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National & World

California’s subsequent ‘Huge One’ may not be what we count on, researchers say

Madisony
Last updated: August 11, 2025 9:14 pm
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California’s subsequent ‘Huge One’ may not be what we count on, researchers say
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What might the subsequent mega-earthquake on California’s infamous San Andreas fault appear like?

Wouldn’t it be a repeat of 1857, when an earthquake estimated at magnitude 7.7 to 7.9 ruptured the fault from Monterey County all over Los Angeles County? Wouldn’t it be extra akin to the nice 1906 San Francisco earthquake, which started simply offshore of town and ruptured in two instructions, towards Humboldt County and Santa Cruz County?

Don’t wager on an equivalent sequel.

That’s the implication of a examine revealed Monday within the journal Proceedings of the Nationwide Academy of Sciences. The report, coauthored by scientists at Caltech in Pasadena, studied a large earthquake that ruptured within the southeast Asian nation of Myanmar on March 28 — on a fault recognized for being eerily much like the San Andreas.

The earthquake ended up rupturing a for much longer part of the fault than scientists anticipated, given the seismology of the area.

The implications of this examine are that “earthquakes by no means come again precisely the identical method,” Solene L. Antoine, a postdoctoral fellow at Caltech and the examine’s lead writer, mentioned in an interview.

An area man drives a bike previous a broken constructing, within the aftermath of an earthquake in Naypyidaw, Myanmar, on March 30.

(Aung Shine Oo / Related Press)

“It got here as a shock that you possibly can get such an extended rupture,” mentioned Jean-Philippe Avouac, a coauthor of the examine and a professor of geology and mechanical and civil engineering at Caltech.

March’s Mandalay earthquake devastated Myanmar, killing not less than 3,791 folks and a further 63 folks in Thailand. Excessive-rise buildings have been broken as far-off as Ho Chi Minh Metropolis in Vietnam and houses have been broken within the Ruili space of China. Harm was estimated at $1.9 billion, in accordance with the U.S. Geological Survey.

It was essentially the most highly effective earthquake in Myanmar in not less than 79 years.

Map showing a long swath of extreme shaking along more than 300 miles of a ruptured earthquake fault in Myanmar.

“Violent” and “excessive” shaking, proven in pink, was felt all alongside the 317 miles of the ruptured Sagaing fault in Myanmar throughout a magnitude 7.7 earthquake in March.

(U.S. Geological Survey)

The magnitude 7.7 earthquake ruptured an astonishing 317 miles of the Sagaing fault, a discovering based mostly on Antoine’s evaluation of satellite tv for pc knowledge displaying earth motion after the quake. That’s the longest seismic rupture ever documented on a continent.

By comparability, California’s 1906 earthquake ruptured 296 miles of the San Andreas fault; and the 1857 earthquake, 225 miles. Longer seismic ruptures have been discovered solely on subduction megathrusts deep beneath the ocean.

What’s clear from the examine is that whereas California’s subsequent “Huge One” could share some traits of beforehand documented devastating quakes, it’s unlikely to be an actual replay. Because the current expertise in Myanmar reveals, even well-documented faults can behave in stunning methods.

The following step is to develop a mannequin simulating earthquakes over many millennia for the San Andreas fault, which the authors plan to do sooner or later. However the San Andreas fault “is way extra advanced,” Avouac mentioned. “It’s not going to return quickly, as a result of it’s fairly a heavy calculation.”

Nonetheless, such simulations would offer a mannequin of “all potential eventualities in order that we’ve a greater view of the vary of potential ruptures that would occur.”

Rescuers work at the site of a high-rise building under construction that collapsed after a 7.7 magnitude earthquake.

Rescuers work on the website of a high-rise constructing below building in Bangkok, Thailand, that collapsed after a magnitude 7.7 earthquake centered in Myanmar on March 28.

(Wason Wanichakorn / Related Press)

As an illustration, possibly the San Andreas fault will rupture in smaller, separate earthquakes, Avouac mentioned.

Or it may very well be a a lot bigger earthquake — rupturing the fault not simply from Monterey to Los Angeles counties, however maybe all the way in which into San Bernardino, Riverside and Imperial counties, which might exceed magnitude 8. Such a quake could be the biggest simultaneous catastrophe in trendy California historical past, with enormous swaths of the state wracked by highly effective seismic shaking .

By comparability, the 1994 Northridge earthquake’s footprint was comparatively constrained, severely affecting solely a portion of Los Angeles County, particularly the San Fernando Valley — associated to its comparatively smaller magnitude of 6.7.

However whereas modeling earlier exercise on the San Andreas fault will present a glimpse into the wide selection of potential outcomes, it won’t pinpoint exactly when the subsequent nice quake will strike.

“We are able to’t simply count on the very same factor to occur,” Antoine mentioned. “It’s a matter of simply displaying what eventualities are potential, the variety of eventualities and seeing what are the implications of every of these eventualities.”

A Buddhist monk walks near a collapsed pagoda after an earthquake in Mandalay, central Myanmar.

A Buddhist monk walks close to a collapsed pagoda on March 30 after an earthquake in central Myanmar.

(Thein Zaw / Related Press)

Typically, Avouac mentioned, “it’s quiet for a very long time, nothing occurs … stress is build up, the fault is locked for a very long time, nothing occurs, after which, increase, you might have a big earthquake.”

“After which you might have different durations throughout which you might have a variety of [seismic] exercise, however these earthquakes are all smaller,” Avouac mentioned.

However “smaller” earthquakes, within the minds of researchers, are nonetheless large to the layperson. Within the examine’s simulations, there are durations the place earthquakes round magnitude 7.7 are frequent. In different durations, earthquakes max out at magnitude 7.5 or so, however are extra frequent.

Your entire size of the Sagaing fault — together with areas that didn’t rupture within the March earthquake — is 750 miles, north to south, from the Himalayas to the Andaman Sea, and helps accommodate the northward push of the Indian tectonic plate.

The truth that 317 miles of the Sagaing fault ruptured in March was stunning to scientists. Solely about 170 miles had been quiet seismically for greater than a century, having final ruptured in 1839.

Two maps showing sections of various earthquake faults that ruptured in separate earthquakes over the centuries.
These maps present the 317 miles of the Sagaing fault that ruptured in March, in comparison with the historic ruptures, as outlined in a 2016 examine, of the San Andreas fault in California in 1730, 1812, 1857 and 1906.

(Solene Antoine / Caltech)

Scientists name these “seismic gaps” — specific areas of a fault that haven’t not too long ago ruptured.

Typically, scientists would’ve anticipated solely this long-dormant 170-mile piece of the Sagaing fault to rupture, Avouac mentioned, however no more not too long ago ruptured sections. That features a 100-mile stretch that ruptured in massive earthquakes in 1929 and 1930, and a 50-mile stretch that went off in a pair of quakes in 1946 and 1956.

As an alternative, even these fault segments ruptured within the large March earthquake.

So what offers?

A potential clarification is the Sagaing fault’s extraordinary smoothness. “And folks have noticed that when the fault could be very easy, the rupture … tends to propagate at a velocity” so quick that it leads to an “extraordinarily elongated rupture,” Avouac mentioned.

The examine additionally revealed the outcomes of a pc mannequin simulation taking a look at how earthquakes would possibly rupture alongside sections of the whole 750-mile lengthy Sagaing fault. The code, developed by examine coauthor Kyungjae Im of Caltech, means that over a hypothetical 1,400-year interval, there could be no repeatable patterns.

In different phrases, earthquakes didn’t appear to re-occur like clockwork, rupturing the identical stretch of fault in a repeatable, predictable sample.

“There’s complexity right here. And it’s because every time you might have an earthquake, it redistributes the stress on the fault, which goes to affect the subsequent earthquake,” Avouac mentioned. “There’s a self-induced complexity within the course of, and that results in a little bit of randomness.”

There’s one certainty, which is sure to disappoint anybody who shares the hope {that a} “Huge One” merely gained’t ever strike California once more.

“There might be an earthquake sooner or later,” Antoine mentioned. “If there’s stress build up on the fault, the fault gained’t maintain eternally.”

Additional analysis and observations are important to refine fashions of future potential earthquakes, together with from the Sentinel satellites, that are operated by the European Area Company, the authors mentioned.

The opposite coauthors of the examine are Rajani Shrestha and Chris Milliner of Caltech; Chris Rollins of Earth Sciences New Zealand; Kang Wang of the Washington-based EarthScope Consortium; and Kejie Chen of the Southern College of Science and Expertise in Shenzhen, China.

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