Pangea - pangea - Pangaea - Wikipedia

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Due to mantle convection within the Earth's surface new material constantly comes up between the Earth's tectonic plates at rift zones , causing them to move away from the rift and toward one another at the ends. In the case of Pangea, the Earth's continents were eventually moved so much over millions of years that they combined into one large supercontinent.

The theory of plate tectonics provides an explanation for these continent movements. According to this theory, Earth's outer shell is divided into a series of plates. These plates consist of the crust and a small amount of the underlying mantle. The plates slide over a weak zone in the mantle at a rate of a few centimeters per year. Convection currents in the mantle, caused by the escape of heat from Earth's interior, are what drives the movement of these plates.

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