Two geologists stand in a trench looking at evidence for earthquakes in the layers of soil.
A small fault lying between the San Andreas and San Jacinto faults provides evidence for past earthquakes that involved both major faults. Geologists Tom Rockwell (San Diego State) and Michael Oskin (UC Davis) work in a trench into the fault. (Alba Rodríguez Padilla)

Evidence for Shared Earthquakes Between San Andreas and San Jacinto Faults

The San Andreas and San Jacinto faults have ruptured simultaneously at least three times in the past 2,000 years, most recently in 1812, according to a new study by geologists at the University of California, Davis, and San Diego State University. The work was published Dec. 7 in the journal Geology.

Large earthquakes involving multiple faults increase the threat of strong ground shaking. However, each of these faults on their own can generate a large (magnitude 7.5 or above) earthquake, said Alba Rodríguez Padilla, a graduate student in the UC Davis Department of Earth and Planetary Sciences and first author on the paper.

A computer illustration of the major fault lines in the area of Wrightwood, California
Earthquake faults in the area of Wrightwood, California, include the San Andreas Fault (SAF), the San Jacinto Fault (SJF) and the Lytle Creek Ridge Fault (LCRF).

“Typically, we think earthquakes will remain confined to a single fault, especially for 'mature' faults such as the San Andreas and the San Jacinto, which are well-established, geometrically-simple plate boundary faults,” Rodríguez Padilla said. But researchers previously have shown that it’s theoretically possible for an earthquake to transfer from one fault to another where they come close together at Cajon Pass, north of Los Angeles, she said.

“However, prior to our study, there was no direct physical evidence that these joint ruptures, or shared earthquakes, do in fact occur,” Rodríguez Padilla said. 

Between the south end of the San Andreas Fault and the northern end of the San Jacinto lies a small fault, the Lytle Creek Ridge Fault. This fault would slip only when there is an earthquake shared across the two bigger faults.

The Lytle Creek Ridge Fault does not itself do any work during these shared earthquakes, just acting as a passive marker, Rodríguez Padilla said.

20% to 23% of earthquakes shared

To get evidence of potential shared earthquakes, Rodríguez Padilla and colleagues hand-dug a trench 15 meters (about 50 feet) long and up to 3 meters (about 10 feet) deep along the Lytle Creek Ridge Fault. They identified signs of three earthquake events in the past 2,000 years, based on radiocarbon and pollen dating.

That compares to 15 known earthquakes on the San Andreas and 13 on the San Jacinto over the same time. Based on these findings, the team concluded that 20% to 23% of earthquakes on these major faults are shared with the other fault.

A geologist stands on the ground surface looking a deep trench dug to expose evidence of earthquakes in soil layers.
The study involved digging a trench 15 meters long and up to 3 meters deep into the San Gabriel mountains. (Alba Rodríguez Padilla)

Next, they simulated the historically recorded earthquakes of 1812 and 1857 to see if these could have been multi-fault earthquakes. Based on the simulations, they discarded the 1857 earthquake and found that the 1812 earthquake was capable of jumping faults. 

Additional co-authors on the paper are Professor Michael Oskin and project scientist Irina Delusina, UC Davis Department of Earth and Planetary Sciences; and Thomas Rockwell and Drake Singleton, San Diego State University. Julian Lozos, California State University, Northridge, and Kelian Dascher-Cousineau, UC Santa Cruz, helped dig the trench.

The work was supported by the Southern California Earthquake Center, which is funded by the U.S. Geological Survey and the National Science Foundation.

Andy Fell, UC Davis News and Media Relations

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