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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />3.0 ENGINEERING METHODS <br /> <br />3.1 Hydrologic Analyses <br /> <br />Hydrologic analyses were carried out to establish the peak discharge- <br />frequency relationships for the Crystal River in the vicinity of the Town of <br />Marble, Colorado. <br /> <br />Discharges along the Crystal River were calculated using the PEAKFQ <br />computer program (Reference 2) which performs statistical flood <br />frequency analyses of annual peak discharges following procedures <br />recommended in Bulletin 17-B of the Interagency Advisory Committee on <br />Water Data (1982). The analysis for the Crystal River incorporates USGS <br />gage information with over 46 years of record, along the Crystal River <br />(1956 to 2001). Peak discharges were determined using annual peak <br />discharges from the Placita and Avalanche Creek gages, located just <br />downstream of the Town of Marble. The calculated peak discharges were <br />adjusted at various locations along the study reach based on the guidelines <br />provided in the Manual for Estimating Characteristics of Natural-Flow <br />Streams in Colorado. Technical Manual No.1 (Reference 5), <br /> <br />Peak discharge-drainage area relationships for the Crystal River are shown <br />in Table 2. <br /> <br />Table 2: Summary of Discharges for the Crystal River <br /> <br />Flooding Source and Location <br />Along Crystal River <br />Confluence with Rapid Creek <br />Confluence with Milton Creek <br />Town of Marble <br />Upstream Limit of Study <br /> <br />Drainage Area <br />(Square Miles) <br />93.05 <br />83.65 <br />73,59 <br />53.32 <br /> <br />10-Year <br />1,994 <br />1,833 <br />1,657 <br />1,284 <br /> <br />Peak Discharge (cfs) <br />50-Year 100- Year <br />2,445 2,625 <br />2,248 2,413 <br />2,031 2,181 <br />1,575 1,691 <br /> <br />500- Year <br />3,028 <br />2,783 <br />2,515 <br />1,950 <br /> <br />3.2 Hydraulic Analysis <br /> <br />Analysis of the hydraulic characteristics of flooding from the Crystal <br />River were carried out to provide estimates of the elevations of floods for <br />the 10-, 50-, 100- and 500-year storm events, Water surface elevations <br />(WSELs) were computed using the U. S Army Corps of Engineers HEC- <br />RAS step backwater program (Reference 6), Cross-sections for the <br />backwater program were taken from project topographic mappmg. <br />Hydraulic structures, such as bridges along the project reach were field <br />surveyed in 2003. <br /> <br />ICON Engineering, Inc. <br />May 2004 <br /> <br />6 <br />