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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 />Existing Flooding Conditions <br /> <br />Historically, Pawnee Creek has proven to be the most significant flooding source for the <br />City of Sterling and for Logan County. Flooding in the City of Sterling from Pawnee <br />Creek has occurred mainly as a result of insufficient channel capacity, roadway <br />structures, and the bridges at HWY 6 and the UPRR. The Soil Conservation Service <br />(SCS) completed a floodplain analysis of the Pawnee Creek overflow area in <br />unincorporated Logan County in April of 1992 that determined the 100-year floodplain <br />for existing basin and channel conditions. This report supplemented the previous <br />Leaf/Resource Consultants report of 1983, which was completed for the portion of the <br />Pawnee overflow in the City of Sterling. A floodplain map was prepared which <br />delineated the 100-year floodplain for Pawnee Creek through this study reach. Based on <br />the SCS Report, a description of the existing flood potential is presented below: <br /> <br />South Platte River to HWY 6IUPRR -- Flooding in this reach is limited by the capacity <br />of the existing bridge structures. However, the flooding can be severe and inundate much <br />of the highway and railroad. Flows split downstream of the UPRR bridge causing a very <br />wide (approximately 4,500 feet), shallow floodplain to the confluence with the South <br />Platte River. Two residences are potentially flooded in this reach: One residence is <br />located in the 100-year floodplain and is on the north bank of Pawnee Creek adjacent to <br />the railroad; and the other residence is located further downstream on a higher plateau <br />which could be impacted by potential shallow flooding. Additional flooding occurs to <br />the Sterling No.1 Ditch, and adjacent agricultural lands. <br /> <br />UPRR/HWY 6 to CR. 35 -- Flooding in this reach is basically caused by: (1) <br />Insufficient capacity of the bridges at HWY 6 and the UPRR; (2) insufficient channel <br />capacity on Pawnee Creek; and (3) floodwater draining into the Town of Town of <br />Atwood, which is a result of flow splits from the upper reaches of the basin. The greatest <br />impact of flooding occurs along HWY 6 to the north. Flood flows exceeding the capacity <br />of the bridges travel along HWY 6 damaging fannlands, inundating the Riverside <br />Cemetery, and eventually spreading out to the northwest into the City of Sterling. This <br />area is referred to as the Pawnee Creek Overflow, and is the driving force for the <br />Community to make flood improvements for the Pawnee Creek flood events. <br /> <br />CR. 35 to CR. 33 -- The channel in this reach has limited capacity (less than the lO-year <br />event). Once the flows exceed the channel capacity, they follow along the relatively flat <br />topography in a wide, shallow floodplain. Along the north overbank in an area <br />approximately 1,200 feet downstream of CR. 33, the flows split away from the main <br />channel and are conveyed to the north towards the City of Sterling contributing to the <br />Pawnee Creek Overflow. These flows mainly inundate agricultural fields with some <br />potential for flooding individual structures. Along the south overbank, the flood flows <br />are wide until the creek forms a large oxbow. At this location, the flood flows overtop <br />the bank and follow a direct alignment east to CR. 35. In the area of the oxbow, the <br />Pawnee Creek channel contains the flows until they reach CR. 35 extended and at this <br />point combines back with the main channel flows. <br /> <br />32 <br />