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Last modified
1/25/2010 6:24:14 PM
Creation date
10/4/2006 10:51:03 PM
Metadata
Fields
Template:
Floodplain Documents
County
Statewide
Community
State of Colorado
Stream Name
All
Basin
Statewide
Title
The Big Thompson Flood of 1976 Field Trip Guidebook
Date
1/1/1976
Prepared For
Annual meeting of Geological Society
Prepared By
USGS
Floodplain - Doc Type
Flood Documentation Report
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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 /> <br />HYDROLOGIC ASPECTS OF THE BIG THOMPSON FLOOD <br /> <br />Based on eyewitness acounts, the Big Thompson Flood began about <br /> <br />7 pm and was most pronounced in an area centered a few miles above <br /> <br />Drake. It is known with certainty that by 7:30 pm, U. S. Highway 34 <br /> <br />was blocked by rocks and debris that had been carried off the slopes <br /> <br />above. The high intensity rain falling on soils with a low storage <br /> <br />capacity and residing on steep slopes resulted in rapid runoff to the <br /> <br />slope channels as well as high rates of erosion. Because of the high <br /> <br />spatial variability of the rainfall, tributary and mainstream discharges <br /> <br />were variable and non-synchronous. By 11 pm flood peaks had passed <br /> <br />through the canyon and flow was diminishing. <br /> <br />The peak discharge data listed in Table 1 have been obtained in <br /> <br />two ways. Some data were derived from records of gaging stations that <br /> <br />withstood the flood. Other data were estimated by identifying high water <br /> <br />marks, measuring cross sectional area and solving the Manning equation <br /> <br />for velocity. The spottiness of rainfall and runoff can be verified by <br /> <br />comparing peak unit area discharge for Locations 1 and 2 of Table 1. <br /> <br />The upper two square miles of Dry Gulch produced over 1,600 cubic feet <br /> <br />per second per square mile while the entire six square mile watershed <br /> <br />produced at less than half that rate. Decrease in the peak unit area <br /> <br />discharge continues in a downstream direction until the Big Thompson <br /> <br />enters an area of high precipitation above Drake. In this area an un- <br /> <br />named tributary (Location 4, Table 1) is thought to have produced <br /> <br />6,305 c.s,m. with an estimated peak velocity as high as 45 f.p.s. Long <br /> <br />Gulch, (Location 5, Table 1) which we will visit on the field trip, has <br /> <br />an estimated peak unit area discharge of 9,246 c.s.m. The Big Thompson <br /> <br />21 <br />
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