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• accounts for inclusions end soil lose during selvage due to brush clearing. <br />%BF-Ninevsda•splitro Complex. Th1s map unit is located on the very steep bedrock <br />controlled sideslopes end ridges. All inclusions within this map unit have unsuitable <br />rock fragment contents at or Weer the surface. Na recoverable soil is available from this <br />map unit due to very steep slopes and excessive rock fragments (Addendum 8, Tab 9). <br />11C, 11D-Binco Silty Clay Loem. The Binco silty clay loam map units occur on the gently <br />sloping to moderately steep colluvial fans end residual sideslopes, benches, and <br />toeslopes. The soil profile is deep ri th a thin light colored surface horizon which <br />overlies a clay subsoil end substratum. Adjacent Aaberg soils have moderately deep <br />profiles. Buckskin soils have a dark colored surface horizon and subsoil clay <br />accumulation. <br />the recommended soil salvage thickness is based on [he thickness of the surface horizon <br />since subsurface clay levels are unsuitable. Soil salvage should be terminated near the <br />upper part of the Iambic (Bw) horizon. The mean in situ suitable soil thickness for 13 <br />profiles is 6 inches (Addendum 8, Tab 9). <br />• <br />The 11C and 11D map units consist of 90 percent Binco with 5 percent each of Aaberg and <br />Buckskin (Addendum 3, Tab 9). A 0.5-f oot mean salvage thickness was used for these map <br />units to calculate recoverable soil volumes listed in Table 1 and Exhibit 9-1. <br />12C and 12D-Buckskin Clay Loam. Buckskin clay loam soils occur on gently sloping to <br />moderately steep mountain sideslopes, benches, tans, small knolls, and ridgetops. The <br />soil profile is deep and yell developed with a dark Colored surface horizon and subsoil <br />clay accumulation. This soil has a thinner surface horizon than either Cochetopa or <br />Routt. Adjacent Aaberg end Binco profiles lack a mollic epipedon and argillic horizon. <br />The recommended soil salvage thickness is based solely on the thickness of the surface <br />mollic epipedon and adjacent, untlerlying transitional horizons. Soil salvage should <br />he terminated at the top of the argillic (Bt) horizon. The mean in situ suitable soil <br />thickness for 16 profiles is 9 inches (Addendum B, Tab 9). <br />_ The 12C end 120 map units consist of 75 percent Buckskin rith 10 percent Binco and 5 <br />• percent each of Buckskin variant, Aeber g, and Routt inclusions (Addendum 3, Tab 9). A <br />13 <br />