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Science 20 June 1975: Vol. 188. no. 4194, pp. 1207 - 1208 DOI: 10.1126/science.188.4194.1207
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Articles
Denudation Studies: Can We Assume Stream Steady State?
Stanley W. Trimble 1
1 Department of Geography, University of Wisconsin, Milwaukee 53201
Contemporary stream sediment loads are dubious indicators of regional denudation. Recent analysis of ten river basins in the southeastern United States indicates that of the material eroded from upland slopes since European settlement, only about 5 percent has been exported. The remainder, alluvium and colluvium, will probably not be exported because of extensive reservoir impoundments.
THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
- Happ, S.C., Rittenhouse, G. and Dobson, G.C. 1940: Some principles of accelerated stream and valley sedimentation. US Department of Agriculture Technical Bulletin 695.
- S. W. Trimble (2008)
Progress in Physical Geography
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- The use of historical data and artifacts in geomorphology.
- S. W. Trimble (2008)
Progress in Physical Geography
32, 3-29
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- The sediment delivery problem revisited.
- J. de Vente, J. Poesen, M. Arabkhedri, and G. Verstraeten (2007)
Progress in Physical Geography
31, 155-178
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- Classics in physical geography revisited.
- J. Boardman (2001)
Progress in Physical Geography
25, 261-266
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- Decreased Rates of Alluvial Sediment Storage in the Coon Creek Basin, Wisconsin, 1975-93.
- S. W. Trimble (1999)
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285, 1244-1246
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- Contribution of Stream Channel Erosion to Sediment Yield from an Urbanizing Watershed.
- S. W. Trimble (1997)
Science
278, 1442-1444
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- Equilibrium and response to climatic and tectonic forcing: A study of alluvial sequences in the Devonian Munster Basin, Ireland.
- S. B. Kelly and S. P. Sadler (1995)
Geological Society, London, Special Publications
85, 19-36
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- Contemporary erosion of the Canadian landscape.
- P. Ashmore and P. Ashmore (1993)
Progress in Physical Geography
17, 190-204
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- Changes in Sediment Storage in the Coon Creek Basin, Driftless Area, Wisconsin, 1853 to 1975.
- S. W. Trimble and S. W. TRIMBLE (1981)
Science
214, 181-183
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