<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 />
|