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<br />inches thick. The upper 9 inches of the subsoil is very dark grayish brown <br />heavy silty clay loam. The lower 14 inches is grayish brown silty clay <br />loam. The substratum to a depth of 60 inches or more is light brownish <br />clay loam. Permeability is slow. Available water capacity is high. <br />Runoff is medium and the hazard of water erosion is high. Included with <br />this map unit is about 10 percent Ruko clay, 10 percent Echo clay loam, and <br />S percent Hesperus loam. <br />(DO-CE) Paeosa cobbly loam. 3 to 25 percent sloaes. <br />The Pagosa cobbly loam occurs on mountainsides and formed in alluvium <br />and colluvium derived dominately from mixed sources. It is deep and well <br />drained. <br />Typically the surface is covered with a mat of leaves, needles and <br />twigs about 2 inches thick. The surface layer is dark brown loam about 3 <br />inches thick. The subsurface layer is light gray cobble sandy loam about <br />11 inches thick. The upper 23 inches of the subsoil is light yellowish <br />brown cobbly clay loam. The lower 11 inches is pale brown cobbly clay <br />loam. The substratum to a depth of 60 inches or more is pale brown cobbly <br />clay loam. Permeability is slow. Available water capacity is high. <br />Runoff is medium and the hazard of water erosion is moderate. Included <br />with this map unit is about 10 percent Frisco cobbly loam and 5 percent <br />Marapos silty clay loam. <br />-18- <br />