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surface layer is reddish brown fine sandy loam about 8 inches thick. The underlying material is reddish brown and light reddish brown loam about 28 inches thick over yellowish red stratified loam and sandy loam. Permeability is moderate and the available water capacity is high. The Barnum series consists of deep, well drained soils that formed in alluvium from reddish colored shale and sandstone. The surface layer is typically brown loam about 10 inches thick. The underlying material is reddish brown lam stratified with thin layers of sandy loam and is about 50 inches thick. Permeability is moderate and the available water capacity is high. Connerton-Bamum complex reportedly occurs along the North Poudre Supply Canal adjacent to the western boundary of the proposed permit area. It also reportedly ars along US Highway 287 east of the mine site. mer fine sandy loam, 1 to 9% slopes -This nearly level to strongly sloping soil is on uplands and ridges. It consists of shallow, well drained soils that formed in material athered from reddish brown sandstone. These soils are on uplands and aze underlain sandstone at a depth of 10 to 20 inches. Typically, the surface layer is reddish brown e sandy loam about 7 inches thick. The underlying material is light reddish brown fine idy loam about 7 inches thick. Below this is hard reddish brown sandstone. Yneability is moderate and the auailable water capacity is low. These soils reportedly ;ur southwest of the proposed permit area. ner-Rock outcrop complex, 10 to 50% slopes -This complex consists of moderately 'p or steep oils on uplands and ridges. It is about 55%Purner fine sandy loam and ut 30% rock outcrop. Purner fine sandy loam is smoother and less sloping. A small i of this soil reported occurs between the southern end of the proposed permit area and Highway 287. Atypical profile of this Purner soil is described in the preceding Purner complex, 5 to 20% slopes -This complex consists of strongly sloping to ately steep soils on upland and valley sides. It is about 45% Kirtley loam and 40%Purner fine sandy loam. Kirtley loam is smoother and less sloping, and the is steeper. The Purner soil is described in the preceding paragraphs. The Kirtley loam consists of moderately steep, well drained soils that formed in material weathered from reddish brown sandstone and shale. These soils are on uplands and side slopes and are underlain by so$ shale at a depth of 24 to 40 inches. Typically, the surface layer is reddish brown loam about 4 inches thick. The subsoil is reddish brown heavy loam about 14 inches thick. Permeability is moderate and the available water capacity is medium. This soil complex reportedly occurs adjacent to the northwest portion of the proposed permit area. ~~