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<br />I h', O""'{ <br />...~>- '-~,.... ~ ('. :~ <br /> <br />C H A <br />GUNNISON <br /> <br />P T <br />R I <br /> <br />E R <br />V E <br /> <br />I I <br />R R <br /> <br />E G ION <br /> <br />! The Gunnison River rises among the high pea ks of the Sawatch <br /> Range and flows generally west for about 250 miles (402 km), <br />. joining the Colorado River near the city of Grand Junction (see <br /> figu re 2-1). The Gunnison and its tributaries drain parts of the <br /> Sawatch, West Elk, and San Juan Ranges, as well as the <br /> <br />Uncompahgre Plateau, <br />channel. The natural <br />Gunnison basin. <br /> <br />totaling some 3,000 miles (4,828 km) of <br />environment is extremely diverse within the <br /> <br />NATURAL ENVIRONMENT <br /> <br />The region described in the following text corresponds to the <br />Gunnison River basin located in southcentral Colorado. The basin <br />encompasses about 8,020 square miles (20,772 km2), or <br />approximately 8 percent of the entire state of Colorado. At its <br />greatest dimensions, the region is some 145 miies (233 km) across <br />from east to west and 95 miles (153 km) wide from north to south. <br /> <br />Physiography and Geology <br /> <br />" <br /> <br />The region ranges in elevation from approximately 4,550 feet <br />(1,387 m) at Grand Junction to about 14,300 feet (4,359 m) at <br />Uncompahgre Peak in northwest Hinsdale County. Mountain ranges <br />in the eastern part of the region are composed mostly of <br />Precambrian metamorphic and igneous rocks that have been uplifted, <br />except for the West Elk and Elk Mountains. <br /> <br />. <br /> <br />The West EI ks are <br />uplifted structures <br /> <br />composed of <br />that were <br /> <br />thick volcanic <br />formed by <br /> <br />piles and <br />Tertiary <br /> <br />several <br />igneous <br /> <br />7 <br />