New research released this week found that a fault under the heart of San Diego can produce stronger and more frequent earthquakes than previously thought.

It’s the second study in recent months pointing to heightened quake risks in the San Diego area.

San Diego’s Rose Canyon fault produces powerful earthquakes more frequently than once believed, according to researchers from San Diego State University.

Seismologist Tom Rockwell said that earlier work indicated that such quakes occur every 1,000 to 1,500 years on the 40-mile-long fault, which extends from San Diego Bay, through Old Town and across Mission Valley, and up Rose Canyon through Mt. Soledad, to offshore at La Jolla.

The fault is known to extend as far north as Oceanside offshore.
“A powerful quake in the mid-to-upper 6s could cause liquefaction around San Diego and Mission bays and locally in Mission Valley, and cause the land to be offset across the fault, which would damage buildings,” said Rockwell, one of California’s most experienced seismologists.

In March, scientists proved how San Diego’s Rose Canyon should give residents of Los Angeles and Orange counties something to worry about.

Researchers said the discovery of missing links between earthquake faults shows how a magnitude 7.4 temblor could rupture virtually simultaneously underneath Los Angeles, Orange and San Diego counties.

But to get to a 7.4, the earthquake would not only have to again rupture the Newport-Inglewood fault in Los Angeles and Orange counties. It would also have to jolt the Rose Canyon fault system, which runs all the way through downtown San Diego and hasn’t ruptured since roughly 1650.

“These two fault zones are actually one continuous fault zone,” Valerie Sahakian, the study’s lead author, said earlier this year. 

Sahakian wrote the study while working on her doctorate at Scripps Institution of Oceanography at UC San Diego. Sahakian is now a research geophysicist with the U.S. Geological Survey.

In the past, scientists reported gaps between the two fault systems of as much as 3 miles. But this study showed the gaps are actually less than 1¼ miles apart.

“That kind of characterizes it as one continuous fault zone, as opposed to two different, distinct fault systems,” Sahakian said, making it far easier for an earthquake to keep shaking land as it races down a longer fault, widening the seismic reach of the temblor.

There had already been consensus among scientists over the last three decades that the fault systems were actually one, said Caltech seismologist Egill Hauksson, who was not involved with this study. “We now have real evidence that this is the case,” Hauksson said.




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