Sodalite specimens for sale
5 for sale · $275–$2,500 USD
69 in the gallery
Sodalite is a blue to blue-gray feldspathoid mineral that forms cubic and granular habits with a vitreous to pearly luster. It is most recognized by its rich, uniform blue color often contrasted by white or lighter veining, and it commonly occurs in granular masses rather than sharp crystals. Notable localities include Afghanistan and Canada, where substantial specimen pockets showcase classic blue tones, while other sources such as Myanmar and the USA contribute material that displays strong color and good translucency in thin edges and clusters.
- Formula
- Na4(Si3Al3)O12Cl
- Rarity
- Common
- Stability
- Stable
- Collector interest
- High Interest
- Classification notes
- Feldspathoid silicate; Strunz 9.FA
Key characteristics
- Crystal system
- isometric
- Mohs hardness
- 5.5–6
- Specific gravity
- 2.27–2.33
- Luster
- vitreous, greasy
- Transparency
- transparent, translucent, opaque
- Color
- colorless, white, gray, blue, green, yellow, pink
- Streak
- white
- Cleavage
- poor
- Fracture
- conchoidal, uneven
- Crystal habit
- dodecahedral, granular, massive
- Gem mineral
- Fluorescent: orange, yellow
- Classic / historic
Buy Sodalite specimens
View all 5Where Sodalite is found
Top localities
- Ladjuar Medam26 specimens
- Sar-e-Sang6 specimens
- Dar-e-Zu mine5 specimens
- Poudrette Quarry4 specimens
- Badakhshan3 specimens
- Kokcha Valley3 specimens
- Kiran1 specimen
- Mogok1 specimen
About Sodalite
Collectors value sodalite for its striking hues and its association with other alkali feldspathoid minerals in igneous rocks. It is frequently cut into slabs and cabochons due to its relatively low hardness and pleasing color, making eye-catching display pieces and cluster specimens. While it can form sizable crystals in rare environments, more often it appears as dense aggregates that reveal its characteristic deep blue color when properly cut and polished, appealing to both mineral enthusiasts and display-focused collectors alike.











