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Explore the stratigraphic column of La Brea Smilodon and the significant 1868 Hayward earthquake, highlighting its impact and the Transcurrent strike-slip fault concept.
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The 1868 Hayward earthquake (M7.0) is about twice as large as the model for the southern segment earthquake (M6.7). • Hayward Fault is a NW trending, predominantly right-lateral strike-slip fault zone http://earthquake.usgs.gov/regional/nca/1868/
Transcurrent=strike slip From Tuzo Wilson (of the Wilson cycle)