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<br />--- <br /> <br />-- <br /> <br />-- <br /> <br />The State Geologist has undertaken an analysis of <br />Colorado's most dangerous canyons in which flash flooding <br />can occur. Major canyons which are threatened by flash <br />floods are shown in Annex "A". <br /> <br />While the bulk of these canyons exist along the Front <br />Range, their dispersion over the State is general; many <br />communities with significant population are closely associ- <br />ated with these danger areas. Flash flooding occurs annually <br />throughout Colorado on streams and floodplains and the <br />danger is greatest to settlements located close to the major <br />streams identified in "Riverine Flooding". <br /> <br />Riverine Flooding <br /> <br />Large scale floods can develop from sustained or heavy <br />rainfall from storm systems in the spring, summer and fall <br />months in Colorado. But the most dangerous flood potential <br />is in the spring when rivers are high during the snowmelt <br />run off. Usually, rainfall in addition to snow melt run off <br />is necessary before flood ing occurs. These floods differ <br />from flash floods in that the speed of onset is slower and <br />time available for warning is greater; fewer lives are lost, <br />but millions of dollars worth of valuable farmlands, roads, <br />bridges, and other valuable assets, are at stake. It should <br />be noted, however, that although riverine floods may occur <br />over most of a river system, flash floods may simultaneously <br />occur in headwater areas where steeper gradients exist. <br /> <br />The Rio Grande, South Platte, Arkansas, and the Repub- <br />lican Rivers have a long history of flooding onto the plains <br />areas. In 1965, as a result of heavy rains concentrated <br />around the Castle Rock area, widespread flooding occurred in <br />the Denver Metro area, loss of life and very high damage was <br />also suffered along the Front Range and on the eastern <br />plains. As more development takes place in the Metro area, <br />run off potential increases and extensive damage can be <br />expected despite new flood control dams. <br /> <br />On the Western Slope the Colorado, Yampa, San Juan, <br />Gunnison (N. and S. Fork), Uncompahgre, Animas, White and <br />many other streams can be expected to flood in any given <br />year, The most likely periods for disastrous flooding are <br />during the spring snowmelt when rainfall occurs during peak <br />run off periods in May and June, and when relatively heavy <br />rainfall occurs on the Western Slope in September and <br />October. On the Western Blope in Colorado, water volumes in <br />the spring are normally large and gradients are relatively <br />steep. Riverine flooding can threaten property but the <br />distinction between flash and riverine flooding is blurred. <br />Lives are also at stake. <br /> <br />5 <br />