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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.
Movement on faults can be a combination of dip-slip and strike-slip. Pure dip-slip faults can be normal (h/wall down) or reverse (h/wall up). Pure strike-slip faults can be dextral (right-lateral) or sinistral (left-lateral). Oblique-slip faults combine dip-slip and strike-slip components.Net slip = displacement on a fault, measured in the plane of the fault.) Classification. Fault rocks are classified according to the size of the fragments, and whether they are cohesive or not. If cemented by minerals precipitated from circulating groundwater it is an indurated gouge. Cataclasite: Cohesive fault rocks composed of broken, crushed and rolled grains.