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There are several geological pieces of evidence that support the existence of the supercontinent Pangaea. Some of these include:
Fossil Evidence: The fossils of certain plant and animal species have been found on continents that are now separated by vast oceans. For example, the reptile Mesosaurus, whose fossils have been found in South America and Africa, indicates that these two continents were once connected.
Mountain Belts: The Appalachian Mountains in North America are part of a larger mountain belt that extends into Europe and Africa. The similarity of the rock types, structures, and ages of the Appalachian Mountains and those in other continents is consistent with the idea of Pangaea.
Glacial Evidence: Glacial deposits from the late Paleozoic Era, such as tillites and dropstones, have been found in areas that are now widely separated. These deposits indicate that a large ice sheet covered the southern polar region and that the continents were once joined together in a single landmass.
Paleoclimatic Evidence: The distribution of certain sedimentary rocks, such as coal deposits, suggests that the climate was once much warmer in areas that are now located far from the equator. This is consistent with the idea that the continents were once joined together and that the distribution of land masses influenced global climate patterns.
These are just a few examples of the geological evidence that supports the idea of Pangaea.
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