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<br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />Mas'S'! .,. <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />B.Solls <br />Soi~ in the Uncompahgre Valley have been classified into <br />four primary types: 1) soils formed on and from shale of the <br />Mancos Formation, 2) soils formed on stream terrace de- <br />posits, 3) soils formed on and from sandstone of the Dakota <br />Formation, and 4) recent alluvial flood plain soils adjacent <br />to the Uncompahgre River. The first two soil types listed <br />above are the most important with respect to the proposed <br />hYdroelectric developments. Due to the semiarid climate of <br />the area, the soils have been formed under a sparse vegeta- <br /> <br />tive cover resulting in only moderate to low organic content. <br /> <br />These soils have not been leached to any great depths and, <br /> <br />therefore, retain much of the natural fertility and salinity <br /> <br />of the parent material. They are moderately calcareous and <br />1 <br />have slight to moderate profile development. <br /> <br />About thirty-four percent of the irrigated acreage in the <br />Uncompahgre Valley consists of soils formed on and from the <br />Mancos Formation, also known as adohe soils. The Mancos <br /> <br />Formation is a calcareous marine shale and is fractured and <br /> <br />jointed near the surface. During the weathering process, <br /> <br /> <br />salts in the shale are dissolved and redeposited in the <br /> <br /> <br />joints and bedding planes of the weathered shale. Most of <br /> <br />E-6 <br />