Imperial Fault Zone
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. It terminates on its southern end at the Cerro Prieto spreading center.
The Imperial Fault Zone is thought to accommodate slip from both the San Andreas and the San Jacinto fault zones. However, studies covering the last few hundred years show that the slip rate is insufficient to account for the total slip from the San Andreas system. The surface trace is well-located based on mapped surface offsets from historic events.
The Imperial Fault Zone has a history of earthquakes of moderate magnitude, including several doublet earthquakes.
- 1915 Imperial Valley earthquakes: Two magnitude 6.25 shocks occurred ~1 hour apart. Six people died and several were injured in the second quake at Mexicali, located just inside the Mexican border. Unstable banks of the New and Alamo Rivers caved in many places.
- 1940 El Centro earthquake
- 1979 Imperial Valley earthquake
- Treiman, J.Jerome, compiler, 1999, Fault number 132, Imperial fault, in Quaternary fault and fold database of the United States: U.S. Geological Survey website, http://earthquakes.usgs.gov/hazards/qfaults
- A 300- to 550-year history of slip on the Imperial fault near the U.S.-Mexico border, Thomas and Rockwell (1996)
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