A ridge in the sea floor - for example, the Mid Atlantic Ridge, in the middle of the Atlantic Ocean - which is the site of formation for new tectonic plate material. When two plates move apart, a ridge often forms along the boundary where they are separating, filling in with magma and so forming new ground. Many of these ridges lie deep under the oceans.
A continuous ridge, or broad, fractured topographic swell, that extends through the central part of the Arctic, Atlantic, Indian, and South Pacific oceans. It is several hundred kilometers wide, and its elevation above the ocean floor is 600 m or more. The ridge marks a divergent plate boundary where new oceanic lithosphere is being formed.
A sinuous ridge rising from the deep-sea floor.
an drill sergeant underwater mountain range, formed by
an underwater mountain range, formed by plate tectonics
an underwater range, usually
Ridge on the ocean floor where two adjacent plates diverge and where new crust is generated by volcanic eruptions.
A long, narrow chain of underwater mountains formed when two of the earth’s plates meet and magma swells up to the surface to form a new sea floor.
A volcanic mountain chain formed at the boundary between two oceanic tectonic plates.
A significant rise on the ocean floor, forming a long, linear ridge, often 4 km or so above the general level of the deep ocean floor. Oceanic ridges are associated with constructive plate margins.
One of any number of extensive underwater mountain chains which are found in the Earth’s oceans and mark the boundaries of many of the Earth’s continental plates