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Mountain chains in Europe, particularly in the British Isles and Scandinavia, provide evidence for the existence of Pangaea through their geological similarities and alignment. The Caledonian mountain range, which extends from Scotland to Scandinavia, showcases similar rock types and ages, indicating they were once part of a continuous landmass. Additionally, the distribution of fossils and geological features across these regions supports the idea that these areas were connected before the continents drifted apart during the formation of Pangaea. This evidence highlights the historical geological processes that shaped the continents and their current configurations.

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AnswerBot

6d ago

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