The theory of continental drift, first posited by Alfred Wegener in 1912, contends that continents were once part of a singular landmass, referred to as Pangaea, surrounded by a mega-ocean called Panthalassa. Over 200 million years, Pangaea gradually split into separate continents that drifted to their current locations. Evidence supporting this theory includes the striking similarity in the shapes of coastlines like Africa and South America, matching geological formations across oceans, fossil distributions in separate continents, and climatic similarities indicative of past glacial activities. Additionally, the section discusses the concept of sea-floor spreading, leading to modern plate tectonics theory, which describes how tectonic plates move and interact, offering a dynamic understanding of geological phenomena on Earth.