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The Hosgri Fault zone is located near the coast of Southern California which is completely offshore. It is a reverse and thrust fault. Its last major earthquake occured in 1927 with a magnitude of 7.3. <ref>http://www.data.scec.org/fault_index/hosgri.html</ref> |
The Hosgri Fault zone is located near the coast of Southern California which is completely offshore. It is a reverse and thrust fault. Its last major earthquake occured in 1927 with a magnitude of 7.3. <ref>http://www.data.scec.org/fault_index/hosgri.html</ref> |
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[[Image:Flat eq map anotated.png|thumb|right|300px|This fault is shown in white and is the rightmost fault]] |
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The '''Clayton-Marsh Creek-Greenville Fault''' is located in the eastern [[San Francisco Bay Area]] of [[California]]. It is part of the somewhat parallel system of faults that are secondary to the [[San Andreas Fault]]. The 5.8 magnitude 1980 [[Livermore, California|Livermore]] [[earthquake]] occurred on this [[fault (geology)|fault]]. |
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[[Image:Eq-prob.jpg|thumb|left|150px|Probability map]] |
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== References == |
== References == |
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Revision as of 21:20, 13 October 2009
The Hosgri Fault zone is located near the coast of Southern California which is completely offshore. It is a reverse and thrust fault. Its last major earthquake occured in 1927 with a magnitude of 7.3. [1]
The Clayton-Marsh Creek-Greenville Fault is located in the eastern San Francisco Bay Area of California. It is part of the somewhat parallel system of faults that are secondary to the San Andreas Fault. The 5.8 magnitude 1980 Livermore earthquake occurred on this fault.
