mineral
Carved labradorite animal figurine
Labradorite, calcium-rich plagioclase feldspar (approximately An50–70; (Ca,Na)(Al,Si)₄O₈)
AI-generated identification · may be incorrectHardness 6–6.5 Mohs; dark gray to brown body color with blue-green iridescent labradorescence, vitreous luster, triclinic crystal structure, and two good cleavage directions. The shape is human-carved and polished.
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Physical properties
Hardness 6–6.5 Mohs; dark gray to brown body color with blue-green iridescent labradorescence, vitreous luster, triclinic crystal structure, and two good cleavage directions. The shape is human-carved and polished.
Formation & geological history
Labradorite crystallizes in slowly cooled mafic igneous rocks such as gabbro and anorthosite, generally in Precambrian to younger intrusive complexes. The color flashes result from light interference within microscopic feldspar lamellae.
Uses & applications
Used as an ornamental stone, cabochons, beads, carvings, and collectible figurines; not typically used as a construction stone when highly iridescent.
Geological facts
Its apparent blue flash is not a surface coating but structural iridescence called labradorescence. Strong color depends on viewing angle, polish, and lighting.
Field identification & locations
Identify it by rotating the polished surface under light: genuine labradorite shows directional blue, green, or gold flashes and feldspar-like cleavage. Important sources include Labrador, Canada; Madagascar; Finland; Norway; and Russia.