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Continental drift

Continental drift is a highly supported scientific theory, originating in the early 20th century, stating that Earth's continents move or drift relative to each other over geologic time. The theory of continental drift has since been validated and incorporated into the science of plate tectonics, which studies the movement of the continents as they ride on plates of the Earth's lithosphere.

History
Early history by Peter Paul Rubens, 1633 Abraham Ortelius , James O. Berkland argued that Reclus should be recognized "in the history of the development of plate tectonic theory as one of its foremost pioneers and, perhaps, as its founder". In 2021, Reclus, a tectonics database, was named for Elisée Reclus. Wegener and his predecessors Apart from the earlier speculations mentioned above, the idea that the American continents had once formed a single landmass with Eurasia and Africa was postulated by several scientists before Alfred Wegener's 1912 paper. Wegener was the first to use the phrase "continental drift" (1912, 1915) Willem van der Gracht was virtually the only tectonicist who supported mobilism. In 1939 an international geological conference was held in Frankfurt, organized by the fixist Hans Cloos, == See also ==
General and cited sources
• • • (pb: ) • • (First edition published 1570, 1587 edition online) • • . == External links ==
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