The 1906 San Francisco earthquake was a major earthquake which struck the coast of Northern California at 05:12 am Pacific Standard Time on Wednesday, April 18, 1906. With an estimated moment magnitude of 7.9 and a maximum Mercalli intensity of XI (Extreme), it created high-intensity shaking from Eureka on the North Coast to the Salinas Valley, an agricultural region to the south of the San Francisco Bay Area.

Extensive fires soon broke out in San Francisco and lasted for several days. More than 3,000 people died and over 80% of the city was destroyed. The event is remembered as the deadliest earthquake in the history of the United States. The death toll remains the greatest loss of life from a natural disaster in California's history and high on the list of worst American disasters, natural or man-made.

Tectonic setting

The San Andreas Fault is a continental transform fault that forms part of the tectonic boundary between the Pacific plate and the North American plate. The strike-slip fault is characterized by mainly lateral motion in a dextral sense, where the western (Pacific) plate moves northward relative to the eastern (North American) plate. This fault runs the length of California from the Salton Sea in the south to Cape Mendocino in the north, a distance of about 810 miles (1,300 km). The maximum observed surface displacement was about 20 feet (6 m); geodetic measurements show displacements of up to 28 feet (8.5 m).

1906 San Francisco earthquake
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Earthquake

The 1906 earthquake preceded the development of the Richter scale. The most widely accepted estimate for the magnitude of the quake on the modern moment magnitude scale is 7.9; values from 7.7 to as high as 8.3 have been proposed. According to findings published in the Journal of Geophysical Research, severe deformations in the Earth's crust took place both before and after the earthquake's impact. Accumulated strain on the faults in the system was relieved during the earthquake, which is the supposed cause of the damage along the 280-mile-long (450 km) segment of the San Andreas plate boundary. The 1906 rupture propagated both northward and southward for a total of 296 miles (476 km). Shaking was felt from Oregon to Los Angeles, and as far inland as central Nevada.