If the continents were once joined together, rocks and mountain ranges on the margins of each

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The theory of continental drift, which posits that continents were once joined together in a single landmass and have since drifted apart, implies that rocks and mountain ranges on the margins of each continent would have formed under the same conditions, in the same sequences, at the same time, and with the same structural trends and forces, as they were part of the same geological processes before the continents separated.

If the Continents Were Once Joined Together, Rocks and Mountain