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Scientists largely rejected Alfred Wegener's theory of continental drift due to the lack of a credible mechanism explaining how continents could move across the Earth's surface. Wegener proposed that continents plowed through oceanic crust, but this was inconsistent with the understanding of geology at the time. Additionally, there was insufficient evidence to support his claims, and many geologists favored the prevailing theory of static continents. It wasn't until the development of plate tectonics in the mid-20th century that Wegener's ideas gained acceptance.

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