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<br />' EXHIBIT D <br /> SOILS <br /> 8 Mile Clay Mine <br /> San Isabel Stony Sandy Loam <br /> 1 - 5~ slope <br /> The soils in this area are stony sandy loams that are shallow over gra- <br /> vel and cobbles. The subsoil is moderately coarse te xtured. Large <br /> round boulders are numerous with many of them nearly buried. Permea- <br /> bility of this soil is rapid, and the available water capacity is low. <br /> Samsil Clay Loam <br /> 0 - 3Y slope <br /> The Samsil series is made up of shallow, well-drained soils formed on <br /> upland hills and ridges in clayey residuum weathered from shale. The <br /> surface horizon is strongly calcareous, light brownis h-gray clay about <br /> 3 inches thick. The subsoil, about 9 inches thick, i s strongly calcar- <br />' eous, light yellowish-brown clay. Underlying this is strongly calcar- <br /> eous shale. The permeability is slow, the runoff is rapid, and the <br /> erosion hazard is high. <br />LJ <br />C <br /> <br />1 <br />fl <br /> <br /> <br /> <br /> <br /> <br />