At one point, there was a single giant landmass known as Pangaea. This supercontinent existed during the late Paleozoic and early Mesozoic eras, approximately 335 to 175 million years ago. Over time, Pangaea began to break apart due to tectonic forces, leading to the formation of the continents we recognize today. The gradual drifting of these landmasses continues to shape Earth's geography.
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