Alfred Wegener first proposed the theory of continental drift in 1912. He suggested that the continents were once joined together in a supercontinent called Pangaea, which later broke apart and drifted to their current positions. Wegener's theory was initially rejected by many scientists. However, the theory of plate tectonics later provided a mechanism - seafloor spreading - that explained how the continents could move over time. Today, the movement of continents via plate tectonics is well established in the scientific community.