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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I I <br />I <br /> <br />STUDY AREA DESCRIPTION <br /> <br />Drainage Basin Description <br /> <br />The study area is divided into two drainage basins - Four-Mile Creek and <br /> <br />Mud Gulch. The Four-Mile Creek drainage basin encompasses 434 square miles and <br /> <br />drains portions of Park and Teller Counties in addition to Fremont County <br /> <br />(Figure 1). Most of the tributary area covers woodland and rangeland in fair to poor <br /> <br />conditions, including parts of the Pike National Forest and Mueller State Park. Also <br /> <br />included in this basin are small pockets of development; such as Cripple Creek and <br /> <br />subdivision developments in Canon City. <br /> <br />The Mud Gulch drainage basin contains only 3.61 square miles and borders <br /> <br />the southern portion of Four-Mile Creek basin. It contains mostly agricultural and <br /> <br />range land in fair to poor conditions. It extends into the northern foothills, where <br /> <br />there exists a flood control dam constructed by the RC & D. <br /> <br />The soils in the Four-Mile Creek and Mud Gulch basins can be described in <br /> <br />two categories: <br /> <br />1. Sojis on the Plajns make up 11 percent of Fremont County. They are lewl <br /> <br />and steep. Elevation is 5,000 to 6,000 feet, and average annual <br /> <br />precipitation is 12 inches. These soils are mostly of hydrologic soil complex <br /> <br />Group D, \dth some Band C. They are shaIlO\\' to deep and are well <br /> <br />drained. Thev formed in allmium derived mainlv from shale, limestone, <br />. . <br /> <br />and eolian sands and silt; and in residuum derived mainly from shale and <br /> <br />limestone. The soils are used mainly for irrigated crops, hay and pasture, <br /> <br />or orchards. They are also used as rangeland. <br /> <br />6 <br />