It looks like you're using an Ad Blocker.
Please white-list or disable AboveTopSecret.com in your ad-blocking tool.
Thank you.
Some features of ATS will be disabled while you continue to use an ad-blocker.
Originally posted by BlackPhoenix
Man I hope if a big one is going to happen that it happens soon because my Dad and Stepmom are going on a two week cruise this time next month. I had a bad feeling when they told me they were going because I just know a big one is coming. I worry about a tsunami. Does anyone know if a tsunami way out in the open sea has any effect on a med size cruise liner? I want to tell them not to go but what if I'm wrong. Still I have a bad feeling.
Originally posted by TrueAmerican
lol WOQ!
On another note, anyone see any transform faults here?
neic.usgs.gov...
Ahh nope. Purple=subduction zone, green=transform fault, and ahh, I don't see no green. (At least not where others are reporting the northwestern side of that fault to be a transform fault, I don't.)
Just a note to the otherwise wise, making maps.edit on Sun Feb 10th 2013 by TrueAmerican because: (no reason given)
This earthquake is located adjacent to a complex section of the Australia-Pacific plate boundary, where the Solomon Trench to the west is linked to the New Hebrides (Vanuatu) Trench to the south by a short segment of dominantly strike-slip plate motion.
Thorne has been watching two enormous piles of rock that sit on the boundary between the core and the mantle. One pile is underneath the Pacific Ocean; the other under Africa. Scientists have known about them for 20 years, but Thorne saw something different. “I think this is the first study that might point to evidence that these piles are moving around,” Thorne says. Moving perhaps, but slowly and the piles are maybe 3,000 miles across. Thorne thinks, in fact, that the pile under the Pacific is actually two piles crushing up against each other.
Originally posted by Olivine
reply to post by TrueAmerican
This earthquake is located adjacent to a complex section of the Australia-Pacific plate boundary, where the Solomon Trench to the west is linked to the New Hebrides (Vanuatu) Trench to the south by a short segment of dominantly strike-slip plate motion.
Otherwise known as transform faulting.
Source
Cool graphics added to the summary page since Friday, too.
First posted December 19, 2011