
mineral
Sodalite
Sodalite - Na8(Al6Si6O24)Cl2
AI-generated identification · may be incorrectHardness: 5.5-6.0 Mohs; Color: deep royal blue, grey, or purple with white calcite veins; Luster: Vitreous to greasy; Crystal Structure: Isometric (cubic); Cleavage: Poor; Specific Gravity: 2.27-2.33.
- Hardness
- 5
- Color
- deep royal blue, grey, or purple with white calcite veins
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 5.5-6.0 Mohs; Color: deep royal blue, grey, or purple with white calcite veins; Luster: Vitreous to greasy; Crystal Structure: Isometric (cubic); Cleavage: Poor; Specific Gravity: 2.27-2.33.
Formation & geological history
Formed in silica-poor igneous rocks such as nepheline syenites and phonolites. It occurs in hydrothermal environments and pegmatites through the cooling of alkaline magmas.
Uses & applications
Used primarily as an ornamental stone for carvings, beads, and cabochons in jewelry. It is also used as dimension stone for architectural accents and countertops.
Geological facts
Sodalite is often mistaken for Lapis Lazuli, but lacks the gold-colored pyrite inclusions. It was discovered in Greenland in 1811 and became famous after Princess Margaret of England chose it as a decorative stone for her home.
Field identification & locations
Identify in the field by its distinct rich blue color and white veins (calcite). It will often fluoresce a bright orange-red under ultraviolet (UV) light. Common locations include Canada (Bancroft), Namibia, Brazil, and Russia.
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