Mid-ocean ridge

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What Wikipedia says

A mid-ocean ridge (MOR) is a seafloor mountain system formed by plate tectonics. It typically has a depth of about 2,600 meters (8,500 ft) and rises about 2,000 meters (6,600 ft) above the deepest portion of an ocean basin. This feature is where seafloor spreading takes place along a divergent plate boundary.

Excerpt from the Wikipedia article “Mid-ocean ridge”, under the CC BY-SA 4.0 license. Read the article on Wikipedia