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<br />I <br />II <br />I <br />I <br />Ii <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 />II <br />I <br /> <br />CR. 35 to CR. 33 -- The channel in this reach has limited capacity (less than the 10-year event). Once <br />the flows exceed the channel capacity, they follow along the relatively flat topography in a wide, <br />shallow floodplain. Along the north overbank in an area approximately 1,200 feet downstream of CR. <br />33, the flows split away from the main channel and are conveyed to the north towards the City of <br />Sterling contributing to the Pawnee Creek Overflow. These flows mainly inundate agricultural fields <br />with some potential for flooding individual structures. Along the south overbank, the flood flows are <br />wide until the creek forms a large oxbow. At this location, the flood flows overtop the bank and follow <br />a direct alignment east to CR. 35. In the area of the oxbow, the Pawnee Creek channel contains the <br />flows until they reach CR. 35 extended and at this point combines back with the main channel flows. <br /> <br />CR 33 to CR. 31 -- As in the lower reaches, the channel has limited capacity and cannot handle flows <br />of even the 10-year magnitude. The 100-year floodplain is generally wide with shallow depths and has <br />flows splitting off from the main channel. In the upstream area adjacent to CR. 31, the floodplain is <br />very wide (approximately 4,600 feet). The existing channel and bridge crossing are undersized, and <br />the road acts as a weir spreading out the flood waters. Along the south overbank, flows split in a <br />southeasterly direction away from Pawnee Creek toward HWY 6 near the Town of Atwood. The <br />highway and railroad redirect the flows northeast towards the Pawnee Creek main channel. A berm <br />has been constructed approximately one mile south of the Pawnee Creek crossing. This berm blocks <br />some of the flows and forces a portion of the water over the highway and railroad embankment. The <br />remaining flows overtop the berm and continues north to the highway bridge where they combine with <br />the flows along the main stem of Pawnee Creek. In the lower portion of this reach at CR. 33, the <br />floodplain is confined by the channel banks south of the bridge crossing, as well as by a gravel <br />driveway to the north and CR. 33 to the east, <br /> <br />Upstream of CR. 31 -- No floodplain mapping is available upstream of CR. 31. However, hydraulic <br />analysis was completed by the SCS for a distance of about 1,000 feet, Based on discussions with the <br />City of Sterling and the Colorado Water Conservation Board, the floodplain is very wide in the <br />upstream reaches. There is the potential for flooding of some local residences, as well as damage to <br />agricultural farmland. No major flow splits have been determined in this area which would impact the <br />City of Sterling. <br /> <br />Hydrology <br /> <br />A detailed hydrologic analysis was not completed for this study. Detailed hydrology was completed by <br />the SCS and presented in their April 1992 Report. Flow data for various storm events generated for <br />that report were used as a basis for development of existing floodplain information, as well as for the <br />evaluation of proposed improvements. Final flows were reviewed and approved by the Colorado <br />Water Conservation Board and the City of Sterling for use in this study. A summary of the discharges <br />used for existing conditions is presented in Table 6, <br /> <br />24 <br />