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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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His glasses slid down the ridge of his nose. I'll walk the ridge line today.


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The mid-ocean ridge are mountains that were formed underwater.


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The Mid-Atlanic Ridge is the divergent boundary that is responsible for seafloor spreading. Consisting mostly of divergent boundaries, with transform faults as well, this is the site where new oceanic crust is added, increasing the size of the ocean. This location is dotted with underwater volcanoes as igneous basaltic magma is added to fill in the gap left as the oceanic plates drift away.

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