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USGS · 70045110

Grizzly Valley fault system, Sierra Valley, CA

Abstract

The Grizzly Valley fault system (GVFS) strikes northwestward across Sierra Valley, California and is part of a network of active, dextral strike-slip faults in the northern Walker Lane (Figure 1). To investigate Quaternary motion across the GVFS, we analyzed high-resolution (0.25 m) airborne LiDAR data (Figure 2) in combination with six, high-resolution, P-wave, seismic-reflection profiles [Gold and others, 2012]. The 0.5- to 2.0-km-long seismic-reflection profiles were sited orthogonal to suspected tectonic lineaments identified from previous mapping and our analysis of airborne LiDAR data. To image the upper 400–700 m of subsurface stratigraphy of Sierra Valley (Figure 3), we used a 230-kg accelerated weight drop source. Geophone spacing ranged from 2 to 5 m and shots were co-located with the geophones. The profiles reveal a highly reflective, deformed basal marker that we interpret to be the top of Tertiary volcanic rocks, overlain by a 120- to 300-m-thick suite of subhorizontal reflectors we interpret as Plio-Pleistocene lacustrine deposits. Three profiles image the principle active trace of the GVFS, which is a steeply dipping fault zone that offsets the volcanic rocks and the basin fill (Figures 4 & 5).

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90° N90° S · 180° W ← longitude → 180° E
Source-reported bounding extent: 39.58134870630412° to 39.8739115680129° latitude; -120.50491333007811° to -120.02014160156249° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Ryan Gold, William Stephenson, Jack Odum, Rich Briggs, Anthony Crone, Steve Angster. 2012. Grizzly Valley fault system, Sierra Valley, CA. https://pubs.usgs.gov/publication/70045110

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