What is evidence of contental drift?

Evidence of continental drift includes the matching geological features and fossil records found on continents that are now widely separated, such as the distribution of similar rock formations in South America and Africa. The presence of identical fossils, like those of the Mesosaurus, on different continents also supports the theory. Additionally, the fit of continental margins, particularly the Coastlines of South America and Africa, suggests they were once joined. Paleomagnetic data showing changes in Earth's magnetic field over time further corroborates the movement of continents.