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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 I <br />I <br />I <br /> <br />PIS. However, none of the gaging stations contain enough data to calculate peak discharges for <br />the approximate streams, which are the subject of the hydrology calculations in this report. <br /> <br />F100dinl!: Problems and F1oodinl!: History <br />Floods in the subject watersheds normally occur during the summer months and are caused <br />primarily by intense, localized cloudbursts or thunderstorms. Typically, these floods have high <br />peak discharges with low volumes over short duration. There is usually a very short window of <br />opportunity for flood warning and evacuation once a major storms hits the area, Less damaging <br />floods can also result from rapid melting of mountain snowpack in the spring and early summer <br />months, especially on the larger drainageways. A combination of rainfall and snowmelt can <br />sometimes prove to be the worst flooding scenario for Colorado's mountain streams, Generally, <br />it is assumed that for streams with headwaters below 9,000 feet in elevation, snowmelt does not <br />influence peak discharges. <br /> <br />Many smaller flooding events occurred throughout the South Platte basin in the late 1800's and <br />early 1900's. The most extensively documented flood in the South Platte basin occurred in 1965 <br />as a result of severe downpours over several sub-basins. The flood caused over $500 million in <br />damages in the Denver metropolitan area, Most of the severe flooding events in the County <br />occur due to heavy thunderstorms in the Monument Divide area. The PIS includes a discussion <br />of historic flooding events for each of the entities within the study area. <br /> <br />In response to the severe flooding problems within the South Platte and tributary basins, several <br />flood control reservoirs have been constructed to protect urbanized areas in the western portion <br />of the County. Cherry Creek reservoir, located on Cherry Creek, was completed in 1950. There <br />are on-going studies regarding flood frequency analysis and flood forecasting to determine the <br />existing dam's adequacy for flood protection. Chatfield Reservoir, completed in 1975, is located <br />on the South Platte in the southwestern portion of the Denver metro area. Bear Creek Reservoir, <br />completed in 1982, is located on Bear Creek in the western portion of the Denver metro area. <br /> <br />Previous Studies <br />Due to severe flooding problems within the South Platte basin, several unpublished studies were <br />conducted within the South Platte basin regarding flooding and floodplain issues as they related <br />to design and construction of Cherry Creek, Chatfield and Bear Creek Reservoirs. The first PIS <br />in the county was prepared for the City of Englewood in 1974. This PIS was followed by an PIS <br />for Sheridan in 1976; unincorporated Arapahoe County in 1977; and Cherry Hills Village, <br />Columbine Valley and Greenwood Village in 1978. Glendale was included in the original <br />unincorporated Arapahoe County PIS. In addition, due to significant urban development, basin <br />planning studies and Letters of Map Revision (LOMR) are continually being developed for <br />floodplains in the County. <br /> <br />A summary of information available regarding floodplains in the county available from the <br />CWCB is shown in the Appendix, <br /> <br />Communitv Response to the CWCR Desil!:nation and Approval Process <br />A letter from the CWCB was transmitted to Arapahoe County and each of the incorporated <br />communities regarding the Board's proposed action for designation and approval of the <br /> <br />6 <br />