Alfred Wegener first introduced the theory of continental drift in 1915, which proposed that the continents were once joined together in a supercontinent called Pangaea before slowly drifting apart. Wegener provided two key pieces of evidence to support this theory - the fit of the continental outlines and matching fossil records found on different continents. However, his theory was initially rejected because he could not explain the mechanism of how the continents moved. It is now accepted that the continents sit on tectonic plates that slowly move due to convection currents in the Earth's mantle, providing the explanation Wegener lacked.