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<br />LAND <br /> <br /> <br />GO';_:'?!. <br /> <br />Soils <br /> <br />The general soil map locates soil with similar characteristics and <br />suitability within the basin, (see soils map and legend). Broad characteristics <br />and relationships can then be used to interpret the potential of soils for <br />agricultural, wildlife, recreational, commercial and industrial uses. Problems of <br />erosion, sediment yield, land use and future development are interrelated with <br />soils and their distribution. <br /> <br />The General Soils Map was prepared by delineating mapping units that differ <br />from each other in the kinds of soils that are present. Soils in each mapping <br />unit form patterns that are repeated from place to place. <br /> <br />Mapping units were defined and described according to requirements imposed by <br />the map scale and criteria from "Soil Taxonomy" published December 1975. The soil <br />map unit numbers in this report correspond to the soil map unit numbers of "Soils <br />of Colorado" published July 1977, by CSU Experiment Station - Bulletin 566S. <br /> <br />Assistance on the soils is available at the local Soil Conservation Service <br />offi ce. Pub 1 i shed Soi 1 Survey can al so be obtai ned at these offi ces. "Important <br />Farmlands" maps, which include prime land, are available for purchase through the <br />Bulletin Room 171, S.W. Wing Aylesworth Hall, Colorado State University, <br />Ft. Collins, Colorado 80523. Phone: (303) 491-6198. <br /> <br />Natural Basin Features <br /> <br />The Missouri River Tributaries, Colorado, contains all of the North and South <br />Platte Rivers and Republican River drainages in Colorado. Figure 1 shows the <br />location of the study area. The total area consists of 19,121,000 acres. <br />Elevations in the basin vary from high mountain peaks of 14,000 plus feet above <br />mean sea level and high mountain passes of 11,000 feet in the Rocky Mountains <br />through foothills, plains and river bottomlands to about 3,400 feet mean sea level <br />at Laird, Colorado. Two distinguishable major physical divisions characterize the <br />basin. <br /> <br />The Rocky Mountain System occupies approximately 25 percent of the basin. <br />The Southern Rocky Mountaln province occupies all of the Rocky Mountain System <br />while the High Plains province occupies all of the Interior Plains System. The <br />Southern Rocky Mountain province has extensive areas of coniferous forests and <br />intermingled mountain parks supporting mixed grasses and shrubs. There are a <br />number of intermountain valleys between the mountain masses. These areas are used <br />mainly for grazing. The Rocky Mountain portion of the basin is a primary source <br />of water for the North and South Platte Rivers. <br /> <br />The High Plains province slopes gently eastward from the Rocky Mountains. It <br />occupies approximately 75 percent of the basin. The plains are characterized by <br />nearly level to rolling tablelands, with hilly to rough broken areas along the <br />valley sides. Stream dissection is well established, with broad smooth divides <br />between the larger drainages. <br /> <br />B-1 <br />