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originally posted by: Olivine
Out of curiousity, what does the spectro look like of this low amplitude "stuff" beginning at 15:11 UTC until about 15:14?
(I'm looking at MLAC in GEE--nearest live seismo I've got access to)
Just background noise?
The recent swarm of quakes in and around the mountain is being tied to recent "volcanic unrest" marked by gas emissions and tree die-offs believed to be related to sheets of molten rock intruding upward and cutting off root systems, according to the USGS.
It is unclear whether the latest round of quakes is linked to the volcanic unrest, but USGS spokeswoman Susan Garcia said the region is "pretty active."
Scientists probe link between magnetic polarity reversal and mantle processes
by Staff Writers
Liverpool UK (SPX) Aug 03, 2012
Scientists at the University of Liverpool have discovered that variations in the long-term reversal rate of the Earth's magnetic field may be caused by changes in heat flow from the Earth's core into the base of the overlying mantle.
The Earth is made up of a solid inner core, surrounded by a liquid outer core, in turn covered by a thicker or more viscous mantle, and ultimately by the solid crust beneath our feet.
The magnetic field is generated by the motions of the liquid iron alloy in the outer core, approximately 3,000 km beneath the Earth's crust. These motions occur because the core is losing heat to the overlying solid mantle that extends up to the crust on which we live.
...
Dr Andrew Biggin, from the University's School of Environmental Sciences, said: "The magnetic field has undergone big changes in its behaviour that might be due to the mantle's controlling influence on the core.
In particular, we focused on the time interval between around 200 and 80 million years ago - when dinosaurs were still around - when the magnetic field initially started reversing its polarity very frequently. During this period the polarity was reversing up to 10 times every million years; however 50 million years later, it stopped reversing altogether for nearly 40 million years.
"When these changes in the magnetic field were taking place, the whole of the Earth's crust and mantle, including all of the continents, were undergoing a big rotation with respect to the geographic and time-averaged geomagnetic poles - the points defining the Earth's axis of rotation.
"We suspect that this process, called True Polar Wander and caused by the changing density distribution in the mantle, will have changed the pattern of heat flowing out of the core in such a manner as to cause the magnetic field to first become less stable, with lots of reversals, and then become much more stable - and stop reversing."
...
Plate tectonics may control reversals in the Earth's magnetic field
Oct 24, 2011
The Earth's magnetic field has reversed many times at an irregular rate throughout its history. Long periods without reversal have been interspersed with eras of frequent reversals. What is the reason for these reversals and their irregularity? Researchers from CNRS and the Institut de Physique du Globe, France, have shed new light on the issue by demonstrating that, over the last 300 million years, reversal frequency has depended on the distribution of tectonic plates on the surface of the globe. This result does not imply that terrestrial plates themselves trigger the switch over of the magnetic field. Instead, it establishes that although the reversal phenomenon takes place, in fine, within the Earth's liquid core, it is nevertheless sensitive to what happens outside the core and more specifically in the Earth's mantle. This work is published on 16 October 2011 in Geophysical Research Letters.
...
In conclusion, the degree of asymmetry has varied at the same rhythm as the magnetic reversal rate (number of reversals per million years). The two curves have evolved in parallel to such an extent that they can almost be superimposed. In other words, the further the centre of gravity of the continents moved away from the equator, the faster the rate of reversals (up to eight per million years for a maximum degree of asymmetry).
What does this suggest about the mechanism behind geomagnetic reversals? The scientists envisage two scenarios. In the first, terrestrial plates could be directly responsible for variations in the frequency of reversals: after plunging into the Earth's crust at subduction zones, the plates could descend until they reach the core, where they could modify the flow of iron. In the second, the movements of the plates may only reflect the mixing of the material taking place in the mantle and particularly at its base. In both cases, the movements of rocks outside the core would cause flow asymmetry in the liquid core and determine reversal frequency.
The earthquakes themselves are small, brittle-failure (rock breaking) events. Such events are sometimes called "tectonic." The earthquakes do not result from the underground movement of magma.
originally posted by: NarcolepticBuddha
a reply to: TrueAmerican
Forgive my ignorance, and I AM speaking from a position of ignorance...
Aren't quakes in the 3.0-3.5ish region barely perceptible?..the kind of quakes most people don't notice and/or sleep right through?
I just always wonder why people look at these little quakes as anything other than the Earth just doin' its thang. In my region, we get little swarms of this magnitude every so often and it's no big deal.
I guess what I'm asking is..why is this a "pretty serious swarm?" Sorry, it's just something I've always wanted to ask people who look out for 'quake activity.
originally posted by: Olivine
Well, this is only tectonic activity according to the news release on the CalVO front page.
The earthquakes themselves are small, brittle-failure (rock breaking) events. Such events are sometimes called "tectonic." The earthquakes do not result from the underground movement of magma.
originally posted by: TrueAmerican
originally posted by: Olivine
Well, this is only tectonic activity according to the news release on the CalVO front page.
The earthquakes themselves are small, brittle-failure (rock breaking) events. Such events are sometimes called "tectonic." The earthquakes do not result from the underground movement of magma.
Tectonic my ass.