Alfred Wegener first proposed his theory of continental drift in 1910. He noticed that the continents seemed to fit together like puzzle pieces. Wegener also presented three lines of evidence to support his theory: landforms on different continents matched up, matching plant and animal fossils were found on separated continents, and patterns of past climates did not match the continents' current positions. However, Wegener's theory was initially rejected because he could not explain how or why the continents would move. Wegener believed that evidence from all earth sciences was needed to understand the planet's past configurations and that new discoveries could alter conclusions.