
mineral
Sodalite
Na8(Al6Si6O24)Cl2 (Sodalite)
Hardness: 5.5 to 6 on Mohs scale; Color: typically deep blue with white veins of calcite; Luster: Vitreous to greasy; Crystal Structure: Isometric (cubic); Cleavage: Poor/indistinct; Specific Gravity: 2.27–2.33.
- Hardness
- 5
- Color
- typically deep blue with white veins of calcite
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 5.5 to 6 on Mohs scale; Color: typically deep blue with white veins of calcite; Luster: Vitreous to greasy; Crystal Structure: Isometric (cubic); Cleavage: Poor/indistinct; Specific Gravity: 2.27–2.33.
Formation & geological history
Forms in igneous rocks like nepheline syenites and phonolites through the cooling of silica-poor magmas. Often found in alkaline environments where sodium and aluminum are abundant but silica is scarce.
Uses & applications
Used primarily for ornamental purposes, jewelry (beads, cabochons), carvings, and as a decorative stone in architecture. Occasionally used as a pigment in painting.
Geological facts
Sodalite was first discovered in Greenland in 1811 but became extremely popular after large deposits were found in Ontario, Canada, in 1891. It is often called 'Princess Blue' after Princess Margaret of England visited the mines in Canada.
Field identification & locations
Identify in the field by its intense blue color and characteristic white streaks of calcite. Unlike Lapis Lazuli, it rarely contains golden pyrite flecks. Common locations include Canada (Bancroft), Namibia, Brazil, and Greenland.
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