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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 <br />I <br /> <br />2.0 <br /> <br />2.1 <br /> <br />2.2 <br /> <br />QTUDY AREA DESCRIPTION <br /> <br />Location <br /> <br />This rePort addresses the drainage basins of Rangeview Gulch, Jackass Gulch, <br />LDwer Dad Clark Gulch (downstream of McLellan Reservoir), and the direct flow <br />areas to the South Platte River located between the gulches. <br /> <br />1. Santa Fe Drive, the Denver & Rio Grande Western Railroad (D&RGW), <br />and the Atchison, Topeka and Santa Fe Railroad (AT&SF): These <br />features are located adjacent to each other and run north and south <br />through the study area. These features greatly influence the natural <br />westerly drainage patterns. <br /> <br /> <br />E~~~water <br /> <br />FAl( IN <br /> <br />The study area is located almost entirely within the limits of the City of Littleton. <br />It lies just north of County Line Road and is bounded on the west by the South <br />Platte River and on the east by South Broadway. The drainage basins include <br />approximately 2.6 square miles. The project location is shown on the vicinity <br />map in Figure 2-1. <br /> <br /> AL.....lO.. " <br />26 <br />c_, ~ <br /> ~ <br />~SI~PI " C <br /> . ~ <br /> c <br /> . <br /> . <br /> . <br /> . <br /> r--.... <br /> , c" <br /> , '-> <br /> C~ <br /> <br />Drainaae Basin Characteristics <br /> <br />Some important physical features of the overall study area are discussed below <br />and are labeled on the Location Sheets (Sheets 2 and 3): <br /> <br />2. City Ditch: The ditch (owned by Englewood) flows to the north and is <br />located in the lower portion of the basin, mostly on the west side of <br />Santa Fe Drive. In the future, the ditch is planned to be enclosed in a <br />60-inch pipe. <br /> <br />" <br />. <br />" <br /> <br />" <br />" <br />. <br />u <br /> <br />A'UPA"OE ltD <br /> <br />3. Highline Canal: This feature is owned and operated by the Denver <br />Water Department and crosses the upper basins of Rangeview and <br />Jackass Gulches. Drainage from the Rangeview basin upstream of the <br />Highline Canal would normally flow across the canal into Rangeview <br />Gulch. However, development in the area directs the 1 DO-year flow <br />through a storm sewer system to the Jackass Gulch basin. Flows from <br />the Upper Jackass basin cross the canal in a storm sewer system. <br />Storm runoff from the South Park commercial area just south of the <br />Upper Jackass basin is discharged into the Highline Canal through <br />several onsite detention facilities. During the 100-year event, the total <br />discharge from these facilities is approximately 550 cfs. <br /> <br />ARAPAHOE <br />DOUGLAS <br />COUNTY <br /> <br />PRo.a.CT <br />LOCATIOII <br /> <br />Routine Highline Canal releases during rainfall events have caused local <br />flooding in the Lee Gulch drainageway. From the Highline Canal Master <br />Plan study done in 1975, the capacity of the canal between Lee Gulch <br /> <br />FIGURE 2-1 <br />LOWER DAD CLARK GULCH & DFA 0068 <br />VICINITY MAP <br /> <br />I <br />