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1 <br /> EXHIBIT D <br /> SOILS <br /> Stocks Clay Mine <br /> `~„~a <br />' <br />~ <br />' <br /> San Isabel Stony Sandy Loam <br />d <br />^ <br />' 1 - 5% slope <br /> The soils in this area are stony sandy loans that are shallow over gra- <br /> vel and cobbles. The subsoil is moderately coarse textured. 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 />' Ruby Gravelly Sandy Loam <br /> 5 - 30% slope <br /> This soil series is very shallow to shallow very dark brown loans to <br /> clay loans. This is underlain by acid igneous, basalt, limestone or <br /> sandstone parent rock. It is usually neutral to acid in reaction. <br /> The permeability is moderate to the underlying parent rock. <br /> Also included in this is clayey valley soils, which are roderately <br /> deep, having developed on alluvial deposits, mostly from marine shale <br /> parent materials. Typically, a dark, clayey surface soil overlies a <br /> well-developed clay subsoil. Permeability is slow to very slow. <br /> <br />1 <br />L <br />IJ <br /> <br />1 <br /> <br /> <br />1 <br />