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<br />- <br /> <br />II <br />II <br />tl <br />II <br />II <br />II <br />II <br />II <br />II <br />II <br />II <br />II <br />II <br />II <br />II <br />II <br />II <br />II <br />II <br /> <br />Lower Big Dry Creek Hydrologic Study <br /> <br />channelized and of uniform width and depth. Some areas of embedded cobble are present in <br />areas where bridges cross the stream (Aquatics Associates 1999b). Previous studies (W'WE <br />2000) have indicated that erosion of the streambed (i.e., vertical erosion) is minor in this <br />segment; however, banlc erosion is common on the outside bends of stream meanders. <br /> <br />Overall, the streambed slopes from Standley Lake to the confluence with the South Platte River <br />are relatively mild, less than 0.35 percent, with the exception of slopes ranging from 0.5 to 2.0 <br />percent from just below the dam to approximately 1 04th Avenue. The natural channel slope is <br />affected by several grade control structures that exist along the creek such as bridges, diversion <br />structures, and riprap weirs (WWE 2000). The stream has a concave profile from Standley Lake <br />to approximately 1 04th Avenue, indicating that the stream has downcut over time. This would <br />be expected because of the construction and long-term placement of the dam creating Standley <br />Lake. From 104th AVI:::nue to 128th Avenue, the slope remains fairly constant at approximately <br />0.34 percent. From 128th Avenue to just above the confluence with the South Platte, the slope <br />also remains relatively constant at 0.24 to 0.21 percent. The slope decreases to 0.12 percent just <br />prior to the confluence (WWE 2000). <br /> <br />3.4 Extent of Current Development and Urban Growth Boundaries <br /> <br />Municipal and unineorporated county areas within the watershed boundaries inc:1ude <br />unincorporated Jefferson County (over half of which is Rocky Flats), Westminster, <br />unincorporated Weld County, unincorporated Adams County, the City and County of <br />Broomfield, Thornton, Arvada, and Northglenn, as shown in Figures 2 and 3. Very minor <br />portions of Superior and Federal Heights make up the remainder. Rapid urbanization is <br />occurring along the 1-25, E-470 and U.S. 36 corridors, particularly in northeastern Broomfield <br />and northern Thornton. Historically agricultural areas continue to change to residential, <br />commercial and indm;tria1 uses. The Denver Regional Council of Governments (DRCOG) <br />reports that the middle reaches of the Big Dry Watershed are blanketed by plans for urban growth <br />over the next 25 years (DRCOG 2005). <br /> <br />971-179.092 <br />June 2005 <br /> <br />Page 16 <br /> <br />Wright Water Engineers, Inc. <br />