Originally posted by kennylee
reply to post by Roald
From what I gather from your post, along with westcoasts post, is that the Chile quake should have some effect on the west coast of US. And,
since we haven't seen that yet, then it could mean that if we do, then it will be a major release? I am honestly curious and trying to learn and I
thank you in advance for your reply.
Forgive me, but allow me to first just say that i believe that seismic waves, radiating from the earthquake rupture as deep and strong as M8.8, may
trigger an eruption in an volcano by stirring or shaking the molten rock beneath the volcano. The disturbances that result from this lead to eruption
but, because of the time it takes for pressure to build up inside a volcano and for magma to move towards the surface, an eruption may not occur until
some months after the earthquake
As an example, the great Chilean earthquakes in 1906 and 1960 (the largest earthquake ever recorded) were each followed by activity at six or seven
volcanoes – a significant increase on the average eruption rate of about 1 per year.
Until recently, scientists did not think major earthquakes could set off smaller tremors at distant locations. Then, in 1992, they found that
California’s magnitude-7.3 Landers earthquake set off small jolts as far away as Yellowstone National Park.
Now, to your first question.
Every so often, one large earthquake can trigger another. That happen because the first quake shifts stresses around in the Earth’s crust,
triggering other temblor.
Earthquakes aren’t random events -- they occur when stresses build up, so what i think happened in Chile was that the first quake occurred just like
any major thrusting earthquake, with the subducting plate lurching forward under the other plate. All those other quakes that still are shaking that
area is a direct result of this sudden movement.
I do believe that the passage of this seismic waves may change the water flow in a fault, possibly increasing the number of conduits that water can
flow through which could cause the fault to slip again, further "up". Surface waves might also increase the strain on a fault, or loosen a fault so
that it prematurely breaks or slides.
Generally a rupture will reduce the stress in the fault that's ruptured, but will increase it in other places, and all other things being equal,
we'll get more seismic quake activity in those places.
I also believe that the orientation of a fault—say, north-south or east-west—can affect how a fault responds to seismic stresses. Depending on the
orientation of a fault, it may be that the increase in stress produced by a past earthquake will move that fault closer to failure.
However, in a fault at another orientation, the change in stress could actually lengthen the time to the next earthquake or have no effect at all.
What I'm trying to say is that the activity outside Chile have released build-up stress in the trench/fault and that this release are still ongoing.
And that this release might increase the stress further up the Nazca Plate, which means that I expect to see a domino effect. Quakes moving towards
US.
So, would it result in a major release on the west coast of US?
I do not think so since we then have to pass the Cocos Plate.
The interaction between the Nazca Plate and the South American Plate, where the quakes now are rumbling, is what we call compressional, while the
boundary between the Nazca Plate and the Cocos Plate are extensional, meaning: they move away from each other.
Hope I did not make a fool of myself now. It's quite late here now. Almost 4am. Past my bedtime.