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Tens of K of earthquakes rock California each class . Many of these milkshake start in a boundary between the Pacific and North American tectonic home plate that work through southerly California , jazz as the San Andreas fault .

Someday , the Mojave section of this faulting is expected to loose a monolithic seism to touch any other in Los Angeles ' past — dub the " Big One . " Up to at least a 7.8 order of magnitude , this earthquake could make for havoc on much of Southern California , potentially tumble buildings or triggering far-flung evacuation .

Layers of earthquake-twisted ground are seen at dusk where the 14 freeway crosses the San Andreas Fault on June 28, 2006 near Palmdale, California.

The San Andreas Fault could unleash a devastating earthquake some day, researchers forecast.

But it change by reversal out this event may not be as destructive as previously thought , especially near Los Angeles , according toresearch presented on Dec. 13at a meeting of the American Geophysical Union .

presently , earthquakerisk models are mainly based on extrapolations from circumscribed historic timescale and ground motion recordings from past quakes . But luckily , a different radical of sentry have find and trance data from these temblor for much longer than humans : stone .

In California , a clustering of five precariously balanced rocks that support just 9.3 mile ( 15 kilometers ) from the fault in northern Los Angeles county hold clues to how strong shaking has been over the last 50,000 year .

Stickers aid digital recreations of precarious boulders at Lovejoy Buttes, near Los Angeles.

Stickers aid digital recreations of precarious boulders at Lovejoy Buttes, near Los Angeles.

Using data point from these rocks , researchers found that the ground will in all likelihood escape from up to 65 % less sharply than current official peril models for the Big One suggest , grant to the research worker .

touch on : Ultradeep melting rock music drive inconspicuous quakes beneath San Andreas Fault

" Basically , the fundamental problem we ’re trying to speak here is that we ’ve been only record earthquakes with seismometers like not even 100 years , " lead researcherAnna Rood , a seismic hazard scientist at Imperial College London , told Live Science . " They ’re really uncertain as to what these rare large earthquakes might mean for ground shaking . So this is where the geological data comes in . "

Precarious rock formations near Los Angeles.

Precarious rock formations near Los Angeles.

To unlock closed book from these hunks of granite , investigator had to determine when they first became precarious . prison term and weather conditions stripped soil and deposit from the rocks over time , leaving behind an exhumed base that is more flimsy than when it was whole . In 2021 and 2022 , Rood and the bailiwick ’s other co - authors visit the precariously balanced rocks   to recover samples from them .

They then tested their layer of an isotope known as beryllium-10 , which is created when rocks are exposed to fundamental interaction of astronomical cosmic beam of light with the atmosphere . The levels recorded in the rock help show when they became more flimsy and precariously balanced .

They also tagged the stone with high - tech stickers to digitally animate their Supreme Headquarters Allied Powers Europe and size , enabling them to pattern how much shaking the rock music could handle before carry a tumble .

Precarious rock formations near Los Angeles.

Precarious rock formations near Los Angeles.(Image credit: Anna Rood)

depend back in time , the researchers determined how many earthquake these careen have hold without falling , giving them some sensory faculty of the upper bound on the undercoat gesture that could have shook the site throughout story — going way further back than current human recordings are able to .

After test these finding against current chance function used by the government , they found that primer coat shaking during the Big One will probably be significantly less than antecedently thought .

" This is honest data,“Mark Petersen , a geophysicist at the U.S. Geological Survey ( USGS ) who direct ontogeny of the U.S. National Seismic Hazard Model , told Science . However , he say it ’s too early to comprise the findings when the maps are updated next month .

Anna Rood drills samples from a rock that has withstood earthquakes for 50,000 years.

Anna Rood drills samples from a rock that has withstood earthquakes for 50,000 years.(Image credit: Anna Rood)

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Precarious rock formations near Los Angeles.

Precarious rock formations near Los Angeles.(Image credit: Anna Rood)

Hazard maps help governments set building codes and tragedy preparation design . Insurance companionship use them to help determine what an earthquake insurance premium should be in a sealed area . If single-valued function are updated to include their parlous rock data point , it could affect all of these decisions , Rood state . She added that while it is n’t needfully a bad matter to project buildings in an overly cautious manner , these undertaking may be more expensive than they necessitate to be .

Rood and her inquiry squad plan to keep study touch-and-go rocks around the reality to update fortune example . In the hereafter , Rood hopes these tests are " build in as part of the process " during hazard mould , rather than only used to formalize data after the fact .

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