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mid atlantic ridge; where is it possible to see a divergent boundary without having to go to the mid ocean ridges; why are divergent boundaries also considered constructive zones?; what plate boundary is the mid ocean ridge on; if a continental plate and a continental plate converge, a subduction zone forms.; transform plate boundary; convergent plate boundary; mid ocean ridge formation

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The Mid-Atlantic Ridge is a divergent plate divider line. The features on the ridge are the result of convection currents within the Earth that separate the North American and Eurasian plates.

New oceanic crust is created along the boundary by rising and solidifying magma. Perhaps the best known of the divergent boundaries is the Mid-Atlantic Ridge. This submerged mountain range, which stretches from the Arctic Ocean to beyond the southern tip of Africa, is just one segment of the global system of mid-ocean ridges that encircles Earth. A divergent boundary occurs when two tectonic plates move away from each other. Along these boundaries, earthquakes are common, and molten magma rock rises from the Earth's mantle toward the surface, solidifying to create new oceanic crust. The Mid-Atlantic Ridge is an example of divergent plate boundaries.

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