Lots of things. Most of which are leading to the creation of new oceanic crust.
The mid ocean ridge separates many plates, not just two. In the Atlantic Ocean it separates the Eurasian and African plates from the North American Plate and the African Plate from the South American Plate. In the Indian Ocean it separates the African Plate from the Antarctic, Australian, Indian Plates and the Australian Plate from the Antarctic Plate. In the Red Sea it separates the African Plate from the Arabian Plate. In the Pacific Ocean it separates the Pacific Plate from the Antarctic, Nazca, Cocos, and Juan de Fuca Plates and the Nazca Plate from the Cocos and Antarctic Plates.
The Mid-Atlantic Ridge is a divergent tectonic plate boundary where the North American Plate and Eurasian Plate are moving away from each other as new oceanic crust is formed. This process leads to volcanic activity, earthquakes, and the formation of underwater mountain ranges along the ridge.
At any divergent plate margin: The Mid-Atlantic Ridge The boundary between the African Plate and Arabian Plate (the Red Sea) Great Rift Valley West Antarctic Rift East Pacific Rise Pacific-Antarctic Ridge Galapagos Rise Gakkel Ridge
Earthquakes along the Mid-Atlantic Ridge occur due to the movement of tectonic plates. The Ridge is a divergent plate boundary where plates are moving apart, causing stress to build up and eventually release as an earthquake. This process is part of the natural tectonic activity that shapes the Earth's surface.
An ocean ridge is most likely to be located at the boundary where two tectonic plates are moving apart, such as the Mid-Atlantic Ridge. This is where new oceanic crust is formed as magma rises to the surface and solidifies, creating a ridge-like structure along the seafloor.
Midocean ridges are areas where continents broke apart. Midocean ridges are closest to the landmasses in younger oceans. One example where a midocean ridge intersected a landmass is the Arabian sea, which was formed by the pulling apart of the Arabian Peninsula and Africa.
One of the midocean ridges is, but others are in other oceans, seas, and bays.
Along the Ridge was created in 2006.
The duration of Along the Ridge is 1.8 hours.
MidOcean Partners was created in 2003.
Older, as it moves away from the mid-ocean ridge the sediment gets thicker and older
The mid ocean ridge separates many plates, not just two. In the Atlantic Ocean it separates the Eurasian and African plates from the North American Plate and the African Plate from the South American Plate. In the Indian Ocean it separates the African Plate from the Antarctic, Australian, Indian Plates and the Australian Plate from the Antarctic Plate. In the Red Sea it separates the African Plate from the Arabian Plate. In the Pacific Ocean it separates the Pacific Plate from the Antarctic, Nazca, Cocos, and Juan de Fuca Plates and the Nazca Plate from the Cocos and Antarctic Plates.
Cemetary ridge
The midocean ridges are the spreading centers where the plates are moving apart. The seamounts are extinct volcanos produced as the plate passed over a mantle hotspot.
friction - convection currents in the mantle drag the plates away from the hot rising zone below the ridgegravity - gravity pulls down on the cold dense plate being subducted under the continent, dragging the plate away from the ridge
An arete is a mountain ridge that is steep sided and narrow along the ridge.
The Mid-Atlantic Ridge is a divergent tectonic plate boundary where the North American Plate and Eurasian Plate are moving away from each other as new oceanic crust is formed. This process leads to volcanic activity, earthquakes, and the formation of underwater mountain ranges along the ridge.