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Interior heat churns our living planet to self-renewal and drives its crustal plates. Earthquakes occur at their boundaries. Where an ocean ridge marks a spreading zone, upwelling molten rock makes new seafloor. Magma can also break through a plate at a hotspot, building volcanoes that plate motion carries away. When plates collide, continental crust crumples into mountains and the seafloor dives, creating a deep trench.
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