Originally posted by Nyiah
o.O I could have sworn the Phillipine & Pacific plates subduct under the Eurasian plate, not the other way around.
That is correct. Well sort of. The further subdivision of the North American and Eurasian Plates into the Okhotsk, Amur, and Yangtze microplates can
confuse this issue, and is a more recent occurrence. For example, the Pacific plate is diving underneath the Okhotsk Plate, and the Okhotsk Plate
itself only recently acquired that name, as geologists were able to see that it apparently existed through study. Formerly, it was part of the North
American plate. Its very existence, or not, is the subject of scientific debate. But for the most part, it seems to be accepted as a microplate on its
own. But then you have people like PuterMan who don't believe in tectonic plate theory at all, or only in part.
The arrows at the plate boundaries on both the plate maps in this thread indicate the direction of subduction. In other words, those arrows indicate
which plate is diving under the other one. There is also another way of referring to them. In my example above, the Pacific Plate can also be called
the subducted plate, and the Okhotsk Plate called the subducting plate, because it is the Okhotsk Plate that is subducting down underneath it the
Pacific Plate.
There is also usually with many plate tectonic maps like this, a given rate of subduction in mm/year at the plate boundaries. That indicates how many
mm per year the subducted plate travels past the interface point, as it is diving under the other plate.
Massive megathrust earthquakes can occur when the upper lip of the subducting plate gets pulled down with the subducted plate and reaches a breaking
point when friction cannot hold it any longer. It springs back up violently, and if underwater, causes tsunamis.
At least that's the way I understand how it works. Anyway, yeah, Japan is probably one of the worst countries in the world in which to build nuclear
reactors, because of its precarious position on several plate boundary junction points. It has one of the highest rates of seismicity anywhere.
Another curious, little known phenomena can occur too at these critical plate boundaries, and they believe this happened in the 2004 Sumatra Quake
which caused that massive tsunami. It happens when a portion of that upper lip is weaker than the rest of the surrounding rock, and during the quake,
a piece of it all of sudden rises up sharply, and higher than the rest of the uplift. This can cause a tsunami itself that is higher than the rest of
the general tsunami. I believe it is called a splay fault, or something like that. In one report, a guy climbed up a tree on a hill to get away from
it, and said the wave STILL went over his head. But he clung on for dear life and survived. Geologists determined that portion of the wave reached
some 33 meters (or about 100 feet) high.
EDIT to answer questions below:
What are your thoughts and its eruption with the highest ever recorded ejection height of 3miles? And that in correlation to the plates which
will reverberate to Fukushima?
1. Well sometimes volcanoes erupt bigger than last time. Sometimes they don't. It's one of the deep mysteries of volcanic systems that is not well
understood- and mostly because there is a limit how far geologists can see what is really going on down there- way deep in the earth. Sometimes
magmatic systems get extremely recharged from deep in the earth, and sometimes they only get partially recharged. This can have a drastic effect on
the intensity of the eruptions, combined with a whole host of other influences- including magma composition, its related and particular degassing
regiments, and the role of hydrothermal features at the time.
2. Volcanic eruptions usually produce limited amplitude seismicity, which can only propagate so far. In this case, I believe there is not, and could
not be, any reasonable connection- because of sheer distance- between what is happening at that volcano, and what happens at Fukushima.
edit on
Mon Aug 19th 2013 by TrueAmerican because: (no reason given)