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- An ophiolite is a section of Earth's oceanic crust and the underlying upper mantle that has been uplifted and exposed, and often emplaced onto continental crustal rocks. These rocks are an altered form of basalt and are often green. Ophiolites are found in mountain belts such as the Alps or the Himalayas, and they provide insight into the dynamics of oceanic crust formation and tectonic processes1234.Learn more:✕This summary was generated using AI based on multiple online sources. To view the original source information, use the "Learn more" links.An ophiolite is a section of Earth's oceanic crust and the underlying upper mantle that has been uplifted and exposed, and often emplaced onto continental crustal rocks. The Greek word ὄφις, ophis (snake) is found in the name of ophiolites, because of the superficial texture of some of them. Serpentinite especially evokes a snakeskin.en.wikipedia.org/wiki/OphioliteAn ophiolite is a section of the Earth's oceanic crust. The underlying upper mantle has been uplifted and exposed above sea level. The rocks which make up ophiolites are an altered form of basalt. The rocks are often green. They are found in the mountain belts such as the Alps or the Himalayas.simple.wikipedia.org/wiki/OphioliteOphiolites are sequences of mafic to ultramafic rock generally believed to represent ancient oceanic lithosphere. They are distributed all across the world being all of them located at present or past orogenic belts, sites of mountain building processes.en.wikipedia.org/wiki/List_of_ophiolitesIt is one of the world's largest and best-exposed segments of oceanic crust, made of volcanic rocks and ultramafic rocks from the Earth's upper mantle that was overthrust onto the continental crust. This ophiolite provides insight into the dynamics of oceanic crust formation and the tectonic processes involved in the creation of ocean basins.en.wikipedia.org/wiki/Samail_Ophiolite
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