
mineral
Tumbled sodalite (probable)
Sodalite, Na₈(Al₆Si₆O₂₄)Cl₂; possibly blue-dyed jasper or lapis lazuli
AI-generated identification · may be incorrectBlue-gray, opaque, and polished with a vitreous-to-waxy luster; sodalite has Mohs hardness 5.5–6, cubic crystal structure, poor cleavage, and specific gravity about 2.2–2.4. The yellow-brown areas may be matrix or staining.
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Physical properties
Blue-gray, opaque, and polished with a vitreous-to-waxy luster; sodalite has Mohs hardness 5.5–6, cubic crystal structure, poor cleavage, and specific gravity about 2.2–2.4. The yellow-brown areas may be matrix or staining.
Formation & geological history
Forms in silica-poor, alkaline igneous rocks such as nepheline syenite, generally during Precambrian to younger alkaline magmatic events. Tumbled specimens are mechanically polished from mined rough.
Uses & applications
Used mainly as an ornamental stone, cabochon, bead, and inexpensive collector specimen; rarely used for industrial purposes.
Geological facts
Sodalite is commonly deep royal blue with white calcite veining, while lapis lazuli typically contains visible golden pyrite flecks. Reliable identification may require hardness, streak, or mineralogical testing.
Field identification & locations
Common sources include Canada, Brazil, Russia, and Namibia. Look for blue color, white calcite patches, and lack of metallic pyrite; avoid assuming identity from color alone because dyed stones resemble it.
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