
mineral
Fluorescent sodalite (hackmanite), likely a polished or tumbled specimen
Sodalite, Na₈(Al₆Si₆O₂₄)Cl₂; hackmanite is a sulfur-bearing variety
AI-generated identification · may be incorrectBlue-green fluorescence under ultraviolet light is visible; sodalite is typically blue with white veining, vitreous to greasy luster, and Mohs hardness 5.5–6. It has a cubic crystal structure and poor cleavage; the image alone cannot confirm the material or variety.
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Physical properties
Blue-green fluorescence under ultraviolet light is visible; sodalite is typically blue with white veining, vitreous to greasy luster, and Mohs hardness 5.5–6. It has a cubic crystal structure and poor cleavage; the image alone cannot confirm the material or variety.
Formation & geological history
Sodalite crystallizes in silica-poor igneous rocks, especially nepheline syenites; deposits formed at various geological ages. Hackmanite’s UV response is associated with trace impurities and defects in its crystal structure.
Uses & applications
Used as an ornamental stone, in carvings and jewelry, and as a mineral specimen; softer than many gemstones, so it is best protected from scratching.
Geological facts
Some sodalite fluoresces orange or pink under UV, while hackmanite can show reversible color change (tenebrescence). The strong cyan glow here may also come from another fluorescent mineral or a treated material.
Field identification & locations
Check for blue body color, white veining, and hardness near 5.5–6; a gemological test is needed for reliable identification. Sodalite occurs in Canada, Brazil, Greenland, and Namibia.
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