
mineral
Sodalite
Na8(Al6Si6O24)Cl2 (Sodium Aluminum Silicate Chloride)
Hardness: 5.5-6.0 on Mohs scale; Color: typically royal blue, often with white calcite veining; Luster: Vitreous to greasy; Crystal Structure: Isometric; Cleavage: Poor; Specific Gravity: 2.27-2.33
- Hardness
- 5
- Color
- typically royal blue, often with white calcite veining
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 5.5-6.0 on Mohs scale; Color: typically royal blue, often with white calcite veining; Luster: Vitreous to greasy; Crystal Structure: Isometric; Cleavage: Poor; Specific Gravity: 2.27-2.33
Formation & geological history
Formed in silica-poor igneous rocks such as nepheline syenites and phonolites. It crystallizes from alkali-rich magmas or through hydrothermal replacement. It is often found in massive form rather than distinct crystals.
Uses & applications
Primarily used for ornamental purposes including beads, cabochons, carvings, and architectural tiles. It is also a popular collector's mineral and a source of sodium in certain industrial applications.
Geological facts
Sodalite was first discovered in Greenland in 1811 but became historically famous after a large deposit was found in Ontario, Canada, during a royal visit by Princess Margaret, leading it to be nicknamed 'Princess Blue.' It is often confused with Lapis Lazuli, but Sodalite lacks the gold pyrite inclusions and has a lower specific gravity.
Field identification & locations
Field identification is based on its deep blue color and the presence of white (Calcite) streaks. Unlike Lapis Lazuli, it will not have brassy pyrite specks. It is common in Bancrofter, Ontario; Brazil; Namibia; and Russia.
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