Longitude: 134°28'45.00"E
Quick poll: Who among you, of my scant readership, has ever heard of the country called Palau?
No one, right?
| © 2010 Matthias Schulz |
So where's the science in this? What does this have to do with plate tectonics?
Some years ago, Rep. Hank Johnson of Congress stated his fear that the small island of Guam would tip over and capsize if overpopulated. Let me clarify something for you: an island is not a floating land mass bobbing in the ocean like a cork. It is the summit of an underwater mountain that has jutted out from the surface of the water, mountains that would dwarf Everest if their bases were at sea level. None of them are planning to capsize anytime soon.
With that in mind, Palau is located right where two oceanic plates, the Philippine Sea and the Caroline, are converging. This is somewhat different than the interaction between the Indo-Australian and Eurasian plates, because the Caroline plate is actually being forced beneath the Philippine plate, or subducting. The crack between the two becomes a deep-sea trench - the Palau Trench. As the Caroline plate sinks deeper, the water it brings lowers the melting point of the mantle, or the layer of the Earth beneath the crust. Melting mantle becomes magma, and this magma rises up through the Philippine plate, cools, and forms a volcano. A chain of such volcanoes are formed, in fact, and this feature is called a volcanic island arc. If a tip sticks out of the water, it becomes an island, and Palau is one such tip. Yes, I am vacationing on a volcano right now - but so is anyone in Hawaii or Indonesia, just to name a few.
That, my friends, is a subduction boundary. Your brains fried? Maybe I should just explain with a nice diagram:
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| © 1984 Tasa Graphic Arts, Inc. |
That's all for today, folks. The sea beckons - I'm off to snorkel in the shallows and see fish and turtles and all that wonderfulness. Ak morolung!

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