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when Alfred Wegener proposed the theory of continental drift in 1912,
he was met with widespread skepticism from the geological community.
Many geologists were adamantly opposed to Wegener's theory, not because of sound scientific
counterarguments, but because it went against the then-accepted beliefs about stationary continents.
This dismissal persisted despite Wegener's substantial evidence,
and the theory was not widely accepted until the concept of plate tectonics emerged in the 1960s.