
mineral
Sodalite
Sodalite (Sodium Aluminum Silicate Chloride) - Na8(Al6Si6O24)Cl2
Hardness: 5.5-6.0 on Mohs scale; Color: Royal blue to gray-blue with white calcite inclusions; Luster: Vitreous to greasy; Crystal Structure: Isometric; Cleavage: Poor; Specific Gravity: 2.2-2.3.
- Hardness
- 5
- Color
- Royal blue to gray-blue with white calcite inclusions
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 5.5-6.0 on Mohs scale; Color: Royal blue to gray-blue with white calcite inclusions; Luster: Vitreous to greasy; Crystal Structure: Isometric; Cleavage: Poor; Specific Gravity: 2.2-2.3.
Formation & geological history
Formed primarily in igneous rocks that crystallized from sodium-rich magmas (nepheline syenites and phonolites). It is also found in contact metamorphic rocks. Deposits can vary in age from Proterozoic to Cenozoic.
Uses & applications
Used primarily as an ornamental stone, for carvings, beads, and jewelry. Also used as a decorative architectural stone for countertops or tiles when found in large blocks.
Geological facts
Sodalite is often confused with Lapis Lazuli, but it lacks the golden pyrite flecks found in Lapis. It was first discovered in Greenland in 1811 but became popular after large deposits were found in Ontario, Canada, in 1891.
Field identification & locations
Identify in the field by its distinct rich blue color and frequent presence of white calcite veins. It is commonly found in Brazil, Namibia, Canada (Bancroft), and Greenland. Collectors look for a deep blue color and fluorescence under UV light (it often glows orange).
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