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The Mid-Atlantic Ridge is an underwater mountain range that runs down the center of the Atlantic Ocean, marking the boundary between the Eurasian and North American tectonic plates to the north, and the African and South American plates to the south. It is a divergent boundary where new oceanic crust is formed as magma rises from the mantle, leading to volcanic activity and the creation of new seafloor. This geological feature plays a crucial role in plate tectonics and ocean circulation.

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