Lots of things. Most of which are leading to the creation of new oceanic crust.
New crust is being formed.
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
no the mid- Atlantic ridge is a transform boundary
tectonic plates
volcanic activity
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.
Older, as it moves away from the mid-ocean ridge the sediment gets thicker and older
MidOcean Partners was created in 2003.
a rift valleyis a dip in the ocean floor a mid ocean ridge is a mountain chain formed on the ocean floor . Rift valley - divergent boundary MidOcean Ridge Convergent Boundary
Thermophiles, they live at the deep sea smokers and require heat to carry out their biological functions instead of sunlight.
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.
New crust is being formed.
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