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Convergent Boundary: Continental- Continental No subduction

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Convergent Boundary: Continental- Continental No subduction

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Convergent Boundary: ocean- ocean with subduction

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Convergent Boundary: ocean- ocean with subduction

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convergent plate boundary two oceanic plates

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Divergent Boundary: ocean- ocean ( seafloor spreading)

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Divergent Boundary: ocean- ocean ( seafloor spreading)

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Convergent Boundary: ocean- continental with subduction

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Convergent Boundary: ocean- continental with subduction

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Divergent Boundary: Continental- Continental 

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Divergent Boundary: Continental- Continental 

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Convergent boundary: Continental- Continental No Subduction

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Convergent boundary: Continental- Continental No Subduction

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The plates moving the boundary are moving towards each other. The convection current causes 2 continental plates to come together. Both plates are the same density therefore no subduction occurs.

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Convergent Boundary: ocean- ocean with subduction

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Convergent Boundary: ocean- ocean with subduction

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The convection currents causes the 2 plates to come together. Under water mountains and volcanoes form. The plates move toward each other.

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Convergent Boundary: ocean- continental with subduction 

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Convergent Boundary: ocean- continental with subduction 

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The move towards each other. The convection currents cause the 2 ocean plates to come together. One plate is always older, colder and denser and dives under. Under water mountains and volcanoes form.

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Transformed boundary are sliding past each other. Convection currents move 2 plates ( ocean and continental) in opposite directions. Convection currents move 2 plates ( ocean or continental) in the same direction at different speeds.

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Divergent Boundary: Continental- Continental 

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Divergent Boundary: Continental- Continental 

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They are moving away from each other. Convection current pulls a continental plate a part. The convection current pulls the 2 ocean plates apart. Hot less dense magma rises in the crack

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Divergent Boundary: ocean- ocean ( seafloor spreading)

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Divergent Boundary: ocean- ocean ( seafloor spreading)

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The divergent plates are moving towards each other. The convection currents causes the 2 continental plates to come together. Both plates are the same density therefore no subduction occurs.