1) Early scientists like Bacon and Snider-Pellegrini noticed similarities between continents like Africa and South America, but it was Wegener who first proposed the theory of continental drift in 1915. 2) Evidence for continental drift includes matching coastlines, similarities in fossils found on different continents, matching rock types along coastlines, and geological features lining up across continents. 3) In the mid-20th century, discoveries of seafloor spreading and plate tectonics provided the mechanism of plate tectonics to explain continental drift, with ocean floors being created at mid-ocean ridges and spreading outward over time.