Poster #056, Earthquake Geology
Assessment of the paleoseismic potential of the Ferrum site along the southernmost San Andreas fault using new UAV imagery, GPR data, and preliminary trenching
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Poster Presentation
2021 SCEC Annual Meeting, Poster #056, SCEC Contribution #11148 VIEW PDF
most recent event appears to have produced between 2 and 3.5 m of lateral slip, with lower overall lateral slip values where multiple strands are present. We also identify offset channels with up to ~7 meters of lateral deflection, which are interpreted as representing multiple (probably 2) events. A cluster of small-scale offsets was identified, generally with displacements of less than a meter but a few up to ~1.5 meters, which probably reflect displacement from creep that postdate the most recent lake and large earthquake event. Along with the UAV imagery interpretations, we acquired ground penetrating radar (GPR) data to map the upper several meters of the subsurface architecture of the fault zone and ponded alluvial sediment to examine stratigraphy and locate faults and fault-related deformation. Following the geophysical analysis, we excavated two 1.5-2 m deep trenches to collect samples for radiocarbon dating to constrain ages on shallow sediments, identify and date lake events, and to verify findings from the GPR surveys. The trenches revealed excellent stratigraphy and evidence for preservation of three or four lake deposits, along with several minor fault splays. The primary fault is located beneath thick dune deposits. We collected over 50 radiocarbon samples, all gastropod shells, representing nearly all stratigraphic units exposed in the trench walls to develop the site chronology and assess the site’s potential for dating earthquake events.
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