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• sandy clay loam. Groundwater is at a depth of 13 to 26 inches. The <br />Torrifluvents are not recommended for lift 1 material because they <br />lack a mollic epidedon. They are suitable for lift 2 material to a <br />depth of 6U inches or snore. A groundwater table may be encountered <br />and the so it snag be difficult to salvage due to wetness. <br />This soil occurs in map unit TA. It was sampled in typical pedon <br />number 6 and in composite sample numbers 236/270. Average lift 1 <br />thickness is U inches, average lift 2 thickness is 6U+ inches, for an <br />average total salvagable thickness for the series of 6U+ inches. <br />2.1.15 Torriorthents <br />Tnis soil is a shallow to deep, well drained, slowly to rapidly <br />permeable soil formed in colluvium derived from sandstone and' shale. <br />It occurs on south facing mountain sideslopes on slopes of 2U to 7U <br />percent. The native vegetation is bunchyrasses and sage. The <br />available water holding capacity is low to moderate. <br />In a typical profile, the surface layer is brown to dark brown,. <br />channery loam about 5 inches thick. The subsoil is light brownish <br />gray to olive brown, very channery clay about 44 inches thick: The <br />substratum is gray, weathered calcareous shale. Uepths to bedrock <br />range from 3 inches to over 60 inches, but most are lU to 60 inches. <br />The soil is mostly within the loamy-skeletal and clayey-skeletal, <br />mixed families of Lithic and Ustic Torriorthents. <br />The Torriorthents are quite variable. The surface layer of the <br />Torriorthents are suitable for lift 2 material, but the subsoils are <br />unsuitable due to excessive channery. <br />This soil occurs in map unit TRD. It was sampled in typical <br />pedon number 27 and in composite sample numbers 201/231 Average <br />lift 1 thickness is U inches, average lift 2 thickness is 14 inches, <br />for an average total salvagable thickness for the soil 14 inches. <br />2.1.16 Vandamore Var. Flaygy Sandy Loam <br />This soil is a moderately deep, well drained, moderately <br />permeable soil formed in residuum derived from sandstone and shale. <br />It occurs on narrow upland ridgecrests and mountain sideslopes on <br />slopes of 5 to 55 percent. The native vegetation is big sage, <br />serviceberry and mountain shrubs. The available water holding <br />capacity is moderate to low. <br />In a typical profile, the surface layer is very dark grayish <br />brown to dark yellowish brown, flaggy sandy loam or sandy clay loam <br />about 6 inches thick. The substratum is yellowish brown, cobbly clay <br />to very cobbly loam about 18 inches thicK. Depth to bedrock is 2U to <br />4U inches. The series is in the loamy-skeletal, mixed (calcareous) <br />family of Typic Cryorthents. <br />Depth to bedrock averages 2U inches. The profile is generally <br />calcareous throughout. Surface cover is about 2U percent flagstones. <br />15 <br />