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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 /> <br />I <br /> <br />I <br /> <br />GEOMORPHOLOGY OF GEOLOGIC HAZARDS IN THE BIG THOMPSON <br />CANYON AREA, LARIMER COUNTY, COLORADO <br /> <br />I <br /> <br />James M. Soule <br />Colorado Geological Survey <br />1313 Sherman Street <br />Denver, Colorado 80203 <br /> <br />I <br /> <br />Introduction <br /> <br />I <br /> <br />Slope inclination, aspect, rock type and local meteorology appear to <br /> <br />be the dominant influences on modern geomorphic processes in the Big <br /> <br />I <br /> <br />Thompson Canyon area and in other similarly situated canyons of the Colo- <br /> <br />rado Front Range. This preliminary report describes several physical <br /> <br />I <br /> <br />attributes of this mountain landscape as they relate to actual and potential <br /> <br />I <br /> <br />geologic hazards. Current studies by the Colorado Geological Survey and the <br /> <br />U. S. Geological Survey to investigate hazardous geomorphic processes in the <br /> <br />I <br /> <br />Big Thompson Canyon and delineate geologic hazard areas are underway. This <br /> <br />work should assist in planning the safe restoration of the Big Thompson <br /> <br />I <br /> <br />Canyon area in the aftermath of recent flooding on July 31 - August 1, 1976. <br /> <br />I <br /> <br />This work is also intended to serve as a model planning guide for other <br /> <br />Front Range canyons. <br /> <br />I <br /> <br />The Big Thompson River and its tributaries are deeply incised into Pre- <br /> <br />cambrian crystalline and metamorphic rocks. Composition of this terrain <br /> <br />I <br /> <br />varies from tonalite and granodiorite to biotite-staurolite-grade metamorphic <br /> <br />I <br /> <br />rocks and amphibolite (Braddock and others, 1970). Weathering and disinte- <br />1 <br />gration of bedrock usually form a thin grus mantle on gentle to moderate <br /> <br />I <br /> <br />granitic slopes. Steeper slopes on these crystalline rocks commonly are <br /> <br />strewn with boulder rubble and are nearly barren of vegetation, especially <br /> <br />I <br /> <br />I <br /> <br />1 <br />As used in this paper, slope modifiers are defined as follows: <br />Very gentle slope: less than one percent (slope) <br />Very gentle to gentle slope: 1 to 5 percent <br />Gentle to moderate slope: 5 to 15 percent <br />Moderate to steep slope: 15 to 30 percent <br />Steep slope: greater than 30 percent <br />Very steep slope: much greater than 30 percent <br /> <br />I <br /> <br />25 <br />
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