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<br />6 <br /> <br />z. Ground water studies by Carpenter, et. a1. (1995) have shown that <br />the volume of water stored in the beaches, river stage <br />fluctuation, and downramp rates are controlling the dynamics of <br />the ground water return flow and seepage erosion. <br /> <br />3. Rill erosion studies performed by the National Park Service <br />(Werre11, et. a1, 1993) have shown that the rate of decline in <br />river stage induces water trapped in the sediment to cut away at <br />beach faces. <br /> <br />4. The Smith and Wiele (1994) model showed that the higher upramp <br />wave would be attenuated by lower Marble Canyon and therefore no <br />impact would be found downstream. <br /> <br />Therefore, it was concluded that as long as the down ramp rate is maintained at <br />1,500 cfs/hr and the daily fluctuation is limited to between 5,000 cfs and <br />8,000 cfs per day, the upramp rate could be changed with no anticipated impact <br />on the sediment resources. <br /> <br />Increases in the release rate and corresponding increase in river stage tend <br />to increase available habitat for fish. The rate of increase is likely to <br />have no effect on the aquatic ecosystem. There should be no impacts to the <br />biological resources below lower Marble Canyon as a result of the increase in <br />ramping rates because the effects will be largely attenuated prior to reaching <br />lower Marble Canyon. All size classes of trout and native fish should be able <br />to accommodate the increase. Since upramp rates are not related to beach <br />erosion, no impacts are anticipated to occur to riparian areas or terrestrial <br />populations associated with the near shore environment. <br /> <br />Cultural resources depend on the sediment resource. Since the increase in the <br />upramp rate would not negatively effect the sediment resource, it would not <br />impact the cultural resources contained within the sediment deposits. <br /> <br />The impacts of increasing the upramp rate on recreation resources below Glen <br />Canyon Dam are also expected to be minimal. Effects on boating operations <br />have not been linked to upramp rates. Boating operations are still linked to <br />changes in river stage and minimum flows. Based on Table Z, the safety <br />effects on wading anglers should be minimal. As shown, increasing the upramp <br />rate from 2,500 cfs/hr to 4,000 cfs/hr results in a stage change of 0.66 .feet <br />(8 inches) more per hour. While this additional change in stage will be <br />noticeable, it is unlikely to result in a difference in the rate of wading <br />mishaps.It is important, however, that anglers be well informed about ramping <br />rates to reduce any potential safety related impacts. <br />