Single land mass, made up of all the present continents, believed to have existed between 300 and 200 million years ago; the rest of the Earth was covered by the Panthalassa ocean. Pangaea split into two land masses
Laurasia in the north and
Gondwanaland in the south which subsequently broke up into several continents. These then moved slowly to their present positions (see
plate tectonics).
The former existence of a single supercontinent was proposed by German meteorologist Alfred Wegener in 1912.
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