The document summarizes theories of continental drift and plate tectonics. In 1915, Alfred Wegener first proposed the theory of continental drift, which states that parts of the Earth's crust slowly drift atop a liquid core. Wegener hypothesized that around 200 million years ago, all the continents were joined together in a supercontinent called Pangaea. Pangaea later broke apart into smaller supercontinents, and by the end of the Cretaceous period the continents had separated into their modern positions. In the 1960s, Harry Hess proposed the theory of seafloor spreading, which provided support for continental drift by showing how ocean floors spread outward from underwater ridges. Plate tectonics expanded on these ideas