The land feature that supports the theory of continental drift is oceans. The theory of continental drift suggests that Earth's continents were once joined together in a supercontinent called Pangaea, which has since broken apart and drifted to their current positions. The existence of matching geological features, such as similar rock formations and fossil records, on opposite sides of the ocean supports the idea that the continents were once connected and have since moved apart. This evidence is known as the "fit of the continents" and is a key piece of support for the theory of continental drift.
