Thursday, September 2, 2010

more island arcs

An island arc is a curving series of volcanic islands that are created through the collision of tectonic plates in an ocean.The particular type plate boundary that yields island arcs is called a subduction zone. In a subduction zone, one lithospheric plate is forced downward under an upper plate. Continual tectonic movement pushes the lower plate deeper until it reaches a depth where temperatures are sufficient to begin to melt the subducted plate and form magmas. These magmas then rise through fractures and melt their way through the overlying crust to be extruded in the form of volcanoes. The volcanoes are generally andesitic in composition. If the overriding plate is oceanic, then volcanoes are extruded underwater and may eventually rise high enough to become islands. The volcanoes form in a line because the angle and rate of subduction, and hence the distance to the depth where melting occurs is consistent. Because the surface of Earth is curved, the line of volcanoes forms in an arcuate pattern in much the same manner as an arc is produced when a planar surface intersects a sphere.teehee.bye

5 comments:

  1. This was really hard to understand and i got boared at the middle but otherwise it was good. sorry...

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  2. HEY CHASEY! GOOD JOB BUT YE MAYBE SOME MORE PICS OR ANYTHING OTHER THAN THE GOOGLE IMAGES. KEPP IT UP! <3

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  3. Awesome chase gret job but 2 scientific lol:)

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  4. wow lots of info but i got bored. TOO many big words! but the inside a volcano part was cool.

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