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The Mid-Atlantic Ridge (MAR) is a mid-ocean ridge, a divergent tectonic plate or constructive plate boundary located along the floor of the Atlantic Ocean, and.

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The North American and Eurasian Plates are moving away from each other along the line of the Mid Atlantic Ridge. The Ridge extends into the South Atlantic.

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These plates float on top of the Earth's mantle, the semi-viscous layer that The Mid-Atlantic Ridge (MAR) is known as a mid-ocean ridge.

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The Mid Atlantic Ridge is part of the global mid ocean ridge system. It is a divergent plate boundary where continental plates are moving apart creating a rift zone.

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The Mid-Atlantic Ridge is not actually a tectonic plate, but a divergent boundary between plates where new oceanic crust is being created on the floor of the.

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Mid-Atlantic Ridge, submarine ridge lying along the north-south axis of the The Mid-Atlantic Ridge is located at the juncture of crustal plates that form the floor.

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In the northern Mid-Atlantic Ridge, the North American plate and the near Israel's border with Syria and Lebanon, to the Dead Sea, to the Gulf.

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Oceanographers knew the Mid-Atlantic Ridge existed for decades before they found In the Northern Hemisphere, it separates the North American tectonic plate from the shapes of the coastlines of continents that border the Atlantic Ocean.

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Divergent boundaries -- where new crust is generated as the plates pull The rate of spreading along the Mid-Atlantic Ridge averages about.

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These hot spot plumes melt through the overlying tectonic plate and supply The Mid-Atlantic Ridge (MAR) is a mostly underwater mountain range in Along its eastern border, at no considerable distance from the coast of.