Well one of the nice things about monitoring two different networks (TA in Gee and WY from the UoU seismographs) is that when one of the WY goes
screwy, and there is not a corresponding event in Gee, then you can reasonably ascertain that it is a malfunction of some kind in the WY recorder. So
that's why anything like that doesn't phase me anymore, when I check the corresponding time location in Gee and there is nothing.
After reading a pretty good bit more (and thanks to all you guys providing links) it has become clear that any major quake (6.0+) up to 1200 km away
from Yellowstone may have an interactive effect with the caldera, and could potentially cause much further damage. So we better hope and pray this
does not happen. And interestingly, the Aleutian Islands, Alaska have been very active lately, with several 3.0+ quakes. And the activity in the
California area is notable as well.
The effects of dynamic interaction of such an event may not be evident for years though, so if one does happen close by it doesn't necessarily mean
that Yellowstone is going to erupt. It will not likely help matters any though, and the effects could be evident immediately to days, weeks or years.
So that is one thing concerning me right now: watching out for other large events within that 1200 km zone while there is clearly a disturbance of
some kind going on at Yellowstone. The most worrisome to me would be a large event (6.0+) anywhere within a 100 mile radius as far as immediate
dynamic interaction is concerned.
Another possibility is dynamic interaction with the known faults that lie close by. Should the activity at the caldera trigger or upset one of those
faults, it is possible then that a fault based quake could occur, which would then by sheer intensity pose a threat to the nearby caldera- potentially
rupturing something that would otherwise stay intact. So there's certainly a lot to consider, and much much more than this.
While volcanologists ponder the meaning of this swarm, a larger event within that perimeter may initially be overlooked as to significance. They are
no doubt monitoring gas emissions as well as ground deformation and other factors. So far from what I have gathered, there is not enough correlating
evidence, other than the swarm, that indicate an imminent eruption- and therefore the reason they have not raised the alert level. But another problem
is that the unique location of this swarm underneath the lake poses some unknowns.
Also, so did anyone get a good explanation of how to quickly convert from amplitude in microns/sec into Richter magnitude? Maybe RussianScientists
could offer up an explanation.
When the last 2.7 hit, I noticed in Gee that at H17A the scales on the left had to expand to 100 to display the wave. When the 2.5 hit shortly
thereafter, the scales expanded to 80. So as long as any new quake hits in that same area close by, it is reasonable to assume that the scale needs to
show at least 100 if the magnitude is beyond 2.7. Makes me wonder what the 3.9 looked like, and how far it expanded the scale.
[edit on 2-1-2009 by TrueAmerican]