Will
a megathrust earthquake strike the NW in 2013? Some clues emerging
There
were 4,800 earthquakes in the Northwest in 2012 and a record
"episodic tremor and slip" event – a string of deep
mini-quakes running from Vancouver Island to below Centralia – over
the summer, but does any of that mean we're likely to see the "big
one" in 2013?
2
January, 2014,
While
the devastating megathrust quakes that happen every 300 to 500 years
in our neck of the woods (those caused by the Juan De Fuca plate's
grinding collision and subduction with the North American plate) are
still impossible to predict, some clues may be emerging.
An
immature science
Taken
together, last year's quakes were "mild" since so few of
them were big enough to be felt, said John Vidale, director of the
Pacific Northwest Seismic Network.
The
biggest and most interesting quake of the year struck under
Victoria, B.C., last week. It was a magnitude 4 temblor and
resembled in depth and fault the magnitude 6.8 Nisqually quake that
damaged Seattle and shook the region in 2001, he said.
He
added that a string of unusual quakes around the globe has the
seismic community baffled. A big earthquake off the coast of
Sumatra in the Indian Ocean six months ago was "very strange"
because of its size and distance from the plate boundary.
It
showed "we can get earthquakes we really hadn't anticipated,"
he said.
In
the past few years, China got hit with an earthquake on a fault
that wasn't mapped, New Zealand suffered a "very rare
earthquake" ...
"There's
a whole series of events in the last decade that give us the
impression that we know less than ever," Vidale said. "We
keep thinking that these are the specific risks we need to look out
for and then earthquakes happen that aren't the ones we thought
were most likely to happen."
Also,
a roughly annual seismic event in the Northwest discovered 12 years
ago – the "episodic tremor and slip,"or ETS – went
wild last summer.
Doing
the 'tremor and slip'
The
boundary between the Juan De Fuca plate offshore and the North
American plate runs under the Puget Sound area from California up
to Canada. That's where we get the megathrust quakes of magnitude 9
or better. Below that danger zone, deeper in the subduction, is
where the ETS happens.
The
tremor and slip this summer was "one of the biggest ETS events
yet monitored," the seismic
network reported in its blog.
And that had the experts "ever so slightly nervous."
"We
thought we knew the pattern pretty well, that it would start down
in the south Puget Sound, spread out for a couple of weeks, mainly
going north under the Vancouver Island," Vidale
told KPLU in October.
"This time broke the pattern ... It started in the north and
came south. It is also the biggest episode we've seen yet."
Clues
to the big one?
"These
are adding stress to the area where we expect damaging earthquakes
to occur," said Stanford University geophysics professor Paul
Segall, "... so what does that mean? What do you do from a
practical standpoint?"
When
the ETS was first discovered, officials in Canada sent out
earthquake warnings when one fired up because they worried these
events signaled a potential quake. After a string of false alarms
and new mysteries, they've stopped the practice.
However,
the question remains: Are these events associated with earthquakes
and if so, how?
Segall
is building computer models to find answers and so far has some
preliminary results that suggest the tremors and slips are in fact
connected to quakes. In his simulations, after a big earthquake,
the events stop for about 100 years and then start up again.
And
then one of them eventually will "spontaneously grow into a
fast, dynamic rupture" – an earthquake. The problem is he
can't tell which one will mutate into disaster.
"You
would hope that there would be something about them that would tip
us off that we're getting near the end of the cycle and there was a
big earthquake about to occur," he said. "In these
simulations, we don't see anything in and of itself that presages
an earthquake."
A
fascinating time
Segall's
initial results were announced by Stanford under the title
"Himalayas
and Pacific Northwest could experience major earthquakes, Stanford
geophysicists say."
The
release explains:
The Cascadia subduction zone, which stretches from northern California to Vancouver Island, has not experienced a major seismic event since it ruptured in 1700, an 8.7–9.2 magnitude earthquake that shook the region and created a tsunami that reached Japan. And while many geophysicists believe the fault is due for a similar scale event, the relative lack of any earthquake data in the Pacific Northwest makes it difficult to predict how ground motion from a future event would propagate in the Cascadia area, which runs through Seattle, Portland and Vancouver. ...
The
work is still young, and Segall noted that the model needs
refinement to better match actual observations and to possibly
identify the signature of the event that triggers a large
earthquake.
"We're
not so confident in our model that public policy should be based on
the output of our calculations, but we're working in that
direction," Segall said in the release.
One
thing that makes Segall's work difficult is a lack of data from
actual earthquakes in the Cascadia region. Earlier this year,
however, earthquakes in Mexico and Costa Rica occurred in areas
that experience slow slip events similar to those in Cascadia.
"There
are a few places in the world where these slow slip events are
associated with small to moderate-sized earthquakes, and they are
very clearly tied in space and time," he said. "The
timing is clear, not a coincidence. They really occur in lockstep."
So,
the research goes on and both Vidale and Segall said they need more
data collection instruments stuck in the ground around the globe to
create data sets that will solve these puzzles.
"One
of the things about the ETS events is that it is a reminder every
15 months or so in the Puget Sound region ... something is
happening down there, and it's pushing stress around and it's just
a reminder that (a megathrust earthquake) is inevitable. It's not
if it's going to happen it's when. It's probably not too soon, but
we can't be too sure of that."
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