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1906 San Francisco earthquake

Earthquake in California

  • 27 min read
  • 11 chapters
San Francisco Earthquake of 1906: Ruins in vicinity of Post and Grant Avenue. Looking northeast.
Chadwick, H. D · Public domain

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Through Earthquake, Tectonics and Fault (geology)

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).

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