The layers of rock formations, particularly the similarity of certain geological features and fossil distributions found in Africa, South America, India, and Australia, support the Continental Drift hypothesis. For instance, the presence of identical fossilized species, such as the Mesosaurus and Glossopteris, across these continents suggests that they were once connected. Additionally, matching rock strata and mountain ranges, like the Appalachian and Caledonian mountains, further indicate that these landmasses were part of a single supercontinent before drifting apart. This geological and paleontological evidence reinforces the idea of continental movement over time.
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