
metamorphic
Polished sodalite-bearing rock
Likely sodalite in a feldspar-rich host; exact rock identification is uncertain from the image
AI-generated identification · may be incorrectBlue sodalite patches with white, orange, and brown host minerals; polished, opaque surface and vitreous-to-greasy luster. Sodalite is typically Mohs 5.5–6, cubic, and has poor cleavage; the mixed specimen’s hardness varies by mineral.
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Physical properties
Blue sodalite patches with white, orange, and brown host minerals; polished, opaque surface and vitreous-to-greasy luster. Sodalite is typically Mohs 5.5–6, cubic, and has poor cleavage; the mixed specimen’s hardness varies by mineral.
Formation & geological history
Sodalite commonly crystallizes in silica-poor igneous rocks such as nepheline syenite and related metasomatic settings. Its geological age depends on the deposit; the pictured piece appears tumbled or polished.
Uses & applications
Used mainly for ornamental stone, cabochons, beads, and mineral collecting; sodalite is also used as a decorative dimension stone.
Geological facts
Sodalite is a sodium-aluminum silicate chloride, Na₈(Al₆Si₆O₂₄)Cl₂; its vivid blue color can resemble lapis lazuli, though it generally lacks abundant gold-colored pyrite.
Field identification & locations
Look for opaque royal-blue areas, often with white veining, alongside contrasting host minerals. Important sources include Canada, Brazil, Namibia, and Greenland; a definitive ID may require testing or mineralogical analysis.
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