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Both continental plates and oceanic plates float on the top of the mantle. Convection currents in the mantle rock cause the top surface of the mantle to move in different directions in different places. The continental plates and oceanic plates floating on the top of the mantle are dragged along in the direction of motion of the top of the mantle directly beneath them.

This process is part of the theory of plate tectonics, which explains many other things beyond the apparent movement of the continents.

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Q: What is the process in which continents move slowly?
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