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<br />SECTION 2.0 <br />STUDY AREA DESCRIPTION <br /> <br />2.5 <br /> <br />2.1 <br /> <br />Topography and Physiography <br /> <br />The Dakota Hogback runs through the Willow and Little Willow Creek Watersheds creating a <br />significant natural hydrologic and topographic boundary. The slope of the terrain and <br />tributaries within the headwater areas of these watersheds in the foothills of the Front Range <br />becomes very steep, having grades greater than 10%, The general slope of the terrain in the <br />middle and lower reaches of the watersheds in the Eastern High Plains province ranges from <br />2% to 6%. <br /> <br />2.2 <br /> <br />Soils <br /> <br />Hydrologic soil types within the watershed study area are shown in Figures 2.IE and 2.1 W. <br />Hydrologic soil types were identified based on the U.S. Department of Agriculture, Soil <br />Conservation Service's Soil Survey of Castle Rock Area. Colorado, dated November 1974 <br />(Reference 3). <br /> <br />2.6 <br /> <br />Hydrologic soil Types B, C and D are predominant in the watershed. Type B soils have <br />moderate infiitration rates, whereas Types C and D soils have lower infiltration potential. <br /> <br />2.3 <br /> <br />Reservoirs and Detention Basins <br /> <br />There are four small reservoirs within the watersheds. The Platte Canyon Reservoir is located <br />in the lower reach of the Little Willow Creek Watershed immediately upstream of the South <br />Piatte River. It is primarily used to control irrigation flows along the High Line Canal which <br />traverses through the lower portion of the watershed. The Aurora Rampart Reservoir is <br />located in the middle of the Little Willow Creek Watershed and serves as a raw water storage <br />facility for the City of Aurora. A regional on-stream detention/water quality pond was <br />constructed as a part of the Roxborough Village Park Subdivision and is located along Willow <br />Creek about I mile upstream of the Platte Canyon Reservoir. There is a low dam located on <br />private property along Willow Creek about three quarters of the way up the watershed, which <br />is privately owned. <br /> <br />2.4 <br /> <br />Flood History <br /> <br />No documentation of flooding in the study area is known to exist. <br /> <br />Vegetation <br /> <br />Vegetation in the watershed consists primarily of native grasses typical of High Plains areas, <br />with a portion of the prairie grassland being used as pasture. About one-half of the study area <br />(primarily the northern one-half) is currently in agricultural use as cropland. Intermittent <br />stands of willow trees grow along the creek beds in the lower reaches, becoming increasingly <br />more dense in the upper reaches. <br /> <br />Natural riparian vegetation is evident along many of the major streams in the study area and <br />consists primarily of cottonwood, willow, and herbaceous wetland vegetation. In general, the <br />natural riparian vegetation is confined to the alluvial channel corridor and varies in width <br />from about 8 to 10 feet in the middle reaches of the watershed. The lower reach of Willow <br />Creek supports a well developed, diverse, and lush riparian corridor. The existing wetland <br />and riparian areas within the watersheds have been deiineated and are described in a report <br />entitled "Willow Creek Watershed and Riparian Areas. Douglas County. Colorado" <br />completed by ERO Resources Corporation, July 1996 (Reference 4). <br /> <br />Watershed Imperviousness <br /> <br />Areas of imperviousness, representative of future development conditions in the study area, <br />are shown in Figures 2.2E and 2.2W (located in the Appendix). Projected development for <br />the basins is based on the Douglas County Master Plan, and discussions with the Douglas <br />County Planning Department and the UD&FCD. A large portion of the study area consists of <br />undeveloped grassland and agricultural land. Small areas of existing development have <br />occurred, primarily in the Little Willow Creek Watershed, The Roxborough Village <br />Subdivision located along Little Willow Creek below the hogback and the residential areas <br />behind the hogback have been developed according to the Douglas County Master Pian, <br />adopted by the Douglas County Planning Commission in January 1992 (Reference 5). The <br />homes in the Roxborough Village area have typically been built at a density of 6 per acre, <br />while the development of homes behind the hogback have historically been on one-half acre <br />lots. In accordance with Volume I of the District's Urban Storm Drainage Criteria Manual <br />(USDCM) (Reference 6), the imperviousness used in the CUHPF/PC model where <br />development has occurred in these areas is 45% and 30%, respectively. <br /> <br />Existing development within the Willow Creek and Little Willow Creek Watersheds is <br />described by the County as separated urbanized areas. According to the Douglas County <br />Planning Department, future development in the separated urbanized areas can be expected to <br />occur at a density equal to developments in the past. Therefore, the imperviousness used in <br />the CUHPF/PC model for the future development conditions within the separated urbanized <br />area is 30% west of the hogback and 45% east of the hogback. The Foothills Water <br />Treatment Plant is situated in the Willow Creek Watershed. This facility is assumed to have <br />an imperviousness of 10%. Outside of the separated urbanized boundaries, there are a few <br />pockets of land currently zoned general industrial or business. For future development <br />conditions, these areas are considered to have an 85% imperviousness. The majority of the <br />area outside of the separate urbanized boundaries is currently zoned agricultural. Because of <br /> <br />4 <br />