Stress across the San Andreas Fault system has reached its highest level in 1,000 years, according to new research from the University of Hawaii.
The study examined a geologic record of earthquake activity over the past millennium to assess stress on the San Andreas and San Jacinto fault systems. Using a physics-based computer model, researchers found that stress that would normally be released in large earthquakes has continued to accumulate.
Lead author Liliane Burkhard said the findings suggest the region could be capable of a rupture involving both fault systems. “Our results show that stress levels on multiple fault segments are now at or above the highest values seen in the past millennium and that the region may be capable of a large through-going rupture involving both fault systems,” said Burkhard, a research affiliate at the University of Hawaii at Manoa and a scientist at the University of Bern in Switzerland.
The study focused in part on Cajon Pass, between the San Bernardino and San Gabriel mountains in Southern California. Burkhard said it may act as an “earthquake gate,” sometimes blocking ruptures from crossing between faults and sometimes allowing them to spread through both systems in a single event.
Researchers said joint ruptures appear more likely when stress levels on both faults are similar. The University of Hawaii said such an event could affect densely populated areas including Los Angeles, San Bernardino, Riverside and the Coachella Valley.