Continental drift explains how Earth's continents have moved relative to each other over time, with Pangaea being a significant part of this geological phenomenon.
Continental drift refers to the movement of the Earth's continents relative to each other over time. The supercontinent Pangaea existed around 200 million years ago when all present-day continents were united. This movement is supported by evidence such as the fit of continents, matching fossil records, and the study of plate tectonics.
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