Laserfiche WebLink
<br />as 'one possible solution; however, <br />"thip wo,uld require such a major <br />c:ommitment of resources that it <br />seems impractical at this time. <br />Therefore, we must face the reali- <br />zation that we have created a new <br />environment in the Grand Canyon <br />and that the physical and ecologi- <br />cal adjustments presently under- <br />way are inevitable. <br /> <br />The system is now so modified that <br />the earlier natural state can no <br />longer serve as the standard. For <br />this reason our focus should be on <br />the processes and rates of adjust- <br />ment to the new river regime. To <br />do this, new data and new investi- <br />gations are needed. In the mean- <br />time, however, the National Park <br />Service must face several difficult <br />decisions concerning regulation of <br />man's use of the river. If human <br />impact on the physical environ- <br />ment is high compared to the post- <br />dam degradation by fluvial and eo- <br />lian processes, then low quotas are <br />a certainty. If, on the other hand, <br />the human impact is low compared <br />to' the post-dam erosion rates, then <br />use may be restricted more by so- <br />cial concerns-for the quality of the <br />wilderness experience, for example <br />-than by environmental concerns. <br />Since 1970 the National Park Ser- <br />vice has, been limiting use of the <br />river to approximately 10,000 visi- <br />tors a year; this level is probably <br />the upper limit for the admittedly <br />subjective criterion of a true wilder- <br />ness experience. <br /> <br />Summary <br /> <br />The Colorado River in its natural <br />state often discharged more than <br />80,000 cfs and carried an average of <br />0.38 million tons of sand and silt a <br />day through the Grand Canyon. <br />This high water scoured the bottom <br />of the canyon and eroded and rede- <br />posited material on the river <br />shores, keeping the river channel <br />navigable for small boats and rafts. <br />In 1963, the river was impounded <br />by Glen Canyon Dam, and the <br />water released by the dam is a tur- <br />bid-free, powerful erosive agent. <br />Daily the discharge varies from <br />4,000 cfs to about 20,000 cfs, creat- <br />ing many effects and problems. <br /> <br />The sediment-free water erodes the <br />existing beach areas but does not <br />resupply the sand lost either to the <br />wind or directly into the river. The <br /> <br />reduced discharge is le.ss capable of <br />clearing the river channel of flash- <br />flood material brought in by tribu- <br />taries, thus creating hazardous rap- <br />ids and falls that may eventually <br />become unnavigable. Diurnal varia- <br />tion in the river's discharge has led <br />to ecological changes along the can- <br />yon bottom: exotic plants, for ex- <br />ample, are rapidly displacing indig- <br />enous species. Increased use of the <br />~river by man in recent years ap- <br />pears to be contributing to the ero- <br />sion problem; however, this impact <br />has not been quantified. <br /> <br />At this time the future of the river <br />bars and terraces is unclear. The <br />system is rapidly approaching a <br />new state at the present rate of <br />change; and it is clear that Emory <br />C. Kolb, one of the pioneer river- <br />men on the Colorado, was correct <br />when he said, "No one will ever <br />know the Colorado as it really was. <br />It's too late" (10). <br /> <br />References <br /> <br />1. Robert Wallace. 1972. The Grand Can- <br />yon: The American Wilderness. New <br />York: Time-Life Books, p. 23. <br /> <br />2. Mark A. Boster. 1972. Co Iura do River <br />Trips within the Grand Canyon Nation- <br />al Park and Monument: A Socioeco- <br />nomic Analysis. Technical Report on <br />Hydrology and Water Resources, Rept. <br />::10. Tucson: Univ. of Arizona, p. 24. <br />3. Kenneth W. Hamblin and J. Keith <br />Rigby. 1969. Guidebook to the Colorado <br />River, part 2. Brigham Young Univ. <br />Geologic Studies, vol. 16. Provo, Utah: <br />Brigham Young Univ., p. 24. <br />4: Luna B. Leopold. 1969. The rapids and <br />the pools: Grand Canyon. In The Colo- <br />rado River Region and John Wesley <br />Powell. Geological Survey Professional <br />Paper 669-D. Washington: U.S. Gov't. <br />Printing Office, p. 135. <br />5. W. O. Smith, C. P. Vetter, and G. B. <br />Cummings. 1960. Comprehensive Sur- <br />vey of Sedimentation in Lake Mead, <br />1948-1949. Geological Survey Profes- <br />sional Paper 295. Washington: U.S. <br />Gov't. Printing Office, p. 196. <br />6. David R. Harris. 1971. Recent plant <br />invasions in the arid and semi-arid <br />Southwest of the United States. In <br />Man's Impact on the Environment, <br />Thomas R. Detwyler, ea.. New York: <br />McGraw-Hili, pp. 469-70. <br />7. Ref.3,p.13. <br />8. U.S. Fish and Wildlife Service. 1973. <br />Threatened Wildlife of the United <br />States. Bureau of Sport Fisheries and <br />Wildlife, Resource Publ. 114. Washing. <br />ton: U.S. Gov't. Printing Office, p. 35. <br />9. Ref. 2, p. 35. <br />10. Ref. 1, p. 131. <br /> <br />1974 .July-August 401 <br /> <br /> <br />::::::..e: <br /> <br />f,':,':':':': <br /> <br />i........ <br />.._.,0.. <br />