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C <br />.• <br />i <br />S•~',s <br />Xz-'3 Baca-`1'•_lep Silt Loans G-~'=. S]o-e <br />• <br />These are deer, gently slopin~•, ••ell drained soils in tablelands and <br />=~^e :.ills. Races soils (about 4u!) have a loam surface abort 6 ir.cres thick <br />an9 a silt}• clay loam s_~b-soil about 1F, inches thick. •diley soils (abort 35;b) <br />h~•;e 3 silt loam surface about 4 inches thic-: and a moderately alkaline silty <br />c7=y loam about 14 inches thick. There are Kenerally ro gravels in t'-e <br />to- fire foot. <br />K1-Cr pages Gravelly Loam <br />The ton 3 to 6 inches is a moderately alkaline, gravelly loam. From <br />C~ <br />6 iad~es to 7u inches is a gravelly sandy loam over sand mixed with fine- <br />modium gravel. Gravel is l-reater than 1(T?o in parent material. <br />From 2 to 1G foot is a sand and eravel hiEhlp varible in depth. <br />T'~is material is over lime cemented sandstone highly weathered in places. <br />It arse=. r.=_. to he rinnaBle in places bait hard sandstone bedrock where thicY.. <br />T'~is sandstone overlays a yellowish and greenish colored shale. <br />The m=aerial nn the nor+h Slone of the eravel nit is dominately a <br />cia•: ~^am high in 7.~me ~•~ith =mall areas of sandy loam. There are occassiona7. <br />s^p'.s of deep sandy-grave7l? material. The nit bottom is covered with fine <br />gavel and sand under]a~n by =, limy-silt material in most areas. <br />\• <br />