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.
The length of the Explorer Ridge is 150 miles. This mid-ocean ridge is a divergent tectonic plate that is located near Vancouver Island in Canada.
The large island located on the Reykjanes Ridge is called Iceland. It is situated at the convergence of the Eurasian and North American tectonic plates, giving rise to its unique geological features like geysers and volcanic activity.
Older, as it moves away from the mid-ocean ridge the sediment gets thicker and older
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
Jamaica is the third largest Caribbean island. It was formed by a central ridge of metamorphic rock and volcanic activity.
The Mid-Atlantic Ridge is found on the ocean floor in the middle of the Atlantic Ocean.
Christmas Ridge underwater mountain is located in the Southern Ocean, east of the Antarctic Peninsula. It is part of the underwater mountain range known as the East Scotia 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.
The biggest island formed by the mid Atlantic ridge is Iceland.
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