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There are several pieces of evidence from land features which support Wegener's idea of continental drift. One example is that if you line up the maps of South America and Africa you will see that the mountain ranges line up, which is strong evidence that the two continents were once one.
Identical fossils found on different continents, such as Africa and South America were strong evidence that they were once connected. Marsupials found in Australia also have direct links to ones found in North and South America.
The geographic distribution of the swimming reptile Mesosaurus provides evidence that supports continental drift. Fossils belonging to the Mesosaurus were found far away from each other, in both South Africa and South America.
South America and Africa fit together like puzzle pieces.
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The entire east coast of South America clearly appears to fit snugly with Africa's west coast.
One of the major evidence for the existence of Pangea is the shape of the continents. For instance, it looks very much like South America and Africa would fit together like two puzzle pieces.
Evidence to prove the existence of the supercontinent Pangaea includes fossil evidence of similar plant and animal species across continents, the matching shapes of coastlines and mountain ranges on different continents, and the distribution of ancient rock formations that line up when continents are fitted together. Additionally, geological evidence such as rock layers and paleoclimatic data also supports the theory of Pangaea's existence.
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The presence of similar fossils and rock formations on different continents, along with the matching shapes of the continents' coastlines like a jigsaw puzzle, supports the theory of continental drift proposed by Alfred Wegener in the early 20th century. This theory suggests that all the continents were once part of a supercontinent called Pangaea, which gradually broke apart and drifted to their current positions.
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