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In mineralogy, a concentric texture describes roughly spherical layers arranged around a common center. This texture is observed in minerals like agate and within geodes, which are rock cavities lined with mineral material. These layers form due to successive depositions of material. Concentric textures can also refer to successive shells within individual crystals that differ in composition, reflecting changes in conditions during crystal growth. This textural feature provides insights into the geological processes and history of the mineral's formation.123

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