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FLOOD02948
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Last modified
1/25/2010 6:25:54 PM
Creation date
10/4/2006 11:21:44 PM
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Floodplain Documents
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Title
Flood of 1997: Hazard Mitigation Team Report in Response to DR-1186-CO Flood Disaster in CO
Date
10/1/1997
Prepared For
State of Colorado
Prepared By
FEMA
Floodplain - Doc Type
Flood Documentation Report
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<br />Surface and Hydrology <br /> <br />The greatest impacts from the 1997 flood event occurred in the following areas <br />(Larimer, Logan and Morgon counties): <br /> <br />Larimer County <br /> <br />Spring Creek drainoge in Fort Collins <br /> <br />Fairbrooke and Clearview Drainage Channels in western Fort Collins <br /> <br />West Vine Drainage area in Northwestern Ft. Collins <br /> <br />Colorado State University locol drainage area <br /> <br />Morgan County <br /> <br />Shaefer Draw north and into the Town of Weldona <br /> <br />Logan County <br /> <br />Pawnee Creek northwest/west of Sterling in Atwood, <br />and the City of Sterling <br /> <br />Numerous streams .and watercourses contributed to flood damages in the <br />following additionally declared counties: lincoln, Prowers, Crowley, Kiowa, Weld, <br />Baco, Otero, Clear Creek, Phillips and Elbert. <br /> <br />Larimer, Logan, Weld, Morgan and Clear Creek counties have drainage <br />tributaries to the South Platte River. In addition, portions of Elbert and Lincoln <br />counties have tributaries to the South Platte River. The river basin has a drainage <br />area of about 24,300 square miles and is located in three states, Colorado [79 <br />percent of the basin); Nebraska (15 percent of the basin); and Wyoming (6 <br />percent of the basin). <br /> <br />The basin has a continental-type climate modified by topography, in which there <br />are large temperature ranges and irregular seasonal and annual precipitotion. <br />Mean temperatures increase from west to east and on the plains from north to <br />south. Areas along the Continental Divide average 30 inches or more of pre- <br />cipitation annually, which includes snowfall in excess of 300 inches. In contrast, <br />annual precipitation on the plains east of Denver, Colorado, and in the South <br />Park area in the southwest part of the basin, ranges from 7 to 15 inches. Most of <br />the precipitation on the plains occurs as rain, which falls between April and <br />September. <br /> <br />Rangeland is present across all areas of the basin except over the high moun- <br />tain forests. Agricultural land is restricted mostly to the plains. Urban or built-up <br />I~nd is present primarily along the Frant Range urban corridor in Colorado. <br /> <br />Phillips County and parts of Lincoln and Elbert Counties have drainage tributar- <br />ies to the Republican River. The Republican River is, in turn, tributary to the <br />Kansas River in Kansas. The Republican River Basin in Colorado consists prima- <br />rily of rangeland with some farming and ranching communities scattered through- <br />out the basin. <br />
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