
mineral
Blue sodalite bead necklace
Sodalite, Na₈(Al₆Si₆O₂₄)Cl₂
AI-generated identification · may be incorrectThe beads appear opaque, blue, and polished, but the image does not show enough detail to confirm sodalite; lapis lazuli or dyed stone are alternatives. Sodalite has Mohs hardness 5.5–6, a vitreous to greasy luster, and a cubic crystal structure; beads conceal cleavage and specific gravity is about 2.2–2.3.
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Physical properties
The beads appear opaque, blue, and polished, but the image does not show enough detail to confirm sodalite; lapis lazuli or dyed stone are alternatives. Sodalite has Mohs hardness 5.5–6, a vitreous to greasy luster, and a cubic crystal structure; beads conceal cleavage and specific gravity is about 2.2–2.3.
Formation & geological history
Sodalite forms in silica-poor, sodium-rich igneous rocks, especially nepheline syenites, during crystallization or alteration. Such rocks occur in geologically varied settings and ages.
Uses & applications
Sodalite is used as an ornamental stone and in beads, carvings, and decorative objects; it has limited industrial use.
Geological facts
Sodalite is a feldspathoid mineral, not a feldspar. Some sodalite-rich rock, notably lapis lazuli, contains pyrite and calcite.
Field identification & locations
Confirming the stone requires close inspection: sodalite is commonly deep blue with white veining and does not show lapis lazuli’s typical gold pyrite flecks. Similar-looking dyed stones are common in jewelry.
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