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The gradual movement of the continents across the earth's surface through geological time.

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was a supercontinent that existed during the late Paleozoic and early Mesozoic eras.

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the remains or impression of a prehistoric organism preserved in petrified form or as a mold or cast in rock

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a slowly moving mass or river of ice formed by the accumulation and compaction of snow on mountains or near the poles.

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the glacial episodes during the Pleistocene period.

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each of several large landmasses thought to have divided to form the present continents in the geological past.

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German geophysicist who proposed the theory of continental drift (1880-1930)

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a continent or other large body of land.