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FLOOD09597
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Last modified
1/26/2010 10:09:49 AM
Creation date
10/5/2006 4:29:04 AM
Metadata
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Template:
Floodplain Documents
County
Gunnison
Community
Marble Area
Basin
Gunnison
Title
Engineering Geologic Factors of the Marble Area
Date
6/1/1972
Prepared For
Gunnison County
Prepared By
Colorado Geological Survey
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br />-23 ,~ <br /> <br />area. Hydrologic degradation would include both temporary and long- <br /> <br />term obstruction of the flood plain by debris that would, in the nor- <br /> <br />mal course of events, be deposited mostly in areas above the Crystal <br /> <br />River flood plain. Unfavorable side effects would include occasional <br /> <br />damming, and a general condition of backwater upstream from the dis- <br /> <br />charge point during flood flows of the Crystal River. Direct discharge <br />of the mudf10w debris in or near the river would greatly, increase the <br /> <br />sediment supply which could be expected to affect game fish, and the <br /> <br />general stream aesthetics in the downstream direction. If such a solu- <br /> <br />tion is proposed, it would almost certainly require approval from the <br /> <br />U.S. Forest Service, Colorado Division of Game, Fish and Parks, Colo- <br />rado Water Pollution Control Commission, and other interested agencies. <br /> <br />Debris Dams as Possible Solution <br /> <br />An alternative solution would consist of somewhat similar channel- <br /> <br />ization of Slate Creek, but with addition of debris dams or catchment <br /> <br />basins which would be designed to intercept and hold a large part of <br /> <br />the flood debris within retaining structures adjacent to the channel. <br /> <br />There are several complications with such a possible solution which has <br /> <br />been tested in parts of California and the Wasatch Front area of Utah. <br /> <br />The mudf10w events (not ordinary flood waters) are the basic problem, <br /> <br />and the solid matter ("sediment") content of these probably constitutes <br /> <br />70 to 75% of the mass, and nearly all of the volume. The "sediment" <br /> <br />volume is, therefore, roughly equal to the total flow of a mud flood <br /> <br />event. Although we have made no estimate of sediment production in <br /> <br /> <br />the Slate Creek drainage basin, it must be extremely high judging from <br /> <br /> <br />the rapid backwasting of Gallo Bluff and the sizeable and frequent <br /> <br /> <br />debris sheets deposited in the lower reaches of Slate Creek. <br />
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