The two continents that present mirror images of each other are South America and Africa. This is evident when observing their coastlines, which show striking similarities in shape, suggesting a possible connection in their geological history through continental drift.
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The two continents that present mirror images of each other are South America and Africa. This phenomenon is known as continental drift and is attributed to the movement of tectonic plates over geological time. When comparing the coastlines of South America and Africa, particularly along the Atlantic Ocean, their shapes appear remarkably similar, as if they were once connected. This resemblance suggests that these continents were once part of a larger landmass known as Pangaea, which began to break apart around 200 million years ago. Over time, the continents drifted apart due to the movement of tectonic plates, leading to the formation of the Atlantic Ocean. This process left behind geological features and coastlines that mirror each other, providing evidence for the theory of continental drift proposed by Alfred Wegener in the early 20th century.