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<br />Characteristic vegetation in the Rangely area is determined by <br />moisture, exposure, temperature, and elevation. In the immediate <br />environs, which are best defineq as desert rangeland, the vegeta- <br />tion includes saltbush, shadscale, bud sage, and hardy grasses. <br />In the foothill regions, cover is predominantly comprised of big <br />sagebrush with an understory of 'grasses. Aspen, spruce, and fir <br />are characteristic further up-slope, and arctic varieties of willow, <br />sedge, and clover are found above timberline. <br /> <br />In general, the drainage pattern of Rangely is from southeast to <br />northwest. The White River flows westward on a meandering course <br />just north of Rangely. The dra~nage basin of College Canyon Draw, <br />also known as Dragon Wash, is s6uth of the town. The stream enters <br />the town along its southern corporate limits, flowing west and <br />northwest to join the White River. The drainage basin of Coal <br />Mine Draw is also south of town ,and is situated directly to the <br />west of the College Canyon Draw drainage basin. The stream enters <br />the town in the western half of its southern corporate limits, <br />then flows west and northwest tq its confluence with the White <br />River. <br /> <br />Rangely rests on a bedrock form~tion of Mancos Shale of the Upper <br />Cretaceous age. This layer is ~ore than 5,000 feet thick, and is <br />essentially a dark grey, calcareous, marine deposit that weathers <br />light grey to yellow brown. Se~enite gypsum is common throughout <br />the formation. The soils of this area have formed under a low- <br />effective annual precipitation. ' Soil-parent materials are mainly <br />calcareous, clayey shales and s4ndstones/ however, sandy and <br />gravelly outwash, windblown sands and silts, and alluvial sedi- <br />ments are also extensive. Surf~oe soils are light colored and <br />range in texture from sandy loam to silty clay. Subsoils are <br />principally clay loam or clay in texture, and have a permeability <br />rate that varies from moderate to slow. Sandy subsoils with a <br />high permeability rate are a minor component within the area. <br /> <br />Tourism is of little significance to the town, even though Dinosaur <br />National Park is only 30 miles to the north. Available lodging in <br />Rangely is limited to that requ~red for oilfield workers. However, <br />the town is growing. Based on ~970 and 1980 Bureau of Census <br />population figures of 1,591 andi2,113, respectively, Rangely <br />experienced a 33-percent popula~ion growth in ten years. Today, <br />Rangely has a population of app~oximately 2,500, according to a <br />survey conducted by the Town of'Rangely Department of Community <br />Development. <br /> <br />Oil has been the lifeblood of tqe town, but cattle and sheep ranch- <br />ing is also considered important to the economy of this rural <br />community. The town is lookinglforward to further coal and oil <br />development. Other natural res~urces in the Rangely area include <br />rare earths, copper, silver, go~d, thorium, aluminum, low-grade <br /> <br />4 <br />