A new study has found that tectonic stress along Southern California's San Andreas and San Jacinto fault systems has reached levels not seen in at least 1,000 years.
Scientists input records of earthquakes gleaned from geological evidence over the past 1,000 years into the simulation, including radiocarbon dating and tree-ring data, to estimate how much stress the fault systems had developed.
The study's lead author, Liliane Burkhard, said in a statement that the results indicated that stress levels on several fault segments are now "at or above the highest values seen in the past millennium."
"The region may be capable of a large through-going rupture involving both fault systems," Burkhard added. "We also found that Cajon Pass may act as an 'earthquake gate': sometimes blocking large ruptures from crossing between the faults, and sometimes allowing them to pass through and involve both systems in a single event."
Despite the findings, Burkhard emphasized that the study was not a prediction of when an earthquake will occur in the future.
"However, studies like this are important contributions to national and global earthquake hazard research in that we are using rigorous, quantitative science to better understand the risk facing millions of people," Burkhard added.
"Physics-based models like this one give us a clearer picture of the range of scenarios we should be prepared for. That information matters for hazard assessments, infrastructure planning, and emergency preparedness."
