Alfred Wegener originally proposed the theory of continental drift in 1912, which explained that continents shift positions on Earth's surface over geological time. However, the theory was rejected by the scientific community at the time due to a lack of evidence. Wegener gathered evidence that the continents had moved around, including how the continents fit together, matching fossil and rock distributions between continents, and correlated ancient climate zones. The theory was finally accepted in the 1960s when the theory of plate tectonics was introduced and provided a mechanism for continental drift.