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Last modified
1/25/2010 6:47:17 PM
Creation date
10/5/2006 12:59:58 AM
Metadata
Fields
Template:
Floodplain Documents
County
El Paso
Community
Colorado Springs
Stream Name
Cottonwood Creek
Basin
Arkansas
Title
Engineering Study of Cottonwood Creek Drainage Basin
Date
8/7/1979
Prepared For
Colorado Springs
Prepared By
Lincoln Devore
Floodplain - Doc Type
Floodplain Report/Masterplan
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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 <br />I <br />I <br /> <br />Some heavy, but smaller storms have <br /> <br />centered on a line two to three miles east of the mountain range. <br /> <br />The most notable recent storms include the 1965 Monument - Palmer Lake <br /> <br />storm, the 1967 Ivywild - Broadmoor area storm, the 1967 Mesa area <br /> <br />storm, the 1978 north Colorado Springs storm and the 1979 Manitou <br /> <br />storm. Most of these caused considerable damage of one sort or <br /> <br />another, but not major flooding. The exception to this was the major <br /> <br />flood caused by the-1965 Monument - Palmer Lake storm in Douglas <br /> <br />County. This however was part of an overall major storm which had <br /> <br />another center along the storm axis in the Peterson Field area. <br /> <br />It must also be noted that the heaviest <br /> <br />24 hour rainfall reported along this storm axis was over the upper <br /> <br />portions of the Cottonwood Creek, Pine Creek and Kettle Creek basins. <br /> <br />This was the rainfall center of the May 30, 1935 flood on Monument <br /> <br />Creek. Kettle Creek was the prime contributor to this flood flow, <br /> <br />but flow in other creeks - particularly Cottonwood - was also quite <br /> <br />high. No accurate measurement was made of either precipitation or <br /> <br />runoff, but precipitation was reported unofficially as 16 inches in <br /> <br />24 hours near Burgess Road. This unofficial report is probably high, <br /> <br />but there is no doubt that a considerable amount of rainfall during <br /> <br />several intense periods within the general 24 hour storm. <br /> <br />The storm defined as the 100 year <br /> <br />frequency (.01 percent chance of occurrance) and known locally as the <br /> <br />Type II-A storm, is a six hour duration, low intens't storm with a <br /> <br />very high intensity burst at about the 1-1/2 hour point. The 1935 <br /> <br />storm appears to have been similar to a series of three or four such <br /> <br />r') <br /> <br />./' <br />If <br /> <br />/l <br /> <br />-15- <br />
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