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<br /> <br />. <br /> <br />. <br /> <br />Major obstructions to the natural drainage of the <br />watershed include Interstate Highway 70, the Highline <br />Canal and the Grand Valley Canal. These structures cross <br />the watershed in an east-west direction. <br /> <br />. <br /> <br />The Indian Wash watershed can be divided into two <br />distinct sub-basins. The major sub-basin which is <br />drained by Indian Wash includes the entire watershed <br />above the Highline Canal and approximately 60 percent of <br />the watershed south of the canal. The Highline Canal <br />acts as an obstruction to the drainage and intercepts the <br />runoff from 3.4 square miles of the watershed which it <br />diverts to Indian Wash. The second sub-basin is located <br />to the south of the Hi ghl i ne Cana 1 and to the eas t of <br />Indian Wash. The sub-basin is drained by an unnamed <br />channel tributary arbitrarily called the 29~ Road Channel <br />for identification in this report. The 29~ Road Channel <br />flows southerly from the Highline Canal to the Denver and <br />Rio Grande Western Railroad (D&RGW) tracks where it turns <br />southwestward to its confluence with Indian Wash just <br />upstream of the D&RGW bridge. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />The total watershed drainage area at the D&RGW bridge is <br />approximately 15.3 square miles. Of this area, 69 <br />percent or 10.5 square miles lies above the Highline <br />Canal. The area above the lW-l retention dam measures <br />6.2 square miles or 41 percent of the total watershed <br />area. The contributing area of the 29~ Road Channel at <br />the mouth is approximately 1.9 square miles or 12 percent <br />of the total area. <br /> <br />The slope of Indian Wash north of <br />averages 2.5 percent and the slope <br />canal averages 0.5 percent. <br /> <br />the Highline Canal <br />downstream of the <br /> <br />The soils of the study area are composed primarily of <br />materials from the Mancos Shale and a Mesaverde <br />sandstone. These soils are characteristic of soils in <br />desert to semi-arid regions. <br /> <br />. <br /> <br />Vegetation in the watershed is sparse, consisting of <br />greasewood, a salt-to levant shrub; salt brush, and sage <br />brush in the foothills, and pinon-juniper and hardy <br />grasses at the higher elevations. The primary land use <br />for the watershed is rangeland, but a significant amount <br />of the land below Interstate 70 is irrigated (Reference <br />1) . <br /> <br />. <br /> <br />4 <br /> <br />. <br />