1892 Laguna Salada earthquake
|Date||24 February 1892|
|Magnitude||7.1 – 7.2 Mw|
|Countries or regions||Mexico, USA|
|Max. intensity||X (Intense)|
The 1892 Laguna Salada earthquake occurred at 23:20 Pacific Standard Time on February 23 (07:20 UTC on February 24). It had an estimated magnitude of 7.1–7.2 on the moment magnitude scale and a maximum perceived intensity of X (Intense) on the Mercalli intensity scale. The earthquake takes its name from a large dry lake bed in Baja California, Mexico. There were no reported casualties, but the very large shock affected the largely-uninhabited areas of northern Mexico and southern California.
The Salton Trough is part of the complex plate boundary between the Pacific Plate and the North American Plate where it undergoes a transition from the continental transform of the San Andreas Fault system to the series of short spreading centers of the East Pacific Rise linked by oceanic transforms in the Gulf of California. The southern part of the trough is divided into two by the Sierra Cucapa and Sierra Mayor ranges forming the Mexicali Valley to the east and the Laguna Salada to the west. The western side of these ranges is formed by the Laguna Salada Fault, which forms a possible continuation of the Elsinore Fault Zone of southern California. The Laguna Salada Fault shows combined normal (down to the southwest) and dextral (right lateral) movement. Prior to 2010 it showed evidence of recent (probably historical) displacement with a 22 km (14 mi) zone of surface faulting, with 3–4 m (9.8–13.1 ft) of vertical displacement. This is interpreted to be associated with the 1892 earthquake. The fault moved again during the 2010 Baja California earthquake.
The earthquake was felt over a wide area from Los Angeles and San Bernardino in the north to San Quintin in the south. The area in which the perceived intensity of shaking reached VIII (destructive) or more was centered on the mapped fault rupture.
A report from the Los Angeles Times the following day stated no damage was found in Los Angeles, but also specified that severe shocks were felt in San Diego. Masonry walls were cracked in several buildings there, as well as the outlying communities of Otay and Jamul. At the abandoned Carrizo Creek Stage Station, in what is now Anza-Borrego Desert State Park in eastern San Diego county, poorly built masonry was damaged and all adobe buildings were destroyed. At Hook Ranch and Laguna Station the shaking was strong enough to throw people off their feet and at Dulzura Canyon and McCain Valley the ground was seen to move in waves. There were rockfalls at Bratton Valley, Tierra Blanca Canyon, Storm Canyon and Whale Peak and landslides at Dulzura Canyon and Devil's Canyon.
- Hough, S.E.; Elliot A. (2004). "Revisiting the 23 February 1892 Laguna Salada earthquake". Bulletin of the Seismological Society of America (Seismological Society of America) 94 (4): 1571–1578. Bibcode:2004BuSSA..94.1571H. doi:10.1785/012003244.
- Mueller, K.J.; Rockwell T.K. (1995). "Late quaternary activity of the Laguna Salada fault in northern Baja California, Mexico". Geological Society of America Bulletin (Geological Society of America) 107 (1): 8–18. doi:10.1130/0016-7606(1995)107<0008:LQAOTL>2.3.CO;2.
- National Geophysical Data Center. "Comments for the Significant Earthquake". Retrieved 3 January 2012.
- United States Geological Survey (April 10, 2010). "Magnitude 7.2 - BAJA CALIFORNIA, MEXICO". Retrieved 5 January 2012.
- "The Earthquake; No Damage in the City; Heavy Shocks at San Diego; More Quakes This Morning", Los Angeles Times, February 25, 1892
- Stephen R. Van Wormer, Sue Wade, Susan D. Walter, and Susan Arter (June 30, 2007). "An Isolated Frontier Outpost – Historical and Archaeological Investigations of the Carrizo Creek Stage Station". California Department of Parks and Recreation. Retrieved 2012-01-07.
- Stover, C.W.; Coffman, J.L. (1993). Seismicity of the United States, 1568-1989 (Revised). U.S. Geological Survey Professional Paper 1527. United States Government Printing Office. p. 110.