The most common fault type in California is the strike-slip fault type (like the San Andreas fault and the Hayward fault), followed by the thrust fault type (Cascadia fault). It comes just over four months after a 4.4 magnitude quake along the fault near Berkeley. Technically speaking, the Hayward is a right-lateral strike-slip fault. The Hayward fault is an extremely interesting feature of the East Bay and you can see its footprints all over the place once you know where and how to look. On Monday evening (May 14), there was a 3.5 magnitude earthquake along the fault centered just east of Oakland. If that is the case, the longer fault system could produce larger temblors. However, many scientists believe that the Hayward Fault is connected to the Calaveras Fault to the south, the Rodgers Creek Fault to the north and to the Maacama Fault still farther north. Take a look at the The Hayward Fault Zone and Traces Map to examine where the Hayward Fault runs through our City. The San Andreas fault system is to the west, the Garlock fault is to the south and the faults of the Sierra Nevada are to the east. The Hayward Fault is thought capable of generating a magnitude 7.5 quake. White lines are ⦠In a thrust type fault, the earth on one side of the fault slips upward on top of the adjacent side of the fault. The Hayward fault is a 90 kilometer long crack in the Earth's crust that travels through the San Francisco Bay area. For more information, please call Planning at ⦠Its last major rupture occurred in 1868, during California's frontier days, and was the original "Great San Francisco Earthquake" until 1906.. When it ruptures, the Hayward Fault will do more than damage homes, zoos and football stadiums: It will endanger numerous lives and likely deal a devastating economic blow. The Hayward Fault runs through the East Bay from San Pablo Bay in the north The San Andreas fault system is the major geologic boundary between the North American and Pacific tectonic plates and passes through much of the state. The Hayward Fault may be less well-known than the San Andreas Fault, but seismologists now call it a time bomb that could kill nearly a 1,000 people and injure tens of thousands more. The Hayward Fault is restless. The mainshock begins beneath the City of Oakland (star) and causes the Hayward Fault to rupture along about 52 miles of its length (thick black line). Since then, nearly three million people have moved next to the Hayward fault with little regard for its earthquake potential. This sends a vertical force into the surrounding areas. The Hayward Fault, a long and lethal crack in the Earth, slices along the base of the Berkeley Hills and directly through the University of California. This website offers three ways of viewing new USGS mapping of active traces of the Hayward fault.
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