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Divergent Plate Boundaries (or How do you make an ocean?)

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The plates are sliding right past each other. When the convection currents move 2 plates (ocean or continental) in the opposite direction or in the same direction at different speeds.

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: plates slide past each other

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The plates are moving towards each other while the convection currents cause 2 continental plates to move closer together. Because both plates are the same density no subduction occurs and the 2 plates crumble up.

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The plates are moving towards each other while the convection currents cause the 2 plates to move towards each other. One plates is always older and more denser which allows it to dive under

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: the plates that move away

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The 2 plates are moving away from each other while the convection currents pull the 2 plates apart. Then, the magma rises in the middle, cools, hardens, sinks, forming a valley. When it fills in with water it becomes seafloor spreading.

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These 2 plates are moving away from each other and the convection currents pull the 2 ocean plates apart.

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: the plates dive under

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Convergent: 1 continental plate + 1 ocean plate

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Convergent: 1 continental plate + 1 ocean plate

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The plates are moving towards each other while the convection currents become denser ocean plates to dive under continental plates. Then, the ocean plate melts, forms magma, and that magma rises forming a volcano