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... energy under the earth's crust reaches a certain peak, the continents begin to break up.
Because the warmer rock is less dense, it will be lifted to a higher height relative to the surrounding rock.
The cooler temperatures in these higher regions kept the ice from melting, perhaps explaining many of the Ediacaran glaciers.
Land splitting creates new oceans, and seafloor spreading begins, creating a warmer, less dense oceanic crust.
Because of the lower density, these ...
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