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Laguna Salada (Spanish, "salty lagoon") is a vast dry lake some 10 meters below sea level in the Sonoran Desert of Baja California, 30 km (19 mi) southwest of Mexicali. [1] This lake was called "Ha wi mək" in Cocopah language and "Ha-sa-ai" in Kumeyaay language.
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The Imperial Fault Zone is a right lateral-moving strike-slip fault, representing the northernmost transform fault associated with the East Pacific Rise.It is connected to the San Andreas Fault by the Brawley Seismic Zone.
A United States Geological Survey map showing the Laguna Salada Fault outlined in red. The Laguna Salada Fault is a geological fault between the United States and Mexico. About 64–80 kilometers (40–50 mi) long, it straddles the Imperial County-California–Baja California border. [1]
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The Elsinore Fault Zone, not including Whittier, Chino, and Laguna Salada faults, is 180 kilometers (110 mi) long with a slip-rate of 4.0 millimeters/year (0.15 in/yr). It is estimated that this zone is capable of producing a quake of 6.5–7.5 M W. The projected interval between major rupture events is 250 years.
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The quake originally was believed to have occurred on the Laguna Salada Fault, which is about 60 kilometers (37 mi) to 80 km (50 mi) long and straddles the California–Baja California border. [6] The active Laguna Salada Fault ruptured in February 1892 with an estimated M w 7.2 earthquake. [7] [8]