discribe the theory of continental drift
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Continental drift is the theory that the Earth's continents have moved over geologic time relative to each other, thus appearing to have "drifted" across the ocean bed.[2] The speculation that continents might have 'drifted' was first put forward by Abraham Ortelius in 1596. The concept was independently and more fully developed by Alfred Wegener in 1912, but his theory was rejected by many for lack of any motive mechanism. Arthur Holmes later proposed mantle convection for that mechanism. The idea of continental drift has since been subsumed by the theory of plate tectonics, which explains that the continents move by riding on plates of the Earth's lithosphere.
This article is about the development of the continental drift hypothesis before 1958. For the contemporary theory, see plate tectonics. For the Russell Banks novel, see Continental Drift (novel). For the fourth film in the Ice Age franchise, see Ice Age: Continental Drift.
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According to the continental drift theory, in the early stage, around 300 million years ago, the earth's lithosphere was together as a single landmass. It was known as Pangaea. The Pangaea was surrounded by a hydrosphere known as Panthalassa.