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<br />Date <br /> <br />Discharges <br />(Cubic Feet per Second) <br /> <br />J'>.pproxirnate <br />Frequency (Years) <br /> <br />June 7, 1921 <br />September 4, 1938 <br />April 25, 1942 <br />June 15, 1949 <br />. June 18, 1965 <br />'lay 8, 1969 <br />May 8, 1973 <br /> <br />31,000 <br />18,500 <br />19,200 <br />17,800 <br />23,500 <br />21,800 <br />31,500 <br /> <br />100 <br />30 <br />30 <br />25 <br />50 <br />50 <br />100 <br /> <br />Photographs of the 1969 flood in Evans are shown in Figures 2 <br />through 6 (Reference 6). <br /> <br />2.4 Flood Protection Heasures <br /> <br />Two significant flood protection m~asures have been taken in the City <br />of Evans. One was to replace the destroyed 37th Street bridge after <br />the 1969 flood with a much higher, arch-type bridge. The old 37th <br />Street bridge was unable to pass the 1969 flood, causing its destruc- <br />tion and considerable backwater flooding into the eastern section of <br />Evans. ~he new bridge was able to pass most of the 1973 flood without <br />causing much backwater flooding in Evans, even though the discharge <br />was higher in 1973 than in 1969. The other significant flood pro- <br />tection measure was the construction of a levee along the north bank <br />of the South Platte River from u.s. Highway 85 to 37th Street. A <br />larger area of Evans would have been flooded in 1973 if it was not <br />for this levee. The levee will contain a lOa-year flood. <br /> <br />3.0 ENGINEERING METHODS <br /> <br />For flooding sources studied in detail in the cOInPlunity, standard hydro- <br />logic and hydraulic study methods were used to determine the flood <br />hazard data required for this study. Floods having recurrence intervals <br />of 10, SO, 100, and 500 years llave been selected as having special sig- <br />nificance for flood plain management and for flood insurance premium <br />rates. The analyses reported here reflect current conditions in the <br />watersheds of the flooding sources. <br /> <br />3.1 Hydrologic Analyses <br /> <br />Hydrologic analyses were carried out to establish the peak discharge- <br />frequency relationships for floods of the selected rccurrrence <br />intervals for each stream studied in detail in the community. <br /> <br />The U.S. Army Corps of Engineers, Omaha District, provided the flood <br />discharges for the 10-, 50-, 100-, and SOO-year discharges for the <br />South Platte ~iver through Evans (Reference 5). <br /> <br />4 <br />