Reevaluating Late-Pleistocene and Holocene Active Faults in the Tahoe Basin, California-Nevada
CHAPTER 42 Reevaluating Late-Pleistocene and Holocene Active Faults in the Tahoe Basin, California-Nevada Graham Kent Nevada Seismological Laboratory, University of Nevada, Reno, Reno, Nevada 89557-0174, USA Gretchen Schmauder Nevada Seismological Laboratory, University of Nevada, Reno, Reno, Nevada 89557-0174, USA Now at: Geometrics, 2190 Fortune Drive, San Jose, California 95131, USA Jillian Maloney Department of Geological Sciences, San Diego State University, San Diego, California 92018, USA Neal Driscoll Scripps Institution of Oceanography, University of California, San Diego, 9500 Gilman Drive, La Jolla, California 92093, USA Annie Kell Nevada Seismological Laboratory, University of Nevada, Reno, Reno, Nevada 89557-0174, USA Ken Smith Nevada Seismological Laboratory, University of Nevada, Reno, Reno, Nevada 89557-0174, USA Rob Baskin U.S. Geological Survey, West Valley City, Utah 84119, USA Gordon Seitz &DOLIRUQLD*HRORJLFDO6XUYH\0LGGOH¿HOG5RDG060HQOR3DUN California 94025, USA ABSTRACT the bare earth; the vertical accuracy of this dataset approaches 3.5 centimeters. The combined lateral A reevaluation of active faulting across the Tahoe and vertical resolution has rened the landward basin was conducted using a combination of air- identication of fault scarps associated with the borne LiDAR (Light Detection and Ranging) three major active fault zones in the Tahoe basin: imagery, high-resolution seismic CHIRP (acous- the West Tahoe–Dollar Point fault, Stateline–North tic variant, compressed high intensity radar pulse) Tahoe fault, and Incline Village fault. By using the proles, and multibeam bathymetric mapping. In airborne LiDAR dataset, we were able to identify August 2010, the Tahoe Regional Planning Agency previously unmapped fault segments throughout (TRPA) collected 941 square kilometers of airborne the Tahoe basin, which heretofore were difcult LiDAR data in the Tahoe basin.
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