Continental drift was a groundbreaking hypothesis that explained how continents move over the Earth's surface. Alfred Wegener, a geophysicist and meteorologist, proposed the hypothesis in 1912, but it was dismissed by conventional science at the time..8



The rocks developed side by side, according to Wegener, and the land has subsequently drifted apart. Mountain ranges with the identical rock kinds, structures, and ages are now on opposing sides of the Atlantic Ocean. Mountain ranges in eastern Greenland, Ireland, the United Kingdom, and Norway, for example, are similar to the Appalachians in the eastern United States and Canada. Wegener came to the conclusion that they originated as a one mountain range that was split apart as the continents moved apart.