The last major earthquake on this fault was a … Other articles where Strike-slip fault is discussed: fault: Strike-slip (also called transcurrent, wrench, or lateral) faults are similarly caused by horizontal compression, but they release their energy by rock displacement in a horizontal direction almost parallel to the compressional force.

is built across a fault, the ground displacement during an earthquake could seriously damage or rip apart that structure.

Nearly all transform faults are in the deep sea, but the major ones on land are noteworthy and dangerous, such as the Haiti Earthquake of 2010 . The U.S. Geological Survey describes the Hayward Fault as “the single most urbanized earthquake fault in the United States.” Picture via Temblor According to the U.S. Geological Survey, the average rate of creep on the Hayward is 4.6 millimetres per year or about the length of a standard black garden ant, or a quarter of a jelly bean. The Hayward Fault trends to the northwest within the East Bay, extending from San Pablo Bay in Richmond, 60 miles south to San Jose. Most earthquakes are associated with the San Andreas, Hayward, Calaveras, and Concord-Green Valley Faults. We present evidence for recurrence intervals of large earthquakes on the southern Hayward fault at Tyson’s La-goon, also called Tule Pond, a large (0.8 km 0.15 km) sag pond formed in a right step in the fault (Figs. Although large earthquakes on the Hayward Fault have been rare since 1868, a large earthquake could occur on the Hayward fault over the planning period. Determination of earthquake recurrence from geologic evi-dence of past large earthquakes is essential for improving The city of Ukiah, in Northern California sits right next to the Maacama Fault, which is capable of M=7.5 earthquakes and poses a significant threat to the region. 1, 2). A major earthquake along the Hayward fault, together with related landslides, fires, and floods, could have a catastrophic effect in Fremont.

active fault lines in the vicinity. The fault plane is essentially vertical, and the relative slip is lateral along… (Photo from: Trulia) In California, when most people think about faults, their thoughts are immediately drawn to the San Andreas, and to a lesser extent, the Hayward Fault.

The last time it broke was in 1868 when a magnitude 6.8 struck, killing 30 people. Earthquake science was still young, but the architects apparently realized that the Hayward is a fault, where two pieces of crust move past each other. If a structure (a building, road, etc.) The Hayward Fault is located 1.6 miles east of the city and is the closest active fault to Albany. From the televised scenes of the damage caused by the 7.2-magnitude earthquake that struck Kobe, Japan, on 16 January 1995, Bay Area residents saw the possible devastation that could occur if a comparable size earthquake were to strike along the Hayward Fault. The Hayward Fault extends for 62 miles from San Jose to San Pablo Bay, passing through Berkeley and Oakland.

This article raises awareness of earthquake potentials in California which has 99.7% probability of having a moderate-to-large earthquake during the next 30 years.

The Hayward fault is a transform or strike-slip fault that moves sideways, rather than the more common faults that move up on one side and down on the other.