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2005-01-18_REVISION - M1978314 (2)
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2005-01-18_REVISION - M1978314 (2)
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Entry Properties
Last modified
6/15/2021 6:08:10 PM
Creation date
11/21/2007 9:04:40 PM
Metadata
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Template:
DRMS Permit Index
Permit No
M1978314
IBM Index Class Name
Revision
Doc Date
1/18/2005
Doc Name
Response to Adequacy Review
From
Banks and Gesso LLC
To
DMG
Type & Sequence
CN1
Media Type
D
Archive
No
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04038 Banks and Gesso, LLC <br />Cryoborolls-Cryorthents Clays are found on 6-65% slopes (hills and benches at slopes <br />from 6-25% and hills and mountain slopes for slopes of 25-65%) and are in the land <br />capability classification of Vle, nonirrigated, Vlls, nonirrigated and Vlle, nonirrigated at <br />higher slopes. In Cryoborolls soils, the surface layer is 0 to 2 inches consisting of mat of <br />needles, twigs and leaves, and dark brown clay loam from 2 to 7 inches. The <br />subsurface horizon from 7 to 22 inches is dark brown clay. The subsoil is grayish brown <br />clay found at 22 to 39 inches below the surface. The substratum is light brownish gray <br />clay from 39 to 60 inches. This soil is well drained and moderately deep to very deep at <br />greater slopes. The permeability is very slow and available water capacity is low to high <br />at greater slopes. The potential rooting depth is 20 to 60 or more inches and runoff is <br />very high. The hazard of water erosion is very high while the hazard of soil blowing is <br />moderate at lower slopes. In Cryorthents soils, the surface layer consists of 0 to 4 <br />inches of grayish brown clay. The substratum is light brownish gray clay from 4 to 13 <br />inches or 4 to 18 inches for greater slopes. The bedrock is soft, platy, calcareous shale <br />bedrock at 13 inches or at 18 inches for greater slopes. This soil is very shallow to <br />moderately deep and is somewhat excessively to well drained. The permeability is very <br />slow and available water capacity is low. The potential rooting depth is 4 to 40 inches <br />for lower slopes and less than 10 to 40 inches for greater slopes and runoff is very high. <br />The hazard of water erosion is very high. The major current uses of these soils are <br />livestock grazing, wildlife habitat and recreation. <br />Fourmile-Tellura Complex soils are found on 1-8% slopes (mesa and plateau tops) and <br />are in the land capability classification Vlc, nonirrigated. In Fourmile soils, the surface <br />layer is dark grayish brown loam from 0 to 5 inches. The subsurface layer is grayish <br />brown loam from 5 to 10 inches. The subsoil consists of brown very cobbly clay loam <br />from 10 to 23 inches and yellowish brown very cobbly clay loam from 23 to 35 inches. <br />The substratum is brown extremely cobbly loamy coarse sand from 35 to 60 inches. <br />This soil is very deep and well drained. The permeability is moderate and available <br />water capacity is medium. The potential rooting depth is 60 or more inches and runoff is <br />slow to medium. The hazard of water erosion is slight to moderate and the hazard of <br />soil blowing is slight. In Tellura soils, the surface layer is 0 to 4 inches of dark brown <br />cobbly loam. The subsurface layer is brown cobbly loam from 4 to 8 inches. The <br />subsoil consists of brown very cobbly sandy clay from 8 to 32 inches and brown <br />extremely cobbly sandy clay loam from 32 to 51 inches. The substratum is brown <br />King Mountain Sand & Gravel Mine Page 2 of 4 <br />King Mountain Gravel, LLC January 14, 2005 <br />
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