Alfred Wegener called his theory Continental Drift, proposing that the continents were once part of a supercontinent named Pangaea and later drifted apart to their current positions.
Alfred Wegener called his theory Continental Drift. He proposed that the continents were once connected in a supercontinent named Pangaea and later drifted apart to their current positions. Despite facing skepticism initially, his hypothesis of continental drift has evolved into the Theory of Plate Tectonics, supported by evidence such as seafloor spreading and GPS data.
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