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<br />58 <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />II <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 />sand at elevations above the 3l,500 cfs level if sand <br />is in sufficient supply, initiation of fluctuating <br />flows or lower steady flows after these floods will <br />cause loss of the newly-deposited sand throughout the <br />canyon. Loss will be greatest in narrow reaches, <br />where competition for campsites is keenest. <br />Redistribution of sand by fluctuating flow may reduce <br />the area and depth of backwaters. (See Appendix A, <br />Section II.) <br /> <br />IMPACT OF YEAR - ROUND FLUCTUATIONS <br />ON RESOURCES <br /> <br /> CRITICAL RESOURCES <br /> NOTive Trout Trout WW Terres. <br />Chub Fish Repro/Grow Fishi~ Booting Beoches Habitat <br />0 - v: - - - 0 <br /> <br />Figure VI-7. Fluctuations have adverse impacts (-) <br />primarily on the aquatic resources and recreation. <br />They have no significant impact (0) on terrestrial <br />resources and chub, and benefit (+) trout growth. <br /> <br />Flood Releases Have Greatest Potential For <br />Long-Term And Irreversible Impacts <br /> <br />Of the operations evaluated, flooding has the greatest <br />potential to irreversibly impact the Colorado River in <br />Grand Canyon. Flooding was a natural and consistent <br />aspect of pre-dam flows. However, the large amounts <br />of sediment carried by pre-dam flows allowed renewal of <br />beaches and substrate for vegetation. Loss of beaches, <br />sand substrate, and marshes may be nearly irreversible <br />