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When a rock metamorphoses physically, it typically undergoes changes in texture and mineral composition due to heat, pressure, or chemically active fluids. This process can lead to the formation of new minerals and the realignment of existing ones, resulting in a foliated or non-foliated structure. Common examples include the transformation of limestone into marble or shale into schist. These changes enhance the rock's durability and can significantly alter its appearance and properties.

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2w ago

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