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LEFT: three basic types of plate interactions. RIGHT: results of stress building inside the plate |
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Oceanic floor split along the Mid-Atlantic ridge |
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Oceanic plate is sliding beneath the oceanic (LEFT) and continental (RIGHT) plates, forming a subduction zone. Diving plate melts and rising lava forms volcanic belts |
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Two continental plates slide horizontally, past one another, leading to the formation of fault (or transform-fault) boundary |
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LEFT: head-on collision between two contental plates. CENTER-RIGHT: collision of Indian subcontinent with Asia and Himalaya building |