The San Francisco earthquake of 1906. It's possible that an earthquake of similar magnitude could be triggered by another quake on an unconnected fault, a new study reports. |
Now, a new study by researchers at Scripps Institution of Oceanography at the University of California San Diego, published in the journal Science, shows that the cascading effect is frighteningly fast. A large earthquake on one fault can trigger large aftershocks on separate faults within just a few minutes, the researchers found.
The study's authors, Scripps geophysicist Peter Shearer and graduate student Wenyuan Fan, analyzed data from seismic stations that are part of the Incorporated Research Institution for Seismology's global network. They discovered 48 previously unidentified large aftershocks from 2004 to 2015 that occurred within 200 seconds after 27 different magnitude 7 to 8 earthquakes on other faults, some of which were as far as 207.5 miles away.
In one instance cited in the study, a magnitude 7 earthquake off the coast of Indonesia triggered two large aftershocks that were 47 and 137 miles away, respectively, from the main fault, within 68 and 120 seconds of the initial shock.
"The results are particularly important because of their seismic hazard implications for complex fault systems, like California," study-co-author Fan said in a UCSD press release. "By studying this type of triggering, we might be able to forecast hosting faults for large earthquakes."
While most aftershocks occur near the main fault rupture, the study proves that large early aftershocks can also be triggered by seismic waves that jump between faults that aren't directly connected.
Read more at Discovery News
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