╌>

Researchers gain clear picture of fault that threatens Pacific Northwest

  

Category:  News & Politics

Via:  perrie-halpern  •  6 days ago  •  17 comments

By:   Evan Bush

Researchers gain clear picture of fault that threatens Pacific Northwest
A fault off the Pacific coast could devastate Washington, Oregon and Northern California with a major earthquake and tsunami. Researchers mapped it comprehensively for the first time.

S E E D E D   C O N T E N T


A silent colossus lurks off the Pacific coast, threatening hundreds of miles of coastline with tsunamis and devastating earthquakes.

For decades, scientists have warned about the potential of the Cascadia Subduction Zone, a megathrust fault that runs offshore along the coast from northern Vancouver Island to Cape Mendocino, California. When the fault — or even a portion of it — next snaps, it will reshape life in Oregon, Washington and Northern California.

Of particular concern are signals of massive earthquakes in the region's geologic history. Many researchers have chased clues of the last "big one": an 8.7-magnitude earthquake in 1700. They've pieced together the event's history using centuries-old records of tsunamis, Native American oral histories, physical evidence in ghost forests drowned by saltwater and limited maps of the fault.

But no one had mapped the fault structure comprehensively — until now. A study published Friday in the journal Science Advances describes data gathered during a 41-day research voyage in which a vessel trailed a miles-long cable along the fault to listen to the seafloor and piece together an image.

The team completed a detailed map of more than 550 miles of the subduction zone, down to the Oregon-California border.

Their work will give modelers a sharper view of the possible impacts of a megathrust earthquake there — the term for a quake that occurs in a subduction zone, where one tectonic plate is thrust under another. It will also provide planners a closer, localized look at risks to communities along the Pacific Northwest coast and could help redefine earthquake building standards.

"It's like having coke-bottle glasses on and then you remove the glasses and you have the right prescription," said Suzanne Carbotte, a lead author of the paper and a marine geophysicist and research professor at Columbia University's Lamont-Doherty Earth Observatory. "We had a very fuzzy low-resolution view before."

The scientists found that the subduction zone is much more complex than they previously understood: It is divided into four segments that the researchers believe could rupture independently of one another or together all at once. The segments have different types of rock and varying seismic characteristics — meaning some could be more dangerous than others.

Earthquake and tsunami modelers are beginning to assess how the new data affects earthquake scenarios for the Pacific Northwest.

Kelin Wang, a research scientist at the Geological Survey of Canada who was not involved in the study, said his team, which focuses on earthquake hazard and tsunami risk, is already using the data to inform projections.

"The accuracy and this resolution is truly unprecedented. And it's an amazing data set," said Wang, who is also an adjunct professor at the University of Victoria in British Columbia. "It just allows us to do a better job to assess the risk and have information for the building codes and zoning."

Harold Tobin, a co-author of the paper and the director of the Pacific Northwest Seismic Network, said that although the data will help fine-tune projections, it doesn't change a tough-to-swallow reality of living in the Pacific Northwest.

"We have the potential for earthquakes and tsunamis as large as the biggest ones we've experienced on the planet," said Tobin, who is also a University of Washington professor. "Cascadia seems capable of generating a magnitude 9 or a little smaller or a little bigger."

A quake that powerful could cause shaking that lasts about five minutes and generate tsunami waves up to 80 feet tall. It would damage well over half a million buildings, according to emergency planning documents.

Neither Oregon nor Washington is sufficiently prepared.

To map the subduction zone, researchers at sea performed active source seismic imaging, a technique that sends sound to the ocean floor and then processes the echoes that return. The method is often used for oil and gas exploration.

They towed a 9-plus-mile-long cable, called a streamer, behind the boat, which used 1,200 hydrophones to capture returning echoes.

"That gives us a picture of what the subsurface looks like," Carbotte said.

The research vessel Marcus Langseth docks in Seattle after a 41-day expedition along the Pacific coastline. The ship allowed researchers to map the Cascadia Subduction Zone.Courtesy Harold Tobin

Trained marine mammal observers alerted the crew to any sign of whales or other animals; the sound generated with this kind of technology can be disruptive and harm marine creatures. Carbotte said the new research makes it more clear that the entire Cascadia fault might not rupture at once.

"The next earthquake that happens at Cascadia could be rupturing just one of these segments or it could be rupturing the whole margin," Carbotte said, adding that several individual segments are thought to be capable of producing at least magnitude-8 earthquakes.

Over the past century, scientists have only observed five magnitude-9.0 or higher earthquakes — all megathrust temblors like the one predicted for the Cascadia Subduction Zone.

Scientists pieced together an understanding of the last such Cascadia quake, in 1700, in part via Japanese records of an unusual orphan tsunami that was not preceded by shaking there.

"It requires an 8.7 to get a tsunami all the way to Japan," Tobin said.

The people who recorded the incident in Japan couldn't have known that the ground had shaken an ocean away, in the present-day United States.

Today, the Cascadia Subduction Zone remains eerily quiet. In other subduction zones, scientists often observe small earthquakes frequently, which makes the area easier to map, according to Carbotte. That's not the case here.

Scientists have a handful of theories about why: Wang said the zone may be becoming quieter as the fault accumulates stress. And now, we're probably nearing due.

"The recurrent interval for this subduction zone for big events is on the order of 500 years," Wang said. "It's hard to know exactly when it will happen, but certainly if you compare this to other subduction zones, it is quite late."


Tags

jrDiscussion - desc
[]
 
devangelical
Professor Principal
1  devangelical    6 days ago

lemons/lemonade, how much of the potential new state of jefferson and aryan nations will end up being under water?

 
 
 
Buzz of the Orient
Professor Expert
2  Buzz of the Orient    6 days ago

Whose fault is it?

 
 
 
Robert in Ohio
Professor Guide
3  Robert in Ohio    5 days ago

So beach front property in Nevada and Montana is not totally out of the question

 
 
 
Perrie Halpern R.A.
Professor Principal
4  seeder  Perrie Halpern R.A.    5 days ago

I hope not until my daughter moves back from Uni there.

 
 
 
devangelical
Professor Principal
4.1  devangelical  replied to  Perrie Halpern R.A. @4    5 days ago

buy her one of those auto-inflating life vests to wear full time, well, not in the shower...

 
 
 
Ed-NavDoc
Professor Quiet
4.2  Ed-NavDoc  replied to  Perrie Halpern R.A. @4    5 days ago

My oldest grandson and his fiance live on the coast of Southern Oregon in a small town called Reedsport. I think I will send this to him.

 
 
 
CB
Professor Principal
4.3  CB  replied to  Perrie Halpern R.A. @4    5 days ago

Nowhere is 100% risk free of nature. New York had its own recent earthquake and there is a major fault under New Jersey, New York, and Pennsylvania. That is to say, we "await our potential doom" in Calfornia along with the East Coast regions: One Day.

That said, potentially we will all meet our doom one day, some day, and some way.

This in no way takes away from your concern about California and your wonderful daughter.

 
 
 
Ed-NavDoc
Professor Quiet
5  Ed-NavDoc    5 days ago

I'm reminded of that George Strait song about ocean front property in Arizona.

 
 
 
Drinker of the Wry
Junior Expert
6  Drinker of the Wry    5 days ago
Well, I did not think the girl
Could be so cruel
And I'm never going back
To my old school
California tumbles into the sea
That'll be the day I go back to Annandale
 
 
 
shona1
Professor Quiet
7  shona1    5 days ago

Arvo.. New Zealand has been having a few decent shakes lately...always a worry anywhere in the world..

Night time is the worst going by my Kiwi friends...but in the day they aren't to flash either..

 
 
 
CB
Professor Principal
8  CB    5 days ago

Arvo! May you and yours never have to run to and fro during an earthquake! I have experienced plenty. I always can't wait for the shaking to stop (it does after mere seconds), because if it continues I worry about 'everything.' From furniture not properly put to gas-lines breaking. I check everything around me. :) Of course, I turn on the television to learn where its center 'broadcasted.' 

Basically, these are the long-term issues that nature is giving U.S. time to study and find solutions that save mass casualty lives. Instead, the House repeatedly dedicates itself to fighting  a Loser's retribution. We all need to WAKE UP.  This time is being squandered.

 
 
 
shona1
Professor Quiet
8.1  shona1  replied to  CB @8    5 days ago

That is one thing we don't get here other than a few mild rumbles once every blue moon...

Nope, you can have earthquakes much prefer our disasters because you can see them coming.. bushfires, floods, cyclones etc...

My Kiwi friends say you are meant to stand under a door frame, get under a table etc for protection which they do..for them anything after 20  seconds it's regarded as a biggish one..stuff that!!

 
 
 
CB
Professor Principal
8.1.1  CB  replied to  shona1 @8.1    4 days ago

20 seconds is a long time in earthquake 'language.' I agree with them!  Intensity matters with each sec! Sometimes we have the 1 "Thud" or the 3 -5  second "Bounce" and then everythig stops. . . and we begin waiting for aftershocks. Sometimes I feel them; other times I just imagine I feel something. ;)

 
 
 
Drinker of the Wry
Junior Expert
8.1.2  Drinker of the Wry  replied to  shona1 @8.1    4 days ago
That is one thing we don't get here other than a few mild rumbles once every blue moon...

You’re not on a tectonic plate boundary, however, your 7 centimeter annual movement northward while rotating slightly clockwise does exert stress on the rocks within your crust resulting in a few, mild earthquakes.

 
 
 
MrFrost
Professor Guide
9  MrFrost    4 days ago

I live about 80 miles South of Seattle. If it happens it happens.  No matter where you live there is some risk of Mother Nature getting pissed off. 

 
 
 
devangelical
Professor Principal
9.1  devangelical  replied to  MrFrost @9    4 days ago

just lash some maga floaters together and row for shore... /s

 
 
 
devangelical
Professor Principal
9.1.1  devangelical  replied to  devangelical @9.1    3 days ago

FYI - point them all in the same direction with their anuses below the waterline and the out-gassing should propel them forward...

 
 

Who is online

Tessylo
Thomas
Igknorantzruls
Texan1211
JohnRussell
Gazoo


42 visitors