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Floodplain Information Report Volume 3 Gunnison River from Delta to the Confluence with the Colorado River
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Floodplain Information Report Volume 3 Gunnison River from Delta to the Confluence with the Colorado River
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Last modified
8/2/2012 8:47:30 AM
Creation date
7/26/2012 11:50:17 AM
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Template:
Floodplain Documents
Basin
Gunnison
Colorado Mainstem
Title
Floodplain Information Report Volume 3 Gunnison River from Delta to the Confluence with the Colorado River
Date
3/1/1995
Prepared For
The Recovery Implementaiton Program for Endangered Fish Species in the Upper Colorado River Basin
Prepared By
CWCB
Floodplain - Doc Type
Floodplain Report/Masterplan
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■ 5.0 INTERPRETATION OF THIS REPORT <br />5.1 Hydrologic Findings <br />The results of the hydrologic analysis for the Gunnison River are considered accurate. They are <br />' based in part on existing approved data from detailed studies at the upstream and downstream <br />limits of the study reach. The existing data demonstrate a linear relationship of peak flow versus <br />drainage area for the study reach. <br />5.2 Hydraulic Findings <br />The hydraulic methods used for this study are the same used in more detailed studies and much <br />more detailed than the typical approximate studies. The 100 -year flood depths range from 11.6 <br />feet in a medium reach of the river to 17.3 feet near the downstream limit of the study. The <br />flood depths are generally consistent throughout the study reach with differences of only a few <br />feet (12 -17 feet for the 100 -year flow depths). <br />' 5.3 Floodplain Delineations <br />The primary difficulty in presenting precise delineation of the 50 -year and 100 -year floodplains <br />was the limited quality of the available base mapping for the lower Gunnison River. Using <br />USGS topographic quadrangle maps at contour intervals of 20 or 40 feet to portray flood lines <br />' in unsurveyed areas provides limited information. The margin for interpretation is very great, <br />especially in medium to wide reaches of the river where contours are widely spaced. More <br />detailed techniques will be necessary in areas of interest. <br />This study can be utilized to prepare more detailed floodplain delineations in such areas of <br />specific interest. Those who are interested in greater detail have three choices for using this <br />study: <br />1) They can refer to the detailed study information for the upstream stream reach near Delta; <br />2) They can rely on the hydrologic determinations and use other topographic information and <br />hydraulic models; or <br />3) They can use the depth calculations with other topographic information from field surveys <br />or other maps. <br />20 <br />
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