The correct option is I, II, and III, all of which provide compelling evidence for the phenomenon of continental drift. The alignment of ancient rock formations, such as those found on the coast of Brazil and Western Africa, supports the theory that these continents were once joined, which is a fundamental tenet of continental drift. Additionally, the geological origins of gold deposits in Ghana being linked to the Brazil plateau suggest a shared geological history, reinforcing the idea of former land connections. Finally, the existence of similar Gondwana sedimentary systems across multiple Southern Hemisphere landmasses highlights the continuity of geological processes and species distribution, further validating the concept of continental drift as proposed by Alfred Wegener. These interdisciplinary connections in geology, paleontology, and geography form the basis for understanding the dynamic nature of Earth's continents over geological time.