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TECTONIC PLATE INTERACTIONS
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There are 3 types of tectonic plate interactions.
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Divergent Boundary- plates move away from each other
create new rock with volcanoes rift zone examples Mid-Atlantic Ridge & Great Rift Valley in eastern Africa earthquakes
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Convergent Boundary- plates collide, 3 of them due to the type of plate material
2 ocean plates (basalt) converge both will go down into the mantle destroying rock subduction zone trenches and volcanoes these volcanic islands are called island arc example- Japan earthquakes
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1 ocean plate (basalt) 1 continental plate (granite) converge
subduction zone- ocean plate will go down into the mantle destroying rock trenches and volcanoes these volcanic mountains are called a volcanic arc example- Andes Mountains earthquakes
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2 continental plates (granite) converge
neither goes down into the mantle folded mountains example- Himalayas earthquakes
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Transform Faults (strike-slip)
2 plates slide past each other horizontally no mountains are created earthquakes example- San Andreas fault
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