California
quake model looks for ‘mega-quake’ along Cascadia
10
January, 2013
PORTLAND
- New research is giving us some insight into when a major earthquake
could strike the Northwest.
The
research was done in part by Stanford geophysics Professor Paul
Segall. He has been tracking a series of very small tremors that
rumble deep within the earth.
The
slow tremors happen roughly every summer along the Cascadia
Subduction Zone, an undersea fault about 70 miles off the Oregon
Coast.
Over
the last decade, data shows the tremors have been getting
progressively bigger. Last summer, the Pacific Northwest experienced
a notably large one.
Experts
believe those tremors are adding stress to the offshore fault.
Using
this data, Segall built a computer model which suggests it will be
one of those tiny quakes that triggers a major magnitude 9
earthquake.
“What
we do see is that ultimately one of these tends to develop into a
fast and potentially, damaging earthquake,” said Segall.
Segall
said that scientists don't yet know how big those tremors need to get
before they explode into a mega-thrust quake.
And
that means a major earthquake in the Pacific Northwest could still be
hundreds of years away.
But,
he added, those tiny tremors are a good reminder that we always need
to be prepared.
Single
Super Quake Could Affect Both Northern, Southern California: Study
Cal
EMA will consider amending response plans in light of the new
findings, discovered while studying devastating quakes in Asia.
4NBC,
11
January, 2013
For
the first time, scientists and emergency planners are examining
whether a super quake could affect both Northern and Southern
California, rendering the entire state helpless in the aftermath of
the "Big One."
Seismologists
have warned Southern California that a major quake on the lower San
Andreas Fault, the so-called Big One is inevitable. But that the
population centers of both Southern and Northern California could be
affected simultaneously by one quake on the San Andreas Fault has
only recently been recognized as a possibility.
The
study by Professor Nadia Lapusta at the California Institute of
Technology (Caltech) and Japanese collaborator Hiroyuki Noda focused
on explaining the behavior of two devastating quakes in Asia: the
1999 magnitude 7.6 temblor in Taiwan, and the 2011 magnitude 9.0
quake off the eastern coast of Japan.
In
both cases, the quake spread across so-called "creeping"
fault segments long thought to be incapable of transmitting quakes,
according to Caltech Staff Seismologist Kate Hutton, a Lapusta
colleague.
"The
general idea until this paper was that they would stop a quake,"
Hutton said.
It
was believed the slow, creeping movement prevents stress from
building up and keeps such a segment stable, Hutton added.
Lapusta
and Noda developed a computer model to explain how under certain
conditions "a rupture could just kind of barge right through,"
Hutton said. "Now the question is how this would apply to
California."
Such
a creeping zone has been identified in a stretch of the San Andreas
Fault in central California, just north of seismically active
Parkfield.
The
Great San Francisco quake of 1906 occurred on the San Andreas north
of the creeping zone. The 1857 Fort Tejon quake occurred to the
south. No known quake has ever spanned across that creeping zone.
Whether
the model developed by Lapusta and Noda could apply there would
depend on local geological variables not yet completely understood,
Hutton said.
Responsible
for statewide emergency planning and disaster preparedness,
California's Emergency Management Agency (Cal EMA) is reviewing the
new study, according to spokesman Greg Renick. The agency already has
in place a plan for responding to a catastrophic quake in Southern
California, and another plan for the San Francisco Bay Area.
Cal
EMA anticipates that a catastrophic quake affecting a major
population center, much less two, will require response assistance
from outside California, and has established procedures in place.
Beyond that, Cal-EMA now intends to review the newly published
research to see if it exposes any gaps in the current response plans
that could be corrected before they’re needed, Renick said.
Every
fall, Cal EMA's Golden Guardian program creates a disaster scenario
for a multi-agency response drill. The scenario this year involves a
catastrophic quake in the San Francisco Bay Area. A magnitude 7.8
temblor on the southern section of the San Andreas was drilled in
2008.
Moderate
earthquake at the Mexico / Guatemala coast
In the greater Guatemala Champerico area ( destructive earthquake December 2012).
Why ? Because the distance to Champerico is rather limited and also becuase the earthquake’s epicenter in at approx. the same distance to the coast.
Reported depths are varying very much. USGS reported 90 km and EMSC 60 km, but it looks to be definitively in the deeper layers.
Hypocenters in the deeper layers are making it felt in a wider area but also considerably weaker than shallower quakes.
ER is convinced that this earthqake will NOT generate serious damage or injuries.
Update 17:06 UTC : We expect a max. MMI IV (light shaking) for a wide area around the epicenter. This is a typical subduction earthquake triggered by the Pacific Ocean plate moving (and hanging) below the North American Plate. When the stress becomes to big, an earthquake is generated. USGS reports a Magnitude of M5.1, EMSC M5.1, Geofon M5.3, INSIVUMEH M5.1 and SSN Mexico reports a M5.4 @ 27 km.
SRC
|
Location
|
UTC Date/time
|
M
|
D
|
INFORMATION
|
|
ER
|
I Felt A (not Listed) Strong Earthquake
|
Jan 11 23:59 PM
|
4.6
|
0.1
|
||
|
||||||
EMSC
|
Guatemala
|
Jan 11 20:32 PM
|
4.8
|
238.0
|
||
GEOFON
|
Mexico-guatemala Border Region
|
Jan 11 20:32 PM
|
4.8
|
236.0
|
||
USGS
|
Guatemala
|
Jan 11 20:32 PM
|
4.9
|
229.3
|
||
USGS
|
Offshore Chiapas, Mexico
|
Jan 11 16:30 PM
|
5.1
|
90.4
|
||
EMSC
|
Offshore Chiapas, Mexico
|
Jan 11 16:30 PM
|
5.1
|
87.0
|
||
GEOFON
|
Near Coast Of Chiapas, Mexico
|
Jan 11 16:30 PM
|
5.3
|
69.0
|
||
GEOFON
|
Northern Mid Atlantic Ridge
|
Jan 11 12:46 PM
|
4.6
|
10.0
|
||
EMSC
|
Northern Mid-atlantic Ridge
|
Jan 11 12:46 PM
|
4.6
|
10.0
|
||
GEOFON
|
Carlsberg Ridge
|
Jan 11 12:38 PM
|
4.6
|
10.0
|
||
EMSC
|
Carlsberg Ridge
|
Jan 11 12:38 PM
|
4.7
|
10.0
|
||
USGS
|
Carlsberg Ridge
|
Jan 11 12:38 PM
|
4.7
|
9.8
|
||
EMSC
|
Tonga
|
Jan 11 11:39 AM
|
4.8
|
10.0
|
||
GEOFON
|
Tonga Islands
|
Jan 11 11:39 AM
|
4.8
|
10.0
|
||
EMSC
|
Fiji Region
|
Jan 11 09:47 AM
|
4.8
|
386.0
|
||
USGS
|
Fiji Region
|
Jan 11 09:47 AM
|
4.8
|
388.5
|
||
GEOFON
|
Fiji Islands Region
|
Jan 11 09:47 AM
|
4.9
|
370.0
|
||
EMSC
|
Andaman Islands, India Region
|
Jan 11 09:10 AM
|
5.0
|
35.0
|
||
USGS
|
Andaman Islands, India Region
|
Jan 11 09:10 AM
|
5.0
|
34.2
|
||
GEOFON
|
Andaman Islands, India Region
|
Jan 11 09:10 AM
|
4.9
|
10.0
|
||
EMSC
|
Off W. Coast Of N. Island, N.z.
|
Jan 11 05:35 AM
|
4.6
|
11.0
|
||
USGS
|
Off The West Coast Of The North Island Of New
|
Jan 11 05:35 AM
|
4.6
|
11.0
|
||
GEONET
|
Opunake
|
Jan 11 05:35 AM
|
4.6
|
11.0
|
||
GEOFON
|
Aegean Sea
|
Jan 11 00:30 AM
|
4.6
|
10.0
|
http://earthquake-report.com/2013/01/10/major-earthquakes-list-january-11-2013/
No comments:
Post a Comment
Note: only a member of this blog may post a comment.