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<br />flooding potentials based on conditions existing in the community at the <br />time of completion of this study. "'1aps and flood elevations will be <br />amended periodically to reflect future changes. <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 recurrence inter- <br />vals fGr each stream studied in detail in the community. <br /> <br />Flood discharges for the 10-, 50-, 100-, and 500-year floods on <br />Brush Creek Were calculated using regression equations based upon a <br />regional gage analysis for all of Eagle County (Reference 5). <br />Fourteen gages were employed in the county study, representing a <br />combined total of 318 years of record. The analysis was performed <br />using log-Pearson Type III methodology (Reference 6). The IOO-year <br />flood discharges for the approximate study reaches were also taken <br />froM these equations. <br /> <br />Peak discharge-drainage area relationships for Brush Creek are shown <br />in Table 1. <br /> <br />1'able 1. <br /> <br />Summary of Discharges <br /> <br />Flooding Source <br />and Location <br /> <br />Drainage Area <br />(Square Ililes) <br /> <br />Peak Discharges <br />(Cubic Feet per Second) <br />la-Year 50-Year lOa-Year 500-Year <br /> <br />Brush Creek <br />At Upstream and <br />Downstream Corporate <br />Limits of Eagle <br /> <br />150 <br /> <br />875 <br /> <br />1150 <br /> <br />1225 <br /> <br />1400 <br /> <br />3.2 Hydraulic Analyses <br /> <br />Analyses of the hydraulic characteristics of streaMS in the commu- <br />nity were carried out to provide estimates of the elevations of <br />floods of the selected recurrence intervals along each stream <br />studied in the community. <br /> <br />Water-surface elevations for floods of the selected recurrence intervals <br />were computed through use of the u.s. Army Corps of Engineers HEC-2 <br />step-backwater computer program (Reference 7). Cross sections for <br />the backwater analyses of Brush Creek were obtained from topographic <br />maps at a scale of 1:1200, with a contour interval of 2 feet (Refer- <br />ence 8). All bridges were field checked to obtain elevation data <br />and structural geometry. <br /> <br />Locations of selected cross sections used in the hydraulic analyses <br />are shown on the Flood Profiles (Exhibit 1). For stream segments <br />for which a floodway is co~puted (Section 4.2), selected cross <br />section locations are also shown on the Flood Boundary and Floodway <br />j\l'lap (Exhibit 2). <br /> <br />5 <br />