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[[File:Mid-ocean_ridge_cut_away_view.png|left|Mid-ocean ridge cut away view|thumb]] [[File:World_Distribution_of_Mid-Oceanic_Ridges.gif|left|World Distribution of Mid-Oceanic Ridges|thumb|left]] [[File:(Manuscript_painting_of_Heezen-Tharp_World_ocean_floor_map_by_Berann).jpg|(Manuscript painting of Heezen-Tharp World ocean floor map by Berann)|thumb]] [[File:Mid-ocean_ridge_topography.gif|left|Mid-ocean ridge topography|thumb]] [[File:Þingvellir_National_Park,_Bláskógabyggð_(6969755432).jpg|Þingvellir National Park, Bláskógabyggð (6969755432)|thumb]] '''Mid-ocean ridges''' are underwater mountain ranges, formed by [[plate tectonics]]. These ridges are characterized by a [[rift]] at the summit, where [[magma]] from beneath the Earth's crust rises, cools, and solidifies to form new [[oceanic crust]]. This process, known as [[seafloor spreading]], occurs at divergent plate boundaries where tectonic plates move apart from each other.

==Formation and Structure==
Mid-ocean ridges are the result of [[mantle convection]] beneath the Earth's crust. As hot mantle material rises towards the surface at a divergent boundary, it decreases in pressure, melts, and forms magma. This magma then rises through the cracks in the Earth's crust, erupting as [[lava]] and solidifying to form new crust. The continuous addition of new material from below pushes the older crust away from the ridge, creating a pattern of symmetrical seafloor spreading on either side of the ridge.

The structure of a mid-ocean ridge includes the central rift valley, flanked by parallel mountain chains. The rift valley is the deepest part of the ridge, where the seafloor is actively spreading apart. The elevation of the ridge compared to the surrounding ocean floor is due to the buoyancy of the warmer, less dense newly formed crust.

==Global Distribution==
Mid-ocean ridges span about 65,000 kilometers (40,000 miles) across the Earth's oceans, making them the longest mountain range in the world. The most prominent is the [[Mid-Atlantic Ridge]], which extends from the Arctic Ocean to the southern tip of Africa. Other notable mid-ocean ridges include the [[East Pacific Rise]] and the [[Indian Ocean Ridge]].

==Ecology==
The unique environment of mid-ocean ridges supports diverse ecosystems. Hydrothermal vents, found near ridges, eject mineral-rich water that sustains communities of organisms adapted to extreme conditions. These ecosystems are notable for their lack of sunlight, relying instead on [[chemosynthesis]] for energy production.

==Exploration and Research==
Mid-ocean ridges have been a focus of oceanographic research since their discovery. They are key sites for studying [[plate tectonics]], [[volcanism]], and deep-sea ecology. Research is conducted using submersibles, remotely operated vehicles (ROVs), and seafloor observatories.

==Economic and Environmental Significance==
Mid-ocean ridges play a role in the Earth's [[geological cycle]], influencing the chemistry of the ocean and the atmosphere. They are also of interest for mining due to their rich deposits of minerals and [[rare earth elements]]. However, mining activities pose potential threats to the fragile deep-sea ecosystems.

==See Also==
* [[Plate Tectonics]]
* [[Seafloor Spreading]]
* [[Hydrothermal Vent]]
* [[Oceanography]]

[[Category:Oceanography]]
[[Category:Geology]]
[[Category:Plate Tectonics]]

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Mid-ocean ridge - Revision history

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