The document discusses the continental drift theory proposed by Alfred Wegener in 1912, which suggested that all continents were once part of a single landmass called Pangaea. Wegener's theory, supported by evidence such as the fit of continental shapes, fossil similarities, and geological formations across continents, was initially disregarded by scientists due to a lack of explanation for the mechanisms of drift. Despite facing skepticism and not living to see his ideas gain acceptance, his work laid the foundation for modern plate tectonics.