
mineral
Labradorite
Plagioclase Feldspar (Ca,Na)(Al,Si)4O8
AI-generated identification · may be incorrectHardness: 6-6.5 on the Mohs scale, Color: Grey-green, dark grey, brown, or colorless with distinctive iridescent flashes of blue, green, gold, and orange (labradorescence), Luster: Vitreous to pearly, Crystal Structure: Triclinic, Cleavage: Perfect in two directions, Specific Gravity: 2.68-2.72.
- Hardness
- 6-6
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Physical properties
Hardness: 6-6.5 on the Mohs scale, Color: Grey-green, dark grey, brown, or colorless with distinctive iridescent flashes of blue, green, gold, and orange (labradorescence), Luster: Vitreous to pearly, Crystal Structure: Triclinic, Cleavage: Perfect in two directions, Specific Gravity: 2.68-2.72.
Formation & geological history
Forms in igneous rocks such as basalt, gabbro, and anorthosite, as well as in metamorphic rocks. It crystallizes from cooling magma and is commonly found in mafic intrusive and extrusive environments.
Uses & applications
Widely used in jewelry (pendants, rings, cabochons), ornamental objects, and as a decorative building stone due to its optical phenomenon.
Geological facts
Labradorite is famous for labradorescence, a unique optical effect caused by phase exsolution lamellae that diffract light. It was first discovered in Labrador, Canada, in 1770.
Field identification & locations
Easily identified by its dark grey base color combined with striking flashes of multicolored iridescence when turned in the light. Major deposits are found in Canada, Madagascar, Finland, Australia, and Russia.
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