
mineral
Sodalite
Sodalite - Na8(Al6Si6O24)Cl2
Hardness: 5.5-6 (Mohs scale); Color: Royal blue to dark blue often with white calcite streaks; 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 often with white calcite streaks
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 5.5-6 (Mohs scale); Color: Royal blue to dark blue often with white calcite streaks; 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 (nepheline syenites and phonolites) through magmatic crystallization or metasomatism. It is a tectosilicate mineral that often occurs as mass fills in veins.
Uses & applications
Used primarily in jewelry as cabochons or beads, for ornamental carvings, and as a material for architectural surfaces (countertops). Also valued in crystal collecting and metaphysical markets.
Geological facts
Sodalite is often mistaken for Lapis Lazuli, but unlike Lapis, it lacks the golden pyrite inclusions and is generally less expensive. It is frequently nicknamed 'Princess Blue' because it was discovered in Ontario during a royal visit by Princess Margaret in the early 20th century.
Field identification & locations
Identify by its rich blue color and characteristic white calcite veins. Unlike Lapis, it has a lower specific gravity (it feels lighter) and no gold-colored specks. Large deposits are found in Bancroft, Ontario; Greenland; Brazil; and Namibia.
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mineral