NOTE: Text or symbols not renderable in plain ASCII are indicated by [...]. Abstract is included in .pdf document. The Garlock fault is one of the major active faults in California. Although it has not produced any large earthquakes during historic times, abundant fault scarps in Holocene deposits and offset geomorphic features attest to the oc...

NOTE: Text or symbols not renderable in plain ASCII are indicated by [...]. Abstract is included in .pdf document. The Garlock fault is one of the major active faults in California. Although it has not produced any large earthquakes during historic times, abundant fault scarps in Holocene deposits and offset geomorphic features attest to the oc...

NOTE: Text or symbols not renderable in plain ASCII are indicated by [...]. Abstract is included in .pdf document. The Garlock fault is one of the major active faults in California. Although it has not produced any large earthquakes during historic times, abundant fault scarps in Holocene deposits and offset geomorphic features attest to the oc...

NOTE: Text or symbols not renderable in plain ASCII are indicated by [...]. Abstract is included in .pdf document. The Garlock fault is one of the major active faults in California. Although it has not produced any large earthquakes during historic times, abundant fault scarps in Holocene deposits and offset geomorphic features attest to the oc...

NOTE: Text or symbols not renderable in plain ASCII are indicated by [...]. Abstract is included in .pdf document. The Garlock fault is one of the major active faults in California. Although it has not produced any large earthquakes during historic times, abundant fault scarps in Holocene deposits and offset geomorphic features attest to the oc...

The northern segment of the San Andreas fault last ruptured in 1906, producing the great San Francisco earthquake. This study involves the collection and interpretation of geologic data from the segment of the northern San Andreas fault near Point Arena, California, to determine the recurrence interval and slip rate of this segment of the fault....

The northern segment of the San Andreas fault last ruptured in 1906, producing the great San Francisco earthquake. This study involves the collection and interpretation of geologic data from the segment of the northern San Andreas fault near Point Arena, California, to determine the recurrence interval and slip rate of this segment of the fault....

The northern segment of the San Andreas fault last ruptured in 1906, producing the great San Francisco earthquake. This study involves the collection and interpretation of geologic data from the segment of the northern San Andreas fault near Point Arena, California, to determine the recurrence interval and slip rate of this segment of the fault....

The northern segment of the San Andreas fault last ruptured in 1906, producing the great San Francisco earthquake. This study involves the collection and interpretation of geologic data from the segment of the northern San Andreas fault near Point Arena, California, to determine the recurrence interval and slip rate of this segment of the fault....

Geologic mapping provides structural and stratigraphic observations which lead to new insights into the magnitude, timing, and rate of Cenozoic extensional tectonism in the Death Valley region of the Basin and Range province in the western United States. Detailed mapping of the Grapevine Mountains, in northeastern Death Valley, yields new infor...