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L TAG GART gg9 <br /> raw—," <br /> ENGINEERING ASSOCIATES.INC. <br /> 2480 West 26tn Avenue•Suite 340-B•Denver.Colorado 80211 •1303)455.3600•FAX(303)455-9929 <br /> March 19, 1997 <br /> ' Mr. Bill DeGroot <br /> Chief, Floodplain Management <br /> Urban Drainage and Flood Control District <br /> 2480 West 26th Avenue, Suite 156-B <br /> Denver, CO 80211 <br /> RE: Initial Reconnaissance of Drainage Network and South Boulder Creek's <br /> Hydrology, Highway 36 to Approximately the Wellman Ditch, Phase 11. <br /> Dear Mr. DeGroot: <br /> Our Phase I effort identified that the Flood Hazard Area Delineation Report <br /> (FHAD) underestimated the flow leaving South Boulder Creek at Highway 36 and <br /> did not portray spillage paths to the west side of the valley, particularly along <br /> Foothills Parkway. This Phase II report provides an initial reconnaissance of the <br /> overflow routes and approximate flows of the West Valley Overflow north of <br /> Highway 36 to the area of the Wellman Ditch. Drawing No. 3 depicts the results <br /> of this overflow analysis (Drawings 1 and 2 are with the Phase I report). <br /> We obtained and reviewed additional hydrology information by the U.S. Army <br /> Corps of Engineers (Corps). In Phase I we modified the Corps' Storm Water <br /> Management Model (SWMM) model to better reflect the Viele watershed and its <br /> U outfall channel to South Boulder Creek. In this Phase II we have greatly refined <br /> �1 the SWMM model detail downstream of Highway 36 in order to identify <br /> Usignificant flow paths and approximate discharges. <br /> The 100 year spill from South Boulder Creek just upstream of Highway 36 would <br /> flow to the northwest along the south side of the freeway, with an initial portion <br /> returning to South Boulder Creek through the Viele outfall, spillage from the Dry <br /> Creek Ditch No. 2, and the Anderson Ditch. The majority of the spill would <br /> U overtop Highway 36 west of Foothills and flow northerly to the intersection of <br /> Baseline and Foothills. The intersection topography would largely control the <br /> hydraulics of the spill distribution and would result in six surface flow paths and a <br /> seventh path through the culverts under Foothills between the small detention <br /> ponds that are south of Baseline on either side of Foothills. Three of the surface <br /> paths would follow Foothills to the north (two travel lanes and the westerly <br /> u borrow ditch). Two would follow Baseline to the east, and one would overtop <br /> u Foothills slightly south of the intersection. The last three routes would <br /> commingle and split again, following the streets to the north and the Crossover <br /> Hydrology•Hydraulics•Sediment Transport <br /> Civil Engineering for Flood Control Waterways.Water Supply and Parks <br /> Environmental Mitigation•Forensic Services <br />