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FLOOD01863
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Last modified
1/29/2010 10:15:21 AM
Creation date
10/4/2006 10:25:42 PM
Metadata
Fields
Template:
Floodplain Documents
County
Morgan
Logan
Sedgwick
Community
Northeastern Colorado
Stream Name
South Platte River
Title
Report on the Floods of June 1965
Date
1/1/1967
Prepared For
State of Colorado
Prepared By
US Army Corps of Engineers
Floodplain - Doc Type
Flood Documentation Report
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<br />, <br /> <br />velocity flash floods which are particularly hazardous to life and <br />property. The foothills regions have flash floods similar to the <br />mountain regions, but generally reflect a greater hazard because dry <br />washes become raging torrents with high velocities that erode the <br />normal boundaries of stream flow. As the foothills streams converge <br />to form the main tributaries and tributary streams converge on the <br />main. stream, the valleys and flood plains become broader. The <br />broader valleys and flatter stream slopes reduce the discharge rate <br />of the flood by combinations of temporary overbank storage and lower <br />energy gradients. ,The lower velocities increase the duration of <br />flooding and permit the sediment load and debris load carried from <br />upstream areas to be deposited on the more productive lands of the <br />lower valleys. Consequently, the damaging effects in the lower <br />valleys are a combination of destruction by erosion and inundation <br />with reduction in the productive quality of valley lands by flood <br />debris and sediment. The .damaging effects of floods /;lore also governed <br />significantly Qy the nature of storm patterns and tributary runoff. <br />Rainfall concentrated over one tributary watershed generally limits <br />the destructiveness of floods to the tributary stream affected. <br />However, the runoff from larger storm patterns results in flood dis- <br />charges on many tributaries which converge on the main stream, thereQy <br />causing more widespread destruction, prolonged inundation, and greater <br />flood damages over larger areas. <br /> <br />!; <br /> <br />t <br />r <br />t <br />, <br /> <br />III. EXISTING IMPROVEMENTS <br /> <br />14. FEDERAL IMPROVEMENTS <br /> <br />a. Corps of Engineers. <br /> <br />(1) The Cherry Creek Dam and Reservoir on Cherry Creek was <br />completed in 1953 at a cost of $14.1 million. It is situated <br />approximately 11. 5 miles above the mouth. of the stream at central <br />Denver. It controls 385 square miles of the 409 square mile Cherry <br />Creek watershed. The dam is a rolled earth fill structure, with a <br />reservoir storage capacity to the crest of the emergency spillway of <br />96,000 acre-feet. This storage capacity consists of 81,000 acre-feet <br />for flood control storage and 15,000 acre-feet for conservation storage. <br />The conservation pool also serves the project's recreation function. <br /> <br />(2) The Kelly Road Detention Dam is a small capacity (380, <br />acre-feet) flood detention project on Westerly Creek situated near the <br />Lowry Air Force Base at Denver, Colorado. It provides flood protection <br />for portions of Aurora and Denver, Colorado. It was completed by the <br />Corps of Engineers in 1954 at a cost of $221,000. <br /> <br />b. Soil Conservation Service. The Soil Conservation Service has <br />constructed three watershed projects in the South Platte River basin <br />which include a total of 106 floodwater retarding structures. The <br /> <br />8 <br />
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