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1 <br />' E:(HIBIT D <br /> <br />' SOILS <br /> Siloam Clay f4ine <br />t <br /> Pe-Be Penrose f4innequa-Complex <br /> <br />' 25-65% Slopes <br /> pH: 7,9-8.4 <br /> Permeability: .6-2.0 in/hr <br />' <br /> Penrose soils are shallow slopin g, excessively drained stony and rocky soils. <br /> They are found in the plains are a, formed from limestone parent materials. The <br />t surface horizon is a thin stony loam only a few inches thick. The subsoil horizon <br /> continues to a depth of about 12 inches and is similar in composition to the surface, <br /> but is considerably more stony. The substratum begins at a depth of 20 inches <br />' and consists of hard limestone. <br />' M2-C 4lormser Silt Loam <br />1-5Y Slopes <br />' pH: 6.6-8.4 <br />Permeability .2-2.0 in/hr <br />Wormser soils are moderately deep, moderately well drained soils of the foothills <br />t zone. The surface horizon consists of loam or silt loam and is about 6 inches <br />thick. The subsoil, about 36 inches in depth, is mostly clay loam. At this point <br />the substratum begins which is a sandstone bedrock. The permeability of this soil <br />' type is moderately slow. <br />' M4-E Strouoe Extremely Stony Loam <br />9-25b Slopes <br />pH: 7,4-7.8 <br />Permeability: .2-Z.0 in/hr <br />Stroupe soils are shallow, stony and rocky, well drained, and of an undulating <br />' nature. They are situated in the foothills of the area, and were formed in clayey <br />parent materials derived from sandstone. The surface horizon, about 5 inches <br />thick, is brown stony loam. The subsoil horizon, to about 16 inches, consists <br />of a reddish bro~,vn stony clay loam. Fractured sandstone bedrock comprises the sub- <br />stratum, beginning at about 16 inches. <br />1 <br /> <br />1 <br />