
mineral
Polished blue sodalite
Sodalite, Na₈(Al₆Si₆O₂₄)Cl₂, commonly with nepheline, calcite, or lazurite inclusions
AI-generated identification · may be incorrectTypically deep royal to denim blue with white or gray veining and a vitreous to greasy luster; hardness 5.5–6 on the Mohs scale, cubic crystal system, poor cleavage, and specific gravity about 2.27–2.33.
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Physical properties
Typically deep royal to denim blue with white or gray veining and a vitreous to greasy luster; hardness 5.5–6 on the Mohs scale, cubic crystal system, poor cleavage, and specific gravity about 2.27–2.33.
Formation & geological history
Forms in silica-poor, sodium-rich igneous rocks such as nepheline syenite and associated pegmatites. Most material is Cenozoic to Precambrian in age, depending on locality.
Uses & applications
Used as a decorative stone, cabochon, bead, tumbled stone, and ornamental carving material; it is generally less valuable than lapis lazuli but attractive in jewelry.
Geological facts
The blue color comes mainly from sulfur-related defects in the sodalite structure; white calcite veining is common and helps distinguish it from uniform blue stones.
Field identification & locations
Common sources include Canada, Brazil, Namibia, Russia, and the United States. Identify it by its opaque blue body, white veining, moderate hardness, and lack of the abundant golden pyrite typical of lapis lazuli.
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