Tectonic geomorphic markers such as deflected and offset stream channels form the basis for paleoseismic studies that aim to understand the spatiotemporal distribution of earthquakes, their magnitudes, and recurrences. This terrestrial laser scanning dataset includes a scanned stream channel that was deflected by the San Andreas Fault in the Carrizo Plain, California.
Data acquisition was supported by NSF grants(EAR-0651098, EAR-0711282, and EAR-0930643), the US Geological Survey (USGS), and the Southern California Earthquake Center (SCEC)
Citation: null Accessed: 2019-12-11
Dataset Keywords: San Andreas Fault, Bidart, California, paleoseismic, TLS