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<br />k~.--':" _-'- _ __ _ ___,. _~_.L~ ~. __ <br /> <br />{ <br />ec- <br /> <br />('- <br />e( <br /> <br />~ <br /> <br />e( <br /> <br />INI'RODUCTION <br /> <br />This report evaluates the flood potential along Boxelder Creek from a <br />point about 12 miles northwest pf Wellington to its point of confluence <br />with the Cache La Poudre River, southeast of Fort Collins, Larimer <br />Colmty, Colorado. The evaluation was made wxler present conditions and <br />future conditions with the proposed five floodwater retarding structures <br />and one grade stabilizer installed. The proposed structural program <br />was developed by the Soil Conservation Service wxler the authority of <br />Public Law 566 Revised. This report is made for the Colorado Water Con- <br />servation Board to promote the best utilization of the land subject to <br />overflow. This report is based on historical information, data devel- <br />oped by use of the computer, and data developed manually using computer <br />output and other technical data. <br /> <br />This report contains maps, water surface profiles, flood plain cross <br />section locations, and elevations at all cross sections. Flood risks <br />my be appraised and the construction of facilities planned to reduce <br />flood damage. 'Although the flood plain near Fort Collins is not devel- <br />oped, at this time, it is expected to be urbanized in the near future. <br />The possibility of a lOO-year flood frequency stonn runoff or greater <br />occurring definitely exists, and it is important that the probability <br />of such a flood be anticipated in the planning of flood plain developnent. <br /> <br />SlMtARY OF FLOODS <br /> <br />The portion of Boxelder Creek flood plain that is considered in this <br />report extends about 23 miles above its JOOuth. Flooding occurs through- <br />out the flood plain in varying degrees. Local res idents outlined areas <br />of flooding that have occurred in the past, and flooding occurs on an <br />average of once every two years. There is no official gaging station <br />in the, watershed and no known flood flows have been measured. <br /> <br />GENERAL CONDITIOOS AND PAST FLOODS <br /> <br />A map of areas flooded as recalled by local residents is on file with <br />the Soil Conservation Service, Watershed Planning Staff office. The <br />mp, technical data and statements from local people obtained in the <br />field support the high frequency of flooding throughout the flood plain. <br />ÆThe Town of Wellington is subject to flooding from a combination of <br />flow from Boxelder Creek and Coal Creek, and there is a good probability <br />of a mjor stonn causing extensive flooding in Wellington. The area on <br />either side of Interstate Highway 25 and south of State Highway 14 is <br />subject to flooding. This area is agricultural now, but is planned for <br />