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Ann P
Ann P • 2 years ago

Chalcopyrite, known as the Peacock Stone to those in Arizona (a copper-iron sulfite material)

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Botryoidal minerals form when many nearby nuclei, specks of sand, dust, or other particles, are present. Layers of mineral material are deposited radially around the nuclei. As more material is deposited, the spheres grow larger and eventually overlap with those that are nearby. These nearby spheres are then fused together to form the botryoidal cluster.