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<br />I <br /> <br />2 <br /> <br />I <br /> <br />3 <br /> <br />I <br /> <br />Hydraulic and cross-section data prepared by the U.S. Army Corps of <br /> <br /> <br />Engineers (COE) were obtained and utilized during the preparation of this <br /> <br /> <br />report. <br /> <br />I <br /> <br />I I. STUDY AREA DESCRIPTION <br /> <br />I <br /> <br />I <br /> <br />Drainage Basin Characteristics <br /> <br />The Cache la Poudre River originates near the Continental Divide in Rocky <br /> <br /> <br />Mountain National Park and flows through Larimer and Weld Counties before <br /> <br />joining the South Platte River approximately five stream miles east of the <br /> <br /> <br />Greeley corporate limits. <br /> <br /> <br />The drainage basin consists of heavily forested mountain areas in the <br /> <br /> <br />western portion of the basin and rolling prairie in the eastern portion. The <br /> <br /> <br />drainage area of the Cache la Poudre River is 1,890 square miles at the <br /> <br /> <br />confluence with the South Platte River. The climate of the basin ranges from <br /> <br /> <br />alpine in the headwaters to semiarid at the mouth. <br /> <br />I <br /> <br />Mapping <br /> <br />Topographic mapping (1" = 200' with four-foot contour intervals) was <br /> <br /> <br />obtained from Falcon Air Maps and was based on aerial photography made in <br /> <br /> <br />1973. Aerial photographs made in 1982 were obtained and enlarged to 1" = 200' <br /> <br /> <br />scale. The topographic mapping was updated using the new aerial photographs <br /> <br />(October 1982) to locate all new buildings and other physical features. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Acknowledgements <br /> <br />The City of Greeley assembled a Floodplain Panel in 1982 to study the <br /> <br /> <br />problems and assess future uses of the Cache la Poudre floodplain. The <br /> <br /> <br />Floodplain Panel provided valuable input during the course of this study <br /> <br /> <br />regarding community concerns about existing problems and future planning for <br /> <br /> <br />the study area. <br /> <br />We wish to acknowledge the following individuals for their help and <br /> <br /> <br />guidance throughout this study: <br /> <br />I <br /> <br />I <br /> <br />Study Area <br /> <br />The study area consists of the floodplain of the Cache laPoudre River <br /> <br /> <br />within the City. The river enters the corporate limits at approximately 16th <br /> <br /> <br />Avenue and flows in a southeasterly direction about 2.5 miles to Ash Avenue <br /> <br /> <br />where it leaves the corporate limits (see Figure 1). The river has a slope of <br /> <br /> <br />7.3 feet per mile in the study area. The Cache la Poudre River is crossed by <br /> <br /> <br />6th, 8th, 11th and Ash Avenues, 5th and 8th Streets, and the Union Pacific <br /> <br /> <br />Railroad. A control structure located at the City wastewater treatment plant <br /> <br /> <br />is used to divert water to the Great Western Sugar Company and also is used as <br /> <br /> <br />a crossing structure for sewer lines connecting the two sides of the <br /> <br /> <br />wastewater treatment plant. <br /> <br />The floodplain is heavily developed throughout most of the study area <br /> <br /> <br />with residential, commercial and industrial developments. The river is chan- <br /> <br /> <br />nelized with flood control levees present in much of the study area. The <br /> <br /> <br />Union Pacific Railroad tracks act as a barrier to flood flows. The tracks are <br /> <br /> <br />several feet higher than the adjacent land creating a large ponded area during <br /> <br /> <br />large flows. The Colorado and Southern Railroad embankment contains flood <br /> <br /> <br />flows south of the river and west of the Union Pacific Railroad. <br /> <br /> <br />Immediately upstream of the study reach is an area undergoing gravel <br /> <br /> <br />mining. Numerous active and abandoned gravel pits are located in this area. <br /> <br />Also present in the floodplain are remnants of the old river channel and other <br /> <br /> <br />evidence of channel migration. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Mr. Sam Sasaki <br /> <br />Community Development Director <br />for the City of Greeley and <br />Floodplain Panel member <br /> <br />I <br /> <br />I <br /> <br />Mr. Tom Cowan <br /> <br />Floodplain Panel member <br /> <br />I <br /> <br />I <br /> <br />Mr. John Pacheco <br /> <br />Floodplain Panel member <br /> <br />Mr. Tom Romero <br /> <br />Floodplain Panel member <br /> <br />I <br /> <br />I <br /> <br />Mr. Bob Stoll <br /> <br />Floodplain Panel member <br /> <br />I <br /> <br />Mr. Gerry McRae <br /> <br />Floodplain Panel member <br /> <br />I <br /> <br />We also wish to thank Mr. Larry Lang and Mr. Randy Seaholm of the <br /> <br /> <br />Colorado Water Conservation Board for providing technical assistance and <br /> <br /> <br />Mr. Harold Law and Ms. Ann Jamison for additional assistance. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br />