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The existence of the supercontinent Pangaea was first proposed by Alfred Wegener in 1912. He developed the theory of continental drift which suggested that the continents were once joined together in a single landmass before drifting apart to their current positions.
The existence of the supercontinent Pangaea was first proposed by Alfred Wegener, a German meteorologist and geophysicist, in 1912. Wegener's theory of continental drift suggested that the continents were once joined together in a single landmass before drifting apart over millions of years.
The existence of Rodinia, a supercontinent that existed during the late Precambrian period, was first proposed in the 1980s by geologist David L. K. Smith. His work, along with contributions from other researchers, helped to reconstruct the continental arrangement and support the idea of Rodinia's existence. Subsequent studies have further refined our understanding of its formation and breakup.
Supercontinent was first proposed in 1912 by the German meteorologist Alfred Wegener as a part of his theory of continental drift.
Dalton
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Ernest Rutherford
Wegener's theory of continental drift assumed the existence of one original supercontinent called Pangaea.
The existence of people in Holand is prehistorical.
Supercontinent was first proposed in 1912 by the German meteorologist Alfred Wegener as a part of his theory of continental drift.