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<br />Cottonwood Creek, an east bank tributary of Monument Creek, <br />originates near Black Forest north of Colorado Springs. It flows <br />southwesterly through northern Colorado Springs, passes under the <br />Atchison, Topeka, and Santa Fe Railway and Interstate Highway 25, and <br />joins Monument Creek. The stream along most of its course is deeply <br />eroded into rock outcroppings and in the lower reach is lined with <br />willows. Within Colorado Springs, Cottonwood Creek flows in a sand- <br />bottom, riprap-sided channel. <br /> <br />Douglas Creek (North and South) drains an area in and adjacent to <br />northwestern Colorado Springs. The stream flows southeasterly for <br />approximately 8 miles to join Monument Creek near the Templeton Gap <br />Floodway outlet. Lower portions of Douglas Creeks North and South <br />have been channelized into concrete-lined drainage structures. <br /> <br />Dry Creek, <br />Valley Dry <br />Basin. <br /> <br />North Channel <br />Creek, and Big <br /> <br />Dry Creek, North Fork Dry Creek, South <br />Valley, collectively, drain the Dry Creek <br /> <br />, <br /> <br />The Dry Creek Basin is bounded on the west by the Front Range of the <br />Rocky Mountains, on the south and north by ridges, and on the east by <br />Monument Creek. It slopes from west to east toward Monument Creek, <br />rising from an elevation of 6,250 feet to elevation 9,250 feet. The <br />western portion of the basin is heavily forested, mountainous <br />terrain, drained by three major tributaries of Dry Creek. These <br />tributaries are steep, well defined ravines which come to a <br />confluence west of the Sisters of Mount Saint Francis Convent. The <br />central portion of the basin is characterized by gently rolling wide <br />valleys, separated by foothill ridges and mesas. Through the central <br />portion of the basin, Dry Creek is poorly defined and flows through <br />broad, gently sloping meadows. The eastern portion of the basin is <br />fully developed, and Dry Creek flows through well de"ned and eroded <br />channels as well as greenbelt areas (Reference 2). Dry Creek has <br />been channelized from approximately 1,500 feet downstream of Dairy <br />Ranch Road to a point approximately 500 feet upstream of Dancing <br />Horse Road. For the most part, flow in Dry Creek and its tributaries <br />is intermittent. <br /> <br />Kettle Creek, a left-bank tributary to Monument Creek, originates on <br />the western slope of the Black Forest, northeast of Colorado Springs. <br />A 2-mile segment of the lower reach is within U.S. Air Force Academy <br />boundaries. The basin is subject to urban development. Typically, <br />the creek cuts a narrow, deep canyon. Its drainage area encompasses <br />approximately 17 square miles. <br /> <br />Mesa Basin is located in western Colorado Springs. It is bounded on <br />the north by Garden of the Gods Road, on the west by Mesa Road, on <br />the south by Unitah Street, and on the east by Monument Creek. The <br />main channel in this basin drains the western portion of the basin. <br />It flows southeasterly through the basin, passes under Interstate <br />Highway 25 between Caramillo and Buena Ventura Streets, and joins <br />Monument Creek. <br /> <br />5 <br />