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_Seafloor Spreading_

1. Hot, molten rock is forced upward toward the seafloor at a mid-ocean ridge.

2. Molten rock pushes sideways in both directions as it rises, moving the mantle with it.

3. Molten rock flows onto the seafloor and hardens as it cools.

4. New seafloor moves away from the ridge, cools, becomes denser, and sinks.

- Maylin

_ Source_ Glencoe Textbook

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