Climate-Modulated Channel Incision and Rupture History of the San Andreas Fault in the Carrizo Plain
The spatial and temporal distribution of fault slip is a critical parameter in earthquake source models. Previous geomorphic and geologic studies of channel offset along the Carrizo section of the south central San Andreas Fault assumed that channels form more frequently than earthquakes occur and suggested that repeated large-slip earthquakes similar to the 1857 Fort Tejon earthquake illustrate typical fault behavior. We found that offset channels in the Carrizo Plain incised less frequently than they were offset by earthquakes.
Grant Ludwig, L., Akciz, S.O., Noriega, G. R., Zielka, O., and Arrowsmith, J R., 2010. Climate modulated channel incision and rupture history of the San Andreas fault in the Carrizo Plain: Science, v. 327, p. 1117-111.
The Forest Service will host its remaining two public meetings in Queen Valley on October 8 and in Tempe on October 10.
Video & Materials
A video presentation – the same information introduced at each public meeting – as well as meeting materials (posters and newsletter) are available for public review.
Draft EIS Released
The Draft Environmental Impact Statement (DEIS) for the Resolution Copper Project and Land Exchange is now available for review under the 'EIS Info' tab.
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