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General Description of the Environment <br /> River, a third tributary to the Missouri River System, originates in the plains of <br /> eastern Colorado. Major tributaries of the Colorado River System also originating <br /> in Colorado include the San Juan, Dolores, Gunnison, White, and Yampa Rivers. <br /> The basins of these major streams are shown on exhibit 1.1. The distribution of <br /> the State's area (104,247 mi2) is shown by major drainage basins in table 2.1. <br /> Table 2.1--Drainage basins of Colorado <br /> River basin Square miles Percent of State <br /> Arkansas 28,297 27 <br /> Colorado 38,542 37 <br /> Missouri 29,877 29 <br /> Rio Grande 7, 531 7 <br /> State total 104,247 100 <br /> • <br /> GEOLOGY <br /> The Southern Rocky Mountain Province is a rugged zone of north-south <br /> trending mountain ranges which form a continuous belt across central Colorado. <br /> The typical mountains have cores of igneous and metamorphic rocks. They <br /> originated by repeated uplifts of igneous rocks through the sedimentary rocks <br /> that were once continuous across this mountainous region. The uplifted rocks <br /> have been modified through the ages by glaciation and other forces of erosion. <br /> Steeply dipping sedimentaries still flank the mountains and extend eastward <br /> under the Great Plains and westward under the Colorado Plateau. <br /> The repeated uplifts combined with erosion have removed nearly all <br /> evidence of the sedimentaries from the mountain province. Exceptions occur <br /> within the South, Middle, and North Parks and the San Luis Valley which are <br /> structural basins resulting from being inactive during the periods of uplift. <br /> Sedimentary rocks, mainly shale, sandstone, and siltstone, are found in the <br /> three parks while the San Luis Valley has been filled with alluvium (sand, gravel, <br /> and clay). <br /> • <br /> 2.2 <br />