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Originally posted by masqua
If you happen to be watching the Iris Seismic Monitor, you'll notice a couple of pesky 4's and some smaller quakes just off Vancouver Island.
This has the markings of precurser and MSH has been more active recently.
www.iris.edu...
Page 114 Middle column : The key to this prospect lies in the innocent sounding realm of the study of fuel coolant interactions (FCIs), which can produce violent explosions of vapour with no chemical interactions involved. FCI's are a potential hazard in industries where hot and cold liquids may come into contact, such as the steel industry where molten steel mixes with water (* I actually remember these explosions as i lived near Port Kembla steelworks for many years). In that case the steel is the fuel and water the coolant but these terms are only relative. Another inductry, where care has been taken to avoid violent FCI explosions is the nuclear power inductry, where in some reactors liquid sodium is used as a coolant and the 'fuel' which might trigger the explosion would be molten uranium dioxide.
Even the more conservative volcanologists, setting a figure of 50 megatons to the size of the krakatoa eruption, would still be left with a power awesomely greater than any poor desperate states might otherwise be able to exploit and a temptation which, given the world situation outlined abovemust make this kind of interaction of serious interest in the world today (1978) Enough Volcanic islands exist around the world for the deliberate triggering of the next krakatoa to be physically possible.
Originally posted by Mayet
To us laymen who just study the plates as a hobby, the movements are obvious and yet no mainstream news is picking it up and saying Hey...........WTF.........
I don't think Mt St Helens is the topper, it seems to release it's pressure rather regular like,
A new volcano smack bang in the middle of area 51 would be kinda fitting wouldn't it
[edit on 10-3-2005 by Mayet]
Originally posted by Mayet
An interesting note ....the site quoted in the link of the article has now changed completely and wiped much of the information and changed it all around since I posted this article. Where it once showed the sharp rise in dramatic detail, the page is now somewhat higgledypiggeddy.
volcano.und.edu...
and the other link
www.volcanolive.com...
seems to be totally down.
[edit on 15-3-2005 by Mayet]