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consructive plate boundary

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consructive plate boundary

movement of convection currents causes two plates to move away from each other and magma rises in the gap forming new land.

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destructive plate boundary

movements of convection currents pushes the continental and oceanic together. the oceanic crust is denser so it is pushed down into the mantle. this is called subduction

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conservative plate boundary

two plates slide past each other but they get stuck and over time pressure builds up and they move past each other

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collision plate boundary

two continental plates collide and they are both forced up and they form mountains

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