The document discusses the concept of continental drift, initially proposed by Alfred Wegener in 1911, which describes how continents were once part of a supercontinent called Pangea and have drifted to their current positions over millions of years. It details historical observations, significance, and various clues such as shapes, fossils, climates, and rock formations that support the theory, while also noting the initial skepticism surrounding Wegener's ideas due to a lack of explanation for the mechanisms of drift. The conclusion emphasizes that paleomagnetic studies provide strong support for the theory, indicating that continents were joined over 200 million years ago.