Effects of local geology on ground motion near San Francisco Bay

Bulletin of the Seismological Society of America
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Abstract

Measurements of ground motion generated by nuclear explosions in Nevada were made for 37 locations near San Francisco Bay, California. The results were compared with the San Francisco 1906 earthquake intensities and the strong-motion recordings of the San Francisco earthquake of March 22, 1957. The recordings show marked amplitude variations which are related consistently to the geologic setting of the recording site. For sites underlain by a layer of younger bay mud or artificial fill, maximum horizontal ground velocities generally increased with thickness of the layer and were as much as ten times greater than those recorded on nearby bedrock. The maximum vertical velocities for these sites were between 1 and 3.5 times greater. Spectral amplification curves clearly define a “dominant ground period” of about 1 second for sites underlain by younger bay mud. For sites underlain by older, more consolidated sediments, no clearly defined “dominant ground period” was found. Maximum ground velocities for the older bay sediment sites were about twice those recorded on bedrock.

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Publication type Article
Publication Subtype Journal Article
Title Effects of local geology on ground motion near San Francisco Bay
Series title Bulletin of the Seismological Society of America
DOI 10.1785/BSSA0600010029
Volume 60
Issue 1
Year Published 1970
Language English
Publisher Seismological Society of America
Contributing office(s) Earthquake Hazards Program
Description 33 p.
First page 29
Last page 61
Country United States
State California
City San Francisco
Other Geospatial San Francisco Bay
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