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<br />I <br />I <br />. <br />I <br />. <br />. <br />I <br />I <br />I <br />II <br />I <br />II <br />'. <br />II <br /> <br />FLOOD HAZARDS <br /> <br />Introduction <br /> <br />The purpose of the flood study is to evaluate flood elevations and areas likely to be <br />impacted by floods within the Town of Rico. Flood events of magnitudes which are <br />expected to be equaled or exceeded once on the average during any 100- or 5OD-year <br />period were analyzed. Cross-sections and roughness parameters were selected based on <br />flows of these magnitudes. All elevations in this study are referenced to the National <br />Geodetic Vertical Datum of 1929 (NGVD). <br /> <br />Three methods were employed to evaluate peak flood discharges for the Dolores River <br />and Silver Creek in this study. A statistical frequency analysis was performed using <br />data for the Dolores River. Historical accounts and photographs of high water <br />elevations and damage caused by flood events without flow measurements were also <br />used to determine flood discharges. Additionally, data from similar drainage basins in <br />the region were considered, panicularly for Silver Creek which is an ungaged basin. <br /> <br />Frequency AlUllyses <br /> <br />I~ <br />~ <br />~ <br />~ <br />- <br /> <br />Peak discharges for the Dolores River were evaluated by applying The U.S. Geological <br />Survey (USGS) Annual Peak Flow Frequency Analyses Program J477 Version 3.7, <br />revised 11-5-81. The reference gage station (USGS 09165000) is located near the <br />Dolores-Montezuma County Line approximately four miles south of Rico. Scotch <br />Creek is the only significant tributary to the Dolores River between Rico and the gage. <br />Silver Creek is another significant tributary which joins the Dolores River near the <br />north Town Limit. Incomplete flow data from a gage located at Rico between 1914 <br />and 1921 were not included in the analysis because these data do not include peak <br />flows. The USGS program generates curve parameters using a log-Pearson Type III <br /> <br />1 <br />