Not all earthquakes result in surface rupture. The Loma Prieta Earthquake of 1989 caused major damage in the San Francisco Bay Area but the movement deep in the earth did not break through to the surface. Fault rupture almost always follows preexisting faults, which are zones of weakness. Rupture may occur suddenly during an earthquake or slowly in the form of fault creep. Sudden displacements are more damaging to structures because they are accompanied by shaking.
Fault creep is the slow rupture of the earth's crust.
Examples of creep are well known along the Hayward Fault where it crosses highly developed areas in Contra Costa and Alameda Counties. Although the Hayward Fault ruptured suddenly in the 1868 earthquake, it also exhibits slow surface creep which offsets and deforms curbs, streets, buildings, and other structures that lie on top of the fault. Earthquake Fault Zone maps can be studied at local planning departments or at offices of the Division of Mines and Geology. These maps show most streets, drainages, and other features. Local government may have already transferred Earthquake Fault Zone boundaries to parcel maps, so the relationship of the Zone to each parcel can easily be determined.