"Slow" Earthquakes May Help Predict Major Quakes
Iphtashu Fitz writes "Think all earthquakes last only seconds or minutes? Think again! Scientists at the University of Washington are measuring a "slow" earthquake some 12 to 25 miles underground that could last as long as a month. Along with the UW scientists, seismologists at the Geological Survey of Canada and Central Washington University have documented at least nine previous so-called slow earthquakes going back to 1992. They seem to occur every 14 months or so, the last one occuring in February and March of last year. These earthquakes, also known as slow-slip earthqakes, can release as much energy as a magnitude 6.8 earthquake but because it's released over such a long period of time nobody on the surface even notices it. One key question the scientists are trying to answer is whether these slow earthquakes add to or relieve stress in the tectonic plates, which could ultimately help to predict major earthqakes."
These earthquakes, also known as slow-slip earthqakes, can release as much energy as a magnitude 6.8
Does this not imply stress is being released?
I am a viral sig. Please help me spread.
From the Science Daily article..."Making that determination will help in understanding whether they are adding to or relieving stress in the Cascadia subduction zone off the Washington and B.C. coast, where the Juan de Fuca plate dives beneath the North American plate. The subduction zone is capable of generating great earthquakes, and scientists recently determined that a Cascadia earthquake in 1700 measured about 9.0 in magnitude."
And Wired... "The coastal region of northwest Washington state and southeast British Columbia is prone to earthquakes, and scientist warn the area gets hit with a devastating shake of magnitude 9 about every 500 years."
Sure.. we're only 196 years off the 500 year mark since the last 9.0, but for it only to pop up a few years ago makes it seem very ominous.
This data, while very interesting, could still go 2 ways. It is helping to alleviate and prevent major earthquakes in that area, or it's a major precurosr to a huge event that could happen in the near future. The hard part? What is considered teh near future... tomorrow? 5 years? 10 years? Guess we'll have to wait and see.
What's even more interesting is that I have yet to see any reports about this coming from any of the California plates, perhaps it hasn't been found or tested for or it's just not there.. Who knows.
Hmmm.
...to hear whether piezoelectricity can be used to detect quakes as well. With all of the smashing and crashing going on, one would think it would have the potential to generate radio waves such that a properly tuned instrument could receive|detect the signal.
ever mentions the fault line that runs along the Mississippi river? Didn't a major quake in the recent past cause the river to run backwards?
"I'm just here to regulate funkiness."
Can someone explain to me the difference in a 'slow earthquake' and just general plate movement? Cause from I just read, I couldn't differentiate between the two.
The seismic staff at the Pacific Northwest National Laboratory
We contribute to the UoW by maintaining the Eastern Washington Seismic Monitoring Network.
"Rocky Rococo, at your cervix!"
Wouldn't it do both. I.e. relieve stress in the spot that slipped, and add to stress in the spots where the plates are still binding?
Still, as far as I have seen the worst to hit North America since europeans settled here struck in a series between 1811 and 1812 near New Madrid, Missouri, one of which reportedly run church bells as far away as Washington DC.
Some day the big one will hit and all the land east of the San Andreas Fault will slide off into the Atlantic Ocean
A feeling of having made the same mistake before: Deja Foobar
Interview with a USGS official on "slow" quakes back in 1992. Click here!
Hmmm.
Just some guesses:
A "slow" quake could release stress along a certain section of the plates, but build up pressure along another section further away - thus leading to a large quake along the second section.
A "slow" quake could ramp up to a large quake if the slippage reaches a point where the plates have less friction against each other.
The faults don't only shift when a major earthquake occurs. A "slow" quake may shift the two plates closer to a point that can only shift through a large quake.
Obviously, IANAS or IANAG - and as neither scientist nor geologist - these are mere guesses based on what I do know of earthquakes.
I was taking one day at a time, but then several days got together and ambushed me. (from a Rhymes with Orange comic)
I believe a research into predicting earthquakes should be encouraged and given more funding. I am saying this because of my own experience. About 3 years ago, my city and lot of cities around my state experienced a major quake reading 7.8 (Bhuj quake in India) that killed more than 30,000 people. I was sleeping when this happened and it was terrifying. Never in my dream I had imagined my city was in earthquake prone zone. Looking at the rumble and bodies gave me shivers. I believe if such a thing is developed so many lives could be saved (if not property). Also this might help in identifying earthquake zones (if I remeber correctly they classify them in zones based on likelihood of having an earthquake) and that can give an impetus to civil authorities to build earthquake proof houses minimising property damage as well. Just my thoughts.
I'm from Costa Rica, which has its share of earthquakes. Common wisdom states that the earthquake cycle comes around every 30 to 40 years, and the lasts about 10 years. During that time, a couple of >6.0 earthquakes are expected. This works like clockwork. In 1910, an earthquake levelled the city of Cartago. More high profile earthquakes happened in the 50's, then 30 years of silence, and then the new wave started around 1984 and continued into the early 90's. It now appears to have subsided. In 1991, I experienced the might of a 7.1 quake. I almost crapped my pants.
The perfect sig is a lot like silence, only louder
...say to the other stress fracture during an earthquake?
"Hey, it's not my fault!"
look above. that's why I suggested piezoelectricity. Pressure can be exerted upon a rock (even by another rock) and it will generate radio waves. So when you're playing rock, paper, scissors, and the two rocks happen to generate enough pressure, it'd be a matter of trying to know what radio frequencies to know to monitor and get a signal. There are some obvious questions about this - in addition to whether it would work; how broad the frequency spectrum you'd have to monitor, how much lead time you'd get, if the intensity of the impending quake could be measured by the signal, and so on.
... but this whole Teutonic Plate Movement thing sounds kinda scary and images of blonde hair and blue eyes spring to mind.
Free Firefox news reader.
One key question the scientists are trying to answer is whether these slow earthquakes add to or relieve stress in the tectonic plates
I am by no means a geologist, but I'd speculate that the slow earthquakes (maybe earthquakes in general?) add stress to some plates and relieve stress in others, somewhat similar to the law of conservation of mass in physical science. That energy has to go somewhere...
This seems counter-intuitive. However, it isn't that far-fetched. Imagine a laterally moving or strike-slip fault (the notorious San Andreas fault is an example). Obviously, motion of the plates on wither side of the fault releases energy. The thing to focus on is what is happening at the ends of the fault. There, the faults can get locked into other plates, and motion causes a build up of stress as motion of one plate is blocked by a stationary plate. Some geologists are concerned that this is happening at the southern end of the San Andreas fault in the San Gorgonio Pass area and at the northern end at the Mendocino Triple Junction.
Some mornings it's hardly worth chewing through the restraints to get out of bed.
Why don't they just call their local psychic. There are even 1-800 numbers for that.
Evolution or ID?
Here and Here.
I was involved in planning for insurance company response to a quake on the New Madrid fault in the early 90's. Living in California, I'm used to quakes and have lived through some bad ones. A quake on the New Madrid fault would be a monumental disaster on many levels. First, as the writer above points out, the building is not to earthquake standards. Damage would be horrific. Places like Memphis would simple cease to exist.
Second, not only are codes inadequate, but the geology of the area contributes to the problem. The solid parent material (bedrock) allows propagation of the energy over a much wider area than in California. The historic New Madrid quakes cause church bells to ring in Boston. This coupled with the fact that many cities and towns are built on alluvial surface material that undergoes liquifaction during a quake means that once the energy reaches a remote area, it will still do a lot of damage.
Third, the extremely high market penetration of earthquake insurance in the commercial and homeowners insurance markets in the midwest means this would be a world-wide financial disaster far exceeding that of the 9/11/01 World Trade Center loss. Earthquake insurance in most midwest states is dirt cheap and has relatively low deductibles. Everybody has it. Here in California, it is expensive and has very high deductibles. Most people don't have it. If you do the math here, you are better off putting the money you would spend on premiums into mitigation efforts like foundation bolts, masonry reinforcements, etc. Our calculations in the 90's on the dollar loss from a repeat of the New Madrid quakes indicated that a Great Depression style financial collapse was not just possible, but likely.
This is seriously scary shit. The New Madrid Earthquake scare has passed, and not too many people in the midwest are doing any real earthquake planning. The next quake on the New Madrid fault will happen, we just don't know when.
Some mornings it's hardly worth chewing through the restraints to get out of bed.
http://quake.wr.usgs.gov/prepare/factsheets/NewMa
I'm moving.
Personally, I don't know why. I'd much rather deal with earthquakes than tornadoes. In an earthquake, your stuff falls into a nice neat little pile (at least before the ensuing fires engulf it). In a tornado, you, your family and your possesions are blown away into other states.
If you're really after the earthquake stuff, just read 'Basin and Range' and 'Assembling California.' (two of the four books that make up 'Annals of the Former World').
In these books, McPhee travels I-80 with a geologist who's an expert in the area they're covering. Each book is about the geology, the geologist, and the road trip. Great read, and you'll end up learning something, whether you intend to or not.
Never shake hands with a man you meet in a fertility clinic.