Continental drift is the movement of Earth's continents relative to each other, explained by plate tectonics.
Continental drift is the breakup and movement of the Earth's continents relative to each other by drifting across the ocean bed. The theory of plate tectonics explains how slow motions within Earth's mantle move large segments of the crust, resulting in a gradual 'drifting' of the continents and the formation of geological features.
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