Rock Identifier
Sodalite (Na8(Al6Si6O24)Cl2 (Sodium Aluminum Silicate Chloride)) — mineral
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
Identified More mineral

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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.