It looks like you're using an Ad Blocker.
Please white-list or disable AboveTopSecret.com in your ad-blocking tool.
Thank you.
Some features of ATS will be disabled while you continue to use an ad-blocker.
Originally posted by dodadoom
Originally posted by beefytee
Originally posted by dodadoom
When we start seeing smoke and brimstone then we can start to worry?
(and coordinate evacuation plans)
[edit on 9-1-2009 by dodadoom]
No that's just a normal montana breezy day.
LOL, I'm pretty close, so I have to stay strapped down here too!
My windmills are puttin out some watts!
Just trying to gain some perspective here.
Which do I need to worry about more,
statistically speaking that is, An asteroid or volcano?
And getting hit by lightning? Car wrecks?
Please, this is as important as all your fancy talk
and high falutin' numbers and such!
Originally posted by startx.jeff
Originally posted by operation mindcrime
reply to post by Mushussu
.i've got beer
What kind of Beer?
Originally posted by geogeek
reply to post by Mushussu
i was also trying to imply ( i failed i guess in conveying intent) that we check the deformation readings to see if we can determine changing stresses / changes in the geometry, such that we can hypothesize something about earthquake movement . Please stop taking me so seriously, I'm harmless ...(if perhaps sometimes not explicit enough in my statements (comes from having never gone beyond 2 finger typing, and trying to economize on keystrokes) )
[edit on 9-1-2009 by geogeek]
[edit on 9-1-2009 by geogeek]
[edit on 9-1-2009 by geogeek]
Originally posted by nydsdan
I wonder if Indonesia will quiet down while another swarm heats up at Yellowstone? More importantly, once this swarm (if that is what it becomes - still early yet) calms down, does Indonesia get a more intense series?
Also, notice the straight line of quakes across NV? Interesting.
Does the full moon have anything to do with it?
Originally posted by operation mindcrime
could the current full moon (or atleast almost full??) be having any effect on any newly formed lava lake under YS??
[edit on 9/1/2009 by operation mindcrime]
Mantle plume minimising earthquakes.(WORLDWATCH)(Juan de Fuca tectonic plate)
Article from: Geographical
Seismic surveys of the Juan de Fuca tectonic plate, located off the northwest coast of the USA, have revealed that a giant magma chamber may be helping to reduce the rate and magnitude of earthquakes in the region.
Geologists from the University of California, Berkeley, have proposed that a large area of upwelling hot rock has effectively lubricated the movement at the plate's boundary as it subducts under the vast North American plate. This, they believe, has reduced the build-up of stress that often occurs along such zones and is released in the form of earthquakes when the plates suddenly slip and adjust to their ...
Originally posted by geogeek
reply to post by severdsoul
last time i saw anything from the volcanolgists, the debate was endless/ heated and conclusions (by mass acceptance) non-existent ....
Originally posted by severdsoul
Originally posted by geogeek
reply to post by severdsoul
last time i saw anything from the volcanolgists, the debate was endless/ heated and conclusions (by mass acceptance) non-existent ....
They may be right, i never really found any specific data saying either way. But it makes scene, Magma is melted ore, or rock, mixed with other stuff,
(love my technical terms. *lol*) Some of which are metal particles, which would make it react more to extra magnetic pull.
Although i really have no idea what i'm talking about, but it sounds plausable.
Mei Xue and Richard M. Allen
University of California, Berkeley
Abstract
Beneath the Pacific Northwest the Juan de Fuca plate, a remnant of the Farallon plate, continues subducting beneath the North American continent. To the east of the Cascadia subduction zone lies the Yellowstone hotspot track. The origins of this track can be traced back to the voluminous basaltic outpourings in the Columbia Plateau around 17 Ma. If these basalts are the result of a large melting anomaly rising through the mantle to the base of the North America continent, such as a mantle plume head, the anomaly would need to punch through the subducting Juan de Fuca slab. Here, we use teleseismic body wave travel time tomography to investigate the fate of the subducted slab and its possible interaction with a plume head. Our dataset is derived from the Oregon Array for Teleseismic Study (OATS) deployment in Oregon and all other available seismic data in this region. We image the subducted Juan de Fuca plate in the mantle east of the Cascades beneath Oregon, where the slab has not been imaged before, to a depth of 400 km but no deeper. The slab dips ~50 deg E and has a thickness of ~75 km. Immediately beneath the slab, we image a low velocity layer with a similar geometry to the slab and extending down to at least ~575 km depth in the VS model. The total length of the high velocity slab is ~660 km, about 180 km longer than the estimated length of slab subducted since 17 Ma. Assuming similar slab geometry to today, this 180 km length of slab would reach ~60 km depth, comparable to the thickness of continental lithosphere. We propose that the absence of the slab below 400 km today is due to the arrival of the Yellowstone plume head ~17 Ma, which destroyed the Juan de Fuca slab at depths greater than the thickness of the continental lithosphere. Given this scenario, the low velocity anomaly beneath the slab is likely the remnant plume head material which has been pulled down by traction with the subducting plate. The amplitude of the observed low velocity anomaly is comparable with that expected for plume head material 100-300 deg C hotter than the surrounding asthenosphere.