NEW LINKAGE OF THE ARROW CANYON RANGE AND WILDCAT WASH FAULTS, SOUTHERN NEVADA: IMPLICATIONS FOR SEISMIC HAZARDS
We tested the hypothesis that the faults have late Quaternary surface ruptures and the fault tips underlap with no strain transfer using new data from detailed field mapping, topographic profiling and logging of natural dissections. Map data, topographic profiles, and logs of natural dissections document fault scarps that cut Quaternary alluvial fans and terrace deposits. The oldest alluvial fan surfaces are offset as much as 30 m. Younger fan surfaces and terraces are offset up to 3 m. Three natural dissections across the WWF range in depth from 3 to 5 m and show at least three colluvial wedges indicating at least that many surface rupturing earthquakes. Map data show that the ACRF and WWF have overlapping fault tips with immature strain transfer between them. The fault tips overlap by at least 0.5 km and are spaced ~1 km apart across strike. The area between the overlapping fault tips contains reverse faults and a broad, gentle fold which suggest the initiation of a relay ramp and the beginning of strain transfer between the faults. Consequently, the faults appear to be in an early stage of linkage. This early linkage of these two young faults has profound implications for seismic hazards to communities in southern Nevada. Linkage increases the total fault length, and thus, the potential rupture length. Therefore, the largest possible earthquake magnitude that may occur along the combined ACRF and WWF is greater than on either individual fault.