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• Permeability of the Pinon soil is moderate. Available water capacity <br /> is very low. Effective rooting depth is ten to twenty inches. Runoff <br /> is moderate, and the hazard of water erosion is high. <br /> The Bowdish soil is moderately deep and well-drained. It formed <br /> in residuum derived dominantly from interbedded sandstone and shale. <br /> Typically, the surface layer is reddish brown loam five inches thick. <br /> The upper part of the subsoil is reddish brown loam seven inches thick. <br /> The lower part is pinkish white gravelly loam eleven inches thick, . <br /> Hard sandstone is at 23 inches. In some areas, the surface layer is <br /> fine sandy loam or sandy loam. <br /> Permeability of the Bowdish soil is moderate. Available water capacity <br /> is low. Effective rooting depth is 20 to 40 inches. Runoff is moderate <br /> • and the hazard of water erosion is high. <br /> The Progresso soil is moderately deep and well-drained. It formed <br /> in alluvium derived dominantly from sandstone. Typically, the surface <br /> layer is reddish brown loam seven inches thick. The subsoil is reddish <br /> brown clay loam seventeen inches thick. The substream is white sandy <br /> loam twelve inches thick. Hard sandstone is at a depth of 36 inches. <br /> In some areas, the surface layer is fine sandy loam. <br /> Permeability of the Progresso soil is moderately slow. Available <br /> water capacity is low. Effective rooting depth is 20 to 40 inches. <br /> Runoff is moderate and the hazard of water erosion is high. <br /> This unit is used for livestock grazing and wildlife habitat. <br /> • -16- <br />