hazazd of water erosion <br />is moderate. The hazard of soil blowing is slight. <br />The Waybe soil is shallow and well drained. It formed in residuum derived from shale. <br />Typically, the surface layer is light gray calcareous channery silty clay loam 4 inches thick. The <br />underlying material to a depth of 15 inches is pale yellow calcareous silty clay loam. Weakly <br />consolidated shale bedrock is at a depth of 15 inches. Depth to weakly consolidated bedrock <br />ranges from ] 0 to 20 inches. <br />Permeability of the Waybe soil is slow. Available water holding capacity is very low. Effective <br />rooting depth is 10 to 20 inches. Runoff is rapid, and the hazard of water erosion is high. The <br />hazard of soil blowing is slight. <br />This unit is used for livestock grazing and wildlife habitat. <br />66 - Evanot loam,1-12% slopes <br />This very deep, well drained soil is on benches and hillslopes. It formed in loess. Elevation is <br />6,200 to 7,200 feet. The average annual precipitation is 13 to ]5 inches, the average annual air <br />temperature is 42 to 45 degrees F., and the average frost-free period is 75 to 95 days. <br />Typically, the surface layer is brown loam 8 inches thick. The upper 12 inches of the subsoil is <br />yellowish brown clay loam. The next 13 inches is very pale brown calcareous clay loam. The <br />lower part to a depth of 60 or more inches is light yellowish brown calcareous loam. <br />• Included in this unit are small areas of Forelle soils. <br />
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