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Wegener's theory of continental drift gained acceptance in the 1960s primarily due to the development of plate tectonics, which provided a comprehensive framework explaining the movement of Earth's lithosphere. Advances in technology, such as sonar mapping of the ocean floor and the discovery of mid-ocean ridges, revealed evidence of seafloor spreading. Additionally, paleomagnetic studies showed that continents had shifted over geological time, supporting Wegener's ideas. This confluence of evidence from multiple scientific disciplines ultimately validated his theory.

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2w ago

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