M=3.2 earthquake near southern tip of San Jacinto Fault

By David Jacobson, Temblor

Check your hazard rank

The 1968 M=6.6 San Jacinto Fault earthquake ruptured near Borrego Mountain. Fortunately, this quake was extremely remote and did not cause disruption. (Photo from: Visit California)


Yesterday morning, a M=3.2 earthquake struck the southern tip of the San Jacinto Fault near Superstition Mountain. The quake occurred at a depth of 11 km, and was nearly pure strike-slip in nature, consistent with movement along the San Jacinto Fault. Because this part of Southern California is sparsely populated, few to no people felt this earthquake, in one of the more seismically hazardous regions in the state. On the USGS website, three people reported feeling it, though given their distance from the epicenter, the reports are not accurate.

This Temblor map shows a fault and earthquake map of Southern California, with the San Jacinto and San Andreas faults labeled. Additionally, yesterday’s M=3.2 quake is in the lower right hand corner. What is evident from this map is that the San Jacinto Fault experiences many more small magnitude earthquakes than the Southern portion of the San Andreas.


The San Jacinto Fault branches off the San Andreas Fault just northwest of San Bernardino, and extends for over 200 km through Southern California. The San Jacinto has a yearly slip rate of 7-17 mm, and when combined with the San Andreas, these two faults accommodate the majority of stress between the North American and Pacific plates. Because of this, the San Jacinto shows regular signs of seismicity. Additionally, while the San Andreas is capable of larger earthquakes than the San Jacinto, smaller magnitude earthquakes are more common on the San Jacinto, as is evident by the Temblor map above.

Over the last 50 years, the San Jacinto Fault has only seen one major surface-faulting event, the 1968 Borrego Mountain earthquake. However, this M=6.5 quake was extremely remote and did not cause damage. Additionally, just to the east, the Superstition Hills Fault, which is part of the San Jacinto Fault Zone ruptured in 1987 in a M=6.6 earthquake. So, the region is capable of large quakes, and the Southern California Earthquake Data Center estimates that the San Jacinto Fault could generate earthquakes reaching M=7.5. In fact, there is some evidence that shows that the M=7.5 earthquake in 1812 ruptured the northern segment of the San Jacinto. A repeat of such an event along the northern segment, which runs through San Bernardino would be devastating to Southern California.

According to the Global Earthquake Activity Rate (GEAR) model, a moderate earthquake is likely to occur in this portion of Southern California in your lifetime. This model uses global strain rates and seismicity since 1977 to forecast likely earthquake magnitudes anywhere on earth. From the Temblor image below, one can see that around the location of yesterday’s earthquake, a M=6.75 quake is likely. Therefore, understanding the seismicity and potential hazards associated with the San Jacinto Fault is important.

This Temblor map shows the Global Earthquake Activity Rate (GEAR) model for much of Southern California. This model uses global strain rates and seismicity since 1977 to forecast what the likely earthquake magnitude in your lifetime is anywhere on earth. What you can see from this image is that in the location of yesterday’s earthquake along the San Jacinto Fault, a d M=6.75 quake is likely.


Southern California Earthquake Data Center