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<br />In the 1974 legislative session, the Colorado General Assembly directly <br /> <br />Located in the west central part of Chaffee County, Cottonwood Creek <br /> <br />drains about 105 square miles. Cottonwood Creek flows in a general <br /> <br />attacked the flood-plain problem by describing it as a natural hazard of <br /> <br />Colorado Revised Statutes 1973, authorizes the Colorado Water Conservation <br /> <br />eastward direction and is fed by three drainages: North Cottonwood, <br /> <br /> <br />Middle Cottonwood, and South Cottonwood Creeks. North Cottonwood drains <br /> <br /> <br />26 square miles and enters the flood plain study area approximately 1.7 <br /> <br /> <br />miles east of the upper study limit. The combined drainage area of <br /> <br /> <br />Middle and South Cottonwood Creeks is about 65 square miles, They join <br /> <br /> <br />to form Cottonwood Creek about 2.9 miles west of the-North Cottonwood <br /> <br />State interest relating to the use of land in House Bill 1041 (Title 24, <br /> <br />Articles 65.1, 32 and 65 CRS 1973, as amended). Section 37-60-l06(1)(c), <br /> <br />Board to designate and approve storm flood-water runoff channels and to <br /> <br />make such designations available to legislative bodies of local juris- <br /> <br />dictions. The Board is providing assistance to local governments in <br /> <br />the development and adoption of effective flood plain ordinances. In <br /> <br />Creek confluence. About 14 square miles of intervening drainages makes <br /> <br /> <br />up the balance of the 105 square miles above the confluence with the <br /> <br />addition, the Board assists and provides financial assistance to flood <br /> <br />plain information studies in Colorado. <br /> <br />Arkansas River. The confluence of Cottonwood Creek with the Arkansas <br /> <br />Requests by Chaffee County and the town of Buena Vista to conduct flood <br /> <br />River lies in a narrow entrenched canyon at the lower study limit. <br /> <br />Effects of potential flooding on the- Arkansas River are not included in <br /> <br />hazard -studies are in accordance with State Legislature House Bill 1041 <br /> <br />this study. A map showing the location of the study area follows page <br /> <br />which requires local governments to identify and designate areas, such <br /> <br />6. <br /> <br />as flood plains, that are of state interest. <br /> <br />DESCRIPTION OF THE STUDY AREA <br /> <br />The upstream drainage area originates in the Sawatch Range of the Rocky <br /> <br />Mountains at the top of the Continental Divide between the Arkansas and <br /> <br />The area of study includes the Cottonwood Creek flood plains in the <br />I <br />vicinity of the town of Buena Vista. The study area is located within <br /> <br />Gunnison River Basins, Elevations vary from more than 13,000 feet along <br /> <br /> <br />the divide to 7,900 feet (mean sea level elevations) at the lower end of <br /> <br />Hydrologic Unit Code Number 11020001. The study begins at the confluence <br /> <br />the study area. Geology in the upper reaches consists of metamorphic <br /> <br /> <br />rock (crystalline), mostly granite and other igneous type rocks. Soils <br /> <br /> <br />are deep to moderately deep with rock outcrops; and the permeability <br /> <br />of Cottonwood Creek with the Arkansas River and extends upstream through <br /> <br />Buena Vista approximately six miles to the San Isabel National Forest <br /> <br />characteristics are moderate to moderately rapid. Ground cover consists <br /> <br />of native grass, brush, and forestland. Cottonwood, pinon-juniper, and <br /> <br />Boundary. The Arkansas River is a major tributary to the Arkansas- <br /> <br />White-Red Water Resources Council Region, <br /> <br />pine trees grow at the lower elevations. Topography has a significant <br /> <br />effect on the semi-arid climate. <br /> <br />Average annual precipitation varies <br /> <br />3 <br /> <br />4 <br />