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Geomorphic analysis of fault scarps and faulted surficial deposits allows for interpretation of late-Quaternary faulting on the Hilton Creek and Round Valley faults, two major range-front faults in the Sierra Nevada frontal fault system, as well as three faults on the north flank of the Coyote warp, a structure that separates the Round Valley fault from range-front faults to the south. Repeated movement...
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