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Updated live from Wikipedia, last check: May 28, 2012 21:59 UTC (43 seconds ago)

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2007 Alum Rock earthquake
Date October 30, 2007 (2007-10-30)
Magnitude 5.6 Mw
Depth 5.7 miles (9 km)
Epicenter location 37°25′55″N 121°46′34″W / 37.432°N 121.776°W / 37.432; -121.776Coordinates: 37°25′55″N 121°46′34″W / 37.432°N 121.776°W / 37.432; -121.776
Countries/
regions affected
 United States
Casualties none

The 2007 Alum Rock earthquake occurred on October 30, 2007 at approximately 8:04 p.m. PDT (October 31, 3:04 a.m. UTC)[1] in the San Jose area in California. It measured 5.6 on the moment magnitude scale and had a depth of 5.7 miles (9.2 km).[2]

The Alum Rock earthquake was the largest in the San Francisco Bay Area since the 1989 Loma Prieta earthquake, which measured 6.9 on the moment magnitude scale. Ground shaking from the Alum Rock quake reached San Francisco and Oakland and other points further north. ElarmS, an earthquake early warning system, accurately predicted the quake seconds before it struck, correctly estimating the quake's magnitude to within 0.5 magnitude units using only three to four seconds worth of data. Scientists with the California Integrated Seismic Network hope to refine the system to provide a 10-second warning in a similar quake to residents of Oakland and San Francisco.[3]

Contents

Geology

The quake occurred about 8–9 kilometers (about 5 miles) underground on the Calaveras Fault. The event caused moderate shaking in the epicentral region with over 60,000 felt reports, existing far beyond Santa Rosa. Based on the distance between aftershocks to the hypocenter, focal mechanisms, and moment tensor solutions, the earthquake ruptured an area of the fault for a length of about 5 km (3 miles), starting at the hypocenter and extending southeast. However, scientists found no surface trace of the earthquake along the fault.[4]

Damage

The earthquake caused minor damage, such as knocking things off of shelves, but caused no casualties. The shaking was felt as far north as Eugene, Oregon. Some parts of the area felt the rupture for up to 15 seconds. David Oppenheimer, a seismologist at the United States Geological Survey (USGS), said that although the quake was felt as a strong jolt over a wide region, it was more significant because it caused stress changes in the Calaveras Fault and the nearby Hayward Fault.[5]

See also

References








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