This document summarizes Alfred Wegener's theory of continental drift, which proposed that the continents were once joined together and have since drifted apart. Wegener noticed that the continents seemed to fit together like puzzle pieces. He gathered evidence from matching landforms, identical fossil distributions, and past climate patterns on separated continents to support his hypothesis of continental movement. While his theory was initially rejected due to lacking an explanation for the driving mechanism of drift, Wegener's extensive evidence helped revive consideration of plate tectonics and continental drift.