
Mineral
Sodalite
Sodalite (Na8Al6Si6O24Cl2)
AI-generated identification · may be incorrectHardness: 5.5 - 6.0; Color: Royal blue to dark blue with white calcite veining; Luster: Vitreous to greasy; Crystal Structure: Isometric (cubic); Cleavage: Poor/indistinct; Specific Gravity: 2.27 - 2.33.
- Hardness
- 5
- Color
- Royal blue to dark blue with white calcite veining
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 5.5 - 6.0; Color: Royal blue to dark blue with white calcite veining; Luster: Vitreous to greasy; Crystal Structure: Isometric (cubic); Cleavage: Poor/indistinct; Specific Gravity: 2.27 - 2.33.
Formation & geological history
Formed in silica-poor igneous rocks such as nepheline syenites and phonolites, or in contact-metamorphosed calcareous rocks. It crystallizes from sodium-rich Magmas. Deposits vary in age from millions to over a billion years old.
Uses & applications
Used primarily in jewelry as cabochons or beads, ornamental carvings, and architectural finishing (slabs for countertops). It is a popular 'healing crystal' and a common specimen for educational mineral collections.
Geological facts
Sodalite is often confused with Lapis Lazuli, but unlike Lapis, it rarely contains golden pyrite inclusions. It is a major component of the rock 'Hackmanite', a variety that changes color when exposed to sunlight (tenebrescence).
Field identification & locations
Identify by its deep blue color and characteristic white streaks of calcite. Notably, most sodalite will fluoresce a bright orange-yellow under short-wave UV light. Common locations include Bancroft (Ontario, Canada), Namibia, Brazil, and Russia.
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