Metamorphic rocks transform from existing rocks through mineral rearrangement caused by heat and pressure without melting the rock entirely.
Metamorphic rocks form through the physical and chemical alteration of pre-existing rocks, whether igneous or sedimentary. These changes occur due to increased temperature and/or pressure without fully melting the rock, resulting in rearrangement of minerals to form new minerals. For example, hornfels demonstrates how minerals rearrange themselves during metamorphism.
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