Rock Identifier
Purple fluorite cluster with metallic sulfide inclusions (Fluorite, calcium fluoride (CaF₂), likely with pyrite or chalcopyrite inclusions) — mineral
mineral

Purple fluorite cluster with metallic sulfide inclusions

Fluorite, calcium fluoride (CaF₂), likely with pyrite or chalcopyrite inclusions

AI-generated identification · may be incorrect

Typically Mohs hardness 4, vitreous luster, cubic crystal structure, and perfect octahedral cleavage; purple zoning is common. The specimen shows translucent purple cubic/blocky crystals with brassy metallic inclusions, though the exact sulfide cannot be confirmed from the image.

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Physical properties

Typically Mohs hardness 4, vitreous luster, cubic crystal structure, and perfect octahedral cleavage; purple zoning is common. The specimen shows translucent purple cubic/blocky crystals with brassy metallic inclusions, though the exact sulfide cannot be confirmed from the image.

Formation & geological history

Fluorite forms hydrothermally in veins and cavities associated with limestone, dolostone, and igneous rocks, commonly during relatively low-temperature mineralization. It occurs in many geological ages; locality and age cannot be determined visually.

Uses & applications

Used industrially as a flux in steel and aluminum production, and as a source of fluorine; attractive clusters are collected and occasionally used decoratively. It is generally not used as jewelry because of its softness and cleavage.

Geological facts

Purple color commonly results from radiation-related color centers or trace elements. Fluorite’s cubic habit and strong cleavage distinguish it from similarly colored quartz and amethyst.

Field identification & locations

Look for cubic faces, glassy luster, softness, and easy cleavage; a steel knife may scratch it, while quartz will not. Major localities include China, Mexico, England, Namibia, Morocco, and the United States.