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USGS · fs20083019

The Hayward Fault— Is it due for a repeat of the powerful 1868 earthquake?

Abstract

On October 21, 1868, a magnitude 6.8 earthquake struck the San Francisco Bay region. Although the region was then sparsely populated, this quake on the Hayward Fault was one of the most destructive in California's history. Recent studies show that such powerful Hayward Fault quakes have repeatedly jolted the region in the past. U.S. Geological Survey (USGS) scientists describe this fault as a tectonic time bomb, due anytime for another magnitude 6.8 to 7.0 earthquake. Because such a quake could cause hundreds of deaths, leave thousands homeless, and devastate the region's economy, the USGS and other organizations are working together with new urgency to help prepare Bay Area communities for this certain future quake.

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90° N90° S · 180° W ← longitude → 180° E
Source-reported bounding extent: 37.5° to 38° latitude; -122.4333° to -121.9167° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Thomas M. Brocher, Jack Boatwright, James J. Lienkaemper, Carol S. Prentice, David P. Schwartz, Howard Bundock. 2008. The Hayward Fault— Is it due for a repeat of the powerful 1868 earthquake?. https://doi.org/10.3133/fs20083019

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