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Originally posted by mrsdudara
Great photo justme. I love seeing comparison shots like that. Where did you find them? If you dont mind me asking.
Originally posted by Valhall
hey mrs! can you give the link for the rainier webcam? I have looked for this before and never been able to find it.
Thank you so much (in advance)!
Originally posted by mrsdudara
It looks like St. Helens is picking up Rainiers voice What is up with that? Surely that cant be right.....can it?
Rainier
St. Helens
It is clear on all the graphs, I just used these two for examples.
The problem this could reflect (IMHO) is that there is a wave traveling through a magmatic channel (i.e. same big pot of magma). Now, if MHS were to blow significant enough to have a large resultant magma flow, there could be the chance that a "draw" on Rainier could occur.
Now, in this post that I made many moon ago, I speculated on the thixotropy and gel strength that could possibly come into play in magma columns:
www.abovetopsecret.com...
Basically, if you take into account a magma column being "capped" by a thixotropic layer of magma, then what you're looking at is a stopper on top of a pressurized column of fluid. Now, the magma capping this isn't necessarily solid, but has achieved a sufficient gel strength to act semi-solid (read the above post). If a draw-down were to occur below this cap (i.e. some of the molten magma column were to be drawn toward MSH), then a dynamic flow situation would ensue below the cap. The evacuated region would cause an insufficient hydraulic head to maintain the pressurized column below.
So...if the ELP traces we are seeing are indications of communication between MSH and Rainier, I think it's worth keeping an eye on!
"It's certainly tempting to think there might be connection," Moran told the Seattle Post-Intelligencer. "But there's no evidence of any link between the two. ... They have completely separate plumbing systems."