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Originally posted by JustMike
I've had some issues with GEE in the past couple of days so Murphy's Law being in effect, I wasn't running it and so I missed this quake entirely.
Originally posted by angelchemuel
Thay have settled on a 7.6!
Rainbows
Jane
reply to post by JustMike
4) I also wrote my reply to you so I could test out my new-style blinking, bright yellow "reply to" linky... (I believe it's the first one of its type on ATS but am willing to stand corrected.) 5) Ummm... I forget what number 5 was... Okay, back On Topic MamaJ, tsunamis can only be generated by undersea quakes if they meet certain conditions. Generally, there needs to be a large amount of thrusting to cause a major tsunami -- as was the case with Japan in March and also the huge quake of Dec 2004, for example. There are other undersea events that can cause tsunamis, such as the one off Newfoundland many years back that was triggered by an undersea landslide following a rather large quake. However, it seems to mostly be the result of megathrust events.
Originally posted by PuterMan
Foreshsocks? (No six actually so sixshocks? )
Interesting but maybe not that Elsenham (London way) has been taken off their drop down menu!
Originally posted by TrueAmerican
Originally posted by PuterMan
Foreshsocks? (No six actually so sixshocks? )
Well on a quake that "big" I keep waiting for the AFTERshocks.
But so far, not seeing much of nothing in GEE, although the long distance to my closest monitored station is probably affecting the ability to see them. Darn it, wish they'd fix RAO.
In July of this year, a M 7.6 event occurred approximately 45 km to the south-southwest of the October 21 earthquake, breaking a normal fault within the subducting Pacific plate also very close to the Kermadec Trench. This event was notable because it triggered a large number of thrust-faulting aftershocks to the west of the plate boundary, on or close to the interface between the Pacific and Australian plates. The October 21 earthquake may be related to that aftershock sequence.