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Metamorphic rocks are formed from existing rocks—either igneous, sedimentary, or other metamorphic rocks—under conditions of high temperature and pressure, typically deep within the Earth's crust. This process, known as metamorphism, causes physical and chemical changes in the rock's mineral composition and structure without melting it. Factors such as heat from nearby magma, pressure from tectonic forces, and chemically active fluids contribute to the transformation. Examples of metamorphic rocks include schist, gneiss, and marble.

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changing.


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