Mountains composed of metamorphic rock can be found in several regions around the world, typically in areas with significant geological activity, such as tectonic plate boundaries. Here are a few notable locations:
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The Himalayas: This mountain range, which includes Mount Everest, is primarily made up of metamorphic rocks such as schist and gneiss, formed from the intense pressure and heat during the collision of the Indian and Eurasian tectonic plates.
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The Appalachian Mountains: Located in eastern North America, the Appalachians contain large areas of metamorphic rocks, including schist, gneiss, and marble, formed during the collision of tectonic plates millions of years ago.
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The Alps: This European mountain range features numerous metamorphic rocks, including gneiss, schist, and marble, formed during the collision of the African and Eurasian plates.
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The Rocky Mountains: Found in North America, particularly in Canada and the United States, the Rockies contain various metamorphic rocks alongside igneous and sedimentary formations.
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The Scottish Highlands: This region includes significant areas of metamorphic rocks, such as schist and gneiss, which were formed during the Caledonian orogeny.
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The Andes: In South America, the Andes mountain range is primarily composed of igneous rocks, but there are also large areas of metamorphic rocks, particularly in regions that have undergone significant geological processes.
These mountains formed through processes that involve intense heat and pressure, often associated with tectonic movements, subduction, and continental collisions over geological time scales.