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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.
Strike-slip faults are usually vertical, while normal and reverse faults are often at an angle to the surface of the Earth. The different styles of faulting can also combine in a single event, with one fault moving in both a vertical and strike-slip motion during an earthquake.