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<br />, <br /> <br />'" <br /> <br />INVESTIGATIONS ~O ANALYSIS <br /> <br />8. Flood Elevation <br /> <br />Internretatlon and Use of Recort <br /> <br />Water surface elevations for the 10-, 25-, 50-, and IOO-year <br />floods, as determined at each cross section, may be found in <br />Table 4 "Flood Frequency-Elevation and Discharge Data". The <br />flood profile data (sheets 1-13) show a graphical relationship of <br />water surface elevations along the stream reaches for the given <br />frequencies. Selected typical cross sections from different <br />reaches within the study area are shown on sheets 1 through 6. <br />The flood profiles may be used in areas where controversy arises <br />over the IOO-year flood boundary shown on the flood plain maps. <br />since the flOOd profile exhibits give the water surface elevation <br />at a specific point on the reference line, the flood elevations <br />can be surveyed on the ground to alleviate any discrepancies on <br />the base map. <br /> <br />A. Freauencv and Discharae <br /> <br />The 10-, 25-, 50-, and 100-year flood events are used as the <br />flood frequencies for this flood plain analysis. Thus, the data <br />developed in this report will be suitable, not only for <br />regulation purposes and H.B. 1041 designation, but is also <br />consistent with Federal Insurance Administration flood insurance <br />studies conducted by the Federal Emergency Management Agency. <br /> <br />These various flood events have an average occurrence of once in <br />the number of years as indicated. For example, the lOO-year <br />flood occurs, on the average, once in a 100-year period, and has <br />a one percent chance of being equaled or exceeded in any given <br />year. <br /> <br />C. Flooded Areas <br /> <br />10-vear. 25-vear and 50-vear Flood Events <br /> <br />Flood plain maps, sheets 1 through 6, show the boundary of the <br />100-year flood plain. The flood plain boundary was plotted using <br />flood contour elevations and stationing from the plotted flood <br />profiles. This was done at elevation intervals compatible with <br />the map contour intervals. Flood contours are shown as wiggly <br />lines at 5 ft intervals perpendicular to the direction of flow. <br /> <br />The particular uses for the various flood events in addition to <br />those stated above are as follows: <br /> <br />Information regarding these lower frequency floods is especially <br />useful for future engineering studies and land use planninq <br />purposes related to minor road systems, minor c~annel ... <br />improvements, the location of parks and recreatIonal faCIlItIes. <br />agricultural lands, and appurtenant structures. The use of the <br />lower frequency floods may be considered in planning flood <br />prp.vention projects to protect agricultural areas or other <br />property where risk to life is not a factor. <br />lOO-year Flood Event <br />The lOO-year flood event may be used in lieu of lower frequencies <br />for engineering design purposes "'~,ere greater security from <br />structure failure is desired. <br /> <br />However, the most important use of the loo-year flood event lies <br />in flood plain management and land use planning as set forth in <br />the state statutes. The State of Colorado and the Federal <br />Government considers the lOO-year frequency flood as the flood <br />event to be used in designing and proteoting structures and <br />dwellings for human occupation. Therefore, all flood plain <br />regulations are based upon the 100-year flood. <br />