
mineral
Tumbled blue stone, likely sodalite
Sodalite (Na₈Al₆Si₆O₂₄Cl₂), possibly blue calcite or dyed quartz
AI-generated identification · may be incorrectOpaque to translucent medium-blue with whitish mottling and a polished/tumbled surface; sodalite has vitreous to greasy luster, hardness 5.5–6, cubic crystal structure, poor cleavage, and specific gravity about 2.2–2.4. The photograph alone cannot confirm identity; dyed stones are possible.
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Physical properties
Opaque to translucent medium-blue with whitish mottling and a polished/tumbled surface; sodalite has vitreous to greasy luster, hardness 5.5–6, cubic crystal structure, poor cleavage, and specific gravity about 2.2–2.4. The photograph alone cannot confirm identity; dyed stones are possible.
Formation & geological history
Natural sodalite forms in silica-poor, alkaline igneous rocks such as nepheline syenite, generally in Precambrian to younger alkaline complexes. Tumbled specimens are mechanically polished from rough fragments.
Uses & applications
Used as an ornamental stone, beads, cabochons, carvings, and inexpensive collector material; rarely used industrially.
Geological facts
Sodalite is commonly deep royal blue and may fluoresce orange under long-wave ultraviolet light. Lapis lazuli can look similar but usually contains visible gold-colored pyrite.
Field identification & locations
Check for white calcite veining, uniform blue dye concentration in cracks, hardness, and streak; localities include Canada, Brazil, Namibia, and Russia. A gemological test or chemical analysis is needed for certainty.
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