
mineral
Tumbled blue glassy mineral, possibly sodalite or blue aventurine
Identification uncertain; likely sodalite (Na₈Al₆Si₆O₂₄Cl₂) or blue-dyed quartz/slag-like material
AI-generated identification · may be incorrectSmall polished fragment with deep navy-blue color, opaque to slightly translucent edges, and vitreous luster. Sodalite has Mohs hardness 5.5–6 and poor cleavage; quartz-based material is harder, about 7. The rounded shape indicates tumbling or abrasion.
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Physical properties
Small polished fragment with deep navy-blue color, opaque to slightly translucent edges, and vitreous luster. Sodalite has Mohs hardness 5.5–6 and poor cleavage; quartz-based material is harder, about 7. The rounded shape indicates tumbling or abrasion.
Formation & geological history
If sodalite, it formed in silica-poor, sodium-rich alkaline igneous rocks, commonly associated with nepheline syenite. If dyed quartz or industrial glass, it is human-processed; the photograph alone cannot distinguish these confidently.
Uses & applications
Used as a lapidary stone, bead, cabochon, or decorative tumbled specimen; sodalite is also collected for its blue color. Commercial value is generally modest.
Geological facts
Natural sodalite commonly shows white calcite veining, which is not apparent here. Uniform intense blue color and glassy fracture can indicate dyed quartz, glass, or slag rather than natural sodalite.
Field identification & locations
Check hardness with a steel file or quartz point, inspect for bubbles and conchoidal glass fracture, and use a streak test: sodalite typically gives a white streak. Common sodalite sources include Canada, Brazil, and Afghanistan.
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