movement along the san andreas fault in this are is by fits and starts the last large earthquake here in 1857 was the result of 9.5 m of instantaneous slip. the average slip rate of the fault can be determined for two periods in the wallace creek area, because two channels of wallace creek are displaced by the fault and the time when the channels first formed is known. calculate the two slip rates by measuring the offset across the fault for both channels
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movement along the san andreas fault in this are is by fits and starts the last large earthquake her...
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