
mineral
Labradorite
Labradorite ((Ca, Na)(Al, Si)4O8)
AI-generated identification · may be incorrectHardness: 6-6.5 Mohs scale; Color: Dark gray to gray-black base with labradorescence (vibrant blue, green, or gold flashes); Luster: Vitreous to pearly; Crystal structure: Triclinic; Cleavage: Perfect in two directions; Specific Gravity: 2.68 to 2.72.
- Hardness
- 6-6
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6-6.5 Mohs scale; Color: Dark gray to gray-black base with labradorescence (vibrant blue, green, or gold flashes); Luster: Vitreous to pearly; Crystal structure: Triclinic; Cleavage: Perfect in two directions; Specific Gravity: 2.68 to 2.72.
Formation & geological history
Formed through the crystallization of mafic igneous rocks such as basalt or gabbro, or in metamorphic rocks. Most notable deposits date back to the Proterozoic eon. Significant deposits are found in anorthosite complexes.
Uses & applications
Primarily used as a gemstone in jewelry (cabochons, beads), decorative carvings, and as a high-end architectural facing stone (countertops or tiles) when found in large quantities known as 'Blue Pearl' granite (anorthosite).
Geological facts
First discovered in Labrador, Canada, in 1770. It is famous for its 'Schiller effect' or labradorescence, which is caused by internal light reflections from sub-microscopic layers of exsolution lamellae within the feldspar structure.
Field identification & locations
Field identification is based on the distinct iridescent play of color when rotated under light. It is commonly found in Canada (Labrador), Madagascar, Russia, and Finland (where the high-quality variety 'Spectrolite' is found). Collectors look for 'full-flash' specimens with minimal fractures.
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