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<br /> make up from about 15 to 35 percent of the soil material. Representative <br /> profiles of the Schofield and Peeler gravelly sandy looms, 25 to 60 percent <br />' slo <br />es <br />are incl <br />ded herein <br /> p <br />, <br />, <br />u <br /> The Matcher series are sandy-skeletal, mixed Typic Cryumbrepts and <br /> consist of well drained, sloping to very steep soils that formed in <br /> granitic glacial moraines under a lodgepole pine vegetation cover. The <br /> mean annual precipitation is about 20 inches, and the mean annual soil <br />' temperature is about 36°F. Permeability is rapid and available water <br />' capacity is low. Forest litter is typically about three inches thick over <br /> approximately a nine inch thick grayish brown stony sandy loam surface <br />t soil. The subsoil is a stony sandy loam. A representative profile of the <br /> Matcher stony sandy loam, five to 25 percent slopes, is included herein. <br />' Histosols occupy concave sites and relatively level areas along major <br /> streams. In the subject area they form a narrow band immediately adjacent <br />' <br /> to Gold Creek towards the southerly side of the permit area. This type of <br />' soil is composed of fiberous, relatively undecomposed material (twigs, <br /> grasses, roots) ranging from about three to 16 inches thick overlying <br /> material which ranges from silty clay to mixed sand, gravel and cobbles. <br /> Typically runoff is slow and the potential for water erosion is slight. <br /> <br />1 <br /> <br />1 <br />1 <br /> <br />' -4- <br />