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Updated February 28, 2017. The Hayward fault is a 90 kilometer long crack in the Earth's crust that travels through the San Francisco Bay area. Its last major rupture occurred in 1868, during California's frontier days, and was the original Great San Francisco Earthquake until 1906.
The motion along a strike-slip fault is parallel to the strike of the fault surface, and the fault blocks move sideways past each other. A strike-slip fault in which the block across the fault moves to the right is described as a dextral strike-slip fault. If it moves left, the relative motion is described as sinistral. Local deformation near bends in strike-slip faults can produce pull-apart basins and grabens.