Understanding Mid-Ocean Ridges

Article by R. Elizabeth C. Kitchen (9,095 pts ) , published Sep 21, 2009

This article focuses on mid-ocean ridges. It will discuss what they are and what they do.

A mid-ocean ridge is simply a mountain underwater in the ocean. They are also sometimes referred to as mid-oceanic ridges. They typically contain a rift, which is a valley, running along their spine. These rifts are created by plate tectonics, which is the large scale motions of the lithosphere on Earth. A mid-ocean ridge is created by ocean floor spreading. This process is responsible for seafloor spreading. When a seafloor is uplifted due to convection currents which cause the mantle to rise as lava emerges. Once the lava cools, new crust is created resulting in mountains under the ocean.

Size

The world's mid-ocean ridges form a single global system and are all connected. This makes them the world's largest mountain range. Its total length is 49,700 miles.

Description

New crystallized magma is constantly forming new crust for the mid-ocean ridge. At ocean ridges the crust is constantly renewing itself. Mid-ocean ridges that spread more slowly tend to have wider, larger rift valleys. An example is the Mid-Atlantic Ridge. This ridges terrain is very rugged and the rift valleys can reach widths of ten to twenty kilometers with a ridge crest relief of nearly three-thousand feet.

Formation

Mid-ocean ridges are formed by two processes. These processes include ridge-push and slab-pull. The weight of a ridge will push away the remaining tectonic plate from the ridge, particularly towards what is known as a subduction zone. This is the ridge-pull process. The slab-pull process begins at the subduction zone. When a tectonic plate's weight is pulled below the above plate dragging the remaining plate behind it is the slab-pull process.

Discovery

Mid-ocean ridges were officially discovered in the 1950's. They were not discovered earlier because they are located deep within the ocean. When mid-ocean ridges were first discovered, scientists thought they were only in the Atlantic Ocean.

Today's Mid-Ocean Ridges

Chile Rise

Southwest Indian Ridge

Southeast Indian Ridge

Cocos Ridge

Central Indian Ridge

East Pacific Rise

Reykjanes Ridge

Chukchi Cap

Pacific-Antarctic Ridge

Alpha Ridge

Mid-Atlantic Ridge

Explorer Ridge

Juan de Fuca Ridge

Gorda Ridge

Mid-Arctic Ridge (also known as the Gakkel Ridge)

 
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