Coast of Iceland
The Mid-Atlantic Ridge is primarily a Northern Hemisphere phenomenon. It's southern-most extent is found at Bouvet Island (Olavtoppen, 780 m, at 54°24′S 03°21′E), which is north of the Antarctic Circle.
The surface.
Mid-Ocean Ridge
Here are examples of a divergent boundary: The Mid-Atlantic ridge, Red Sea Rift, Baikal Rift Zone, East African Rift, East Pacific Rise, Gakkel Ridge, Galapagos Rise, Explorer Ridge, Pacific-Antarctic Ridge, and the West Antarctic Rift.
coast of Iceland
coast of Iceland
Coast of Iceland
The Mid-Atlantic Ridge is primarily a Northern Hemisphere phenomenon. It's southern-most extent is found at Bouvet Island (Olavtoppen, 780 m, at 54°24′S 03°21′E), which is north of the Antarctic Circle.
The Antarctic plate is the tectonic plate under the continent of Antarctica. It extends northward below the oceans to where it meets the Nazca, South American, African, Indo-Australian, and Scotia Plates and forms a divergent boundary along the Pacific-Antarctic Ridge.
The Antarctic plate is the tectonic plate under the continent of Antarctica. It extends northward below the oceans to where it meets the Nazca, South American, African, Indo-Australian, and Scotia Plates and forms a divergent boundary along the Pacific-Antarctic Ridge.
Pacific Ridge School was created in 2007.
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The surface.
It extends northward to its juncture with the Gakkel ridge, northeast of Iceland.
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Mid-Ocean Ridge