Affiliation:
1. Department of Earth and Planetary Sciences, University of California, Santa Cruz, CA, USA.
Abstract
The limits of channel offset
The offset of stream channels across a strike-slip fault offer a record of long-term slip rates. The process itself is an interesting case of landscape evolution because the streams will spill straight across the fault at some point and reset the offset. Dascher-Cousineau
et al.
developed a model for this process that they validated using observations from the Carrizo Plain in California. The model leverages transitions from active to abandoned stream channels to determine when and how drainage networks in these regions reorganize and allow quantification of both slip and bedload transport.
Science
, abf2320, this issue p.
204
Funder
National Aeronautics and Space Administration
U.S. Geological Survey
Southern California Earthquake Center
Publisher
American Association for the Advancement of Science (AAAS)
Reference32 articles.
1. A. C. Lawson The California Earthquake of April 18 1906 (Carnegie Institution of Washington 1908).
2. R. E. Wallace “Notes on stream channels offset by the San Andreas fault southern Coast Ranges California” (1968).10.1017/CBO9781107415324.004
3. Slip along the San Andreas fault associated with the earthquake;Sieh K. E.;Bull. Seismol. Soc. Am.,1978
4. Holocene activity of the San Andreas fault at Wallace Creek, California
5. Slip in the 1857 and Earlier Large Earthquakes Along the Carrizo Plain, San Andreas Fault
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