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Originally posted by berkeleygal
major explosion now
webcam-svo2.pr.kyoto-u.ac.jp...
On Search live-cam: Sakura-jima (Japan)
Originally posted by tracehd1
reply to post by soficrow
I was wondering.. do you know if this volcano erupts much? Are you worried about it? just curious...thanks..
Originally posted by soficrow
...I do find it difficult to understand why some people say volcanic activity is NOT related to earthquake activity. Seems fairly obvious.
Originally posted by Essan
Originally posted by soficrow
...I do find it difficult to understand why some people say volcanic activity is NOT related to earthquake activity. Seems fairly obvious.
Are you suggesting the eruptions - which started in January - caused the later earthquake elsewhere in Japan?
Originally posted by tracehd1
reply to post by soficrow
I was thinking the same thing. What ever possessed them to build Nuke Plants on such un-stable ground?? I thought they were a smart people?
Originally posted by ZiggyMojo
I thought it was common knowledge that quakes triggered or were precursors to volcanic events. Yes, I know public school in the US is pretty much brainwashing and conditioning, but that is something I was taught in grade school clear through highschool. We covered the same topic in a Geology Class I took in College a few years back. There is definitely a link between volcanoes and earthquakes. If you don't believe that you haven't opened a science book in the past quarter century. I think it's clear that the two geologic events are directly connected.
Originally posted by tracehd1
reply to post by soficrow
That's interesting what you say... I'll have to look into that.
If a Nuke plant was built 30yrs ago... but never ran... does it still pose a huge danger? just curious...
Approximately 0.4% of explosive volcanic eruptions occur within a few days of large, distant earthquakes. This many “triggered” eruptions is much greater than expected by chance. Several mechanisms have been proposed to explain triggering through changes in magma overpressure, including the growth of bubbles, the advection of large pressures by rising bubbles, and overturn of magma chambers. Alternatively, triggered eruptions may occur through failure of rocks surrounding stored magma. All these mechanisms require a process that enhances small static stress changes caused by earthquakes or that can convert (the larger) transient, dynamic strains into permanent changes in pressure. All proposed processes, in addition to viscoelastic relaxation of stresses, can result in delayed triggering of eruptions, although quantifying the connection between earthquakes and delayed, triggered eruptions is much more challenging. Mud volcanoes and geysers also respond to distant earthquakes. Mud volcanoes that discharge mud from depths greater than many hundreds of meters may be triggered by liquefaction caused by shaking, and may thus be similar to small mud volcanoes that originate within a few meters of the surface. Changes in permeability of the matrix surrounding main geyser conduits, by opening or creating new fractures, may explain the observed changes in their eruption frequency.