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Geology; September 2000; v. 28; no. 9; p. 803-806; DOI: 10.1130/0091-7613(2000)28<803:EEADIT>2.0.CO;2
© 2000 Geological Society of America
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Erosional equilibrium and disequilibrium in the Sierra Nevada, inferred from cosmogenic 26Al and 10Be in alluvial sediment

Clifford S. Riebe*,1, James W. Kirchner*,1, Darryl E. Granger*,2 and Robert C. Finkel*,3

1 Department of Earth and Planetary Science, University of California, Berkeley, California 94720-4767, USA
2 PRIME Lab and Department of Earth and Atmospheric Sciences, Purdue University, West Lafayette, Indiana 47907-1397, USA
3 Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory, Livermore, California 94551-9900, USA

We used cosmogenic 26Al and 10Be in stream sediment to measure landscape-scale erosion rates for topographically diverse catchments at seven Sierra Nevada sites. At three sites, erosion rates and hillslope gradients are strongly correlated, increasing with proximity to fault scarps and river canyons, which appear to have accelerated local base-level lowering rates, and thus increased catchment erosion rates by up to 15-fold. At four other sites, far from fault scarps and river canyons, erosion rates are much more uniform and less sensitive to average hillslope gradient. Our measurements show that contrasts in landscape erosion rates cannot be inferred from hillslope gradients alone, because landscapes can evolve toward a state of erosional equilibrium, in which steep and gentle slopes erode at similar rates.

Key Words: cosmogenic nuclides • erosion rates • landscape evolution




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