
mineral
Polished labradorite cabochon
Labradorite, a calcic plagioclase feldspar; approximately (Ca,Na)(Al,Si)₄O₈
AI-generated identification · may be incorrectHardness 6–6.5 Mohs; dark gray to blue-gray with blue-green iridescent labradorescence, vitreous luster, triclinic crystal structure, and two good cleavage directions. The oval, domed shape indicates a polished cabochon.
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Physical properties
Hardness 6–6.5 Mohs; dark gray to blue-gray with blue-green iridescent labradorescence, vitreous luster, triclinic crystal structure, and two good cleavage directions. The oval, domed shape indicates a polished cabochon.
Formation & geological history
Forms in mafic igneous rocks such as basalt, gabbro, and anorthosite as magma cools; major deposits are Precambrian, especially Madagascar, Finland, Canada, and Norway. The specimen is human-cut and polished.
Uses & applications
Used for cabochon jewelry, carvings, ornamental objects, and mineral collections. Commercial value is driven chiefly by the strength, color, and coverage of its flash.
Geological facts
Its blue sheen is caused by interference and diffraction from fine lamellar intergrowths within the feldspar. Strong blue or multicolor flash is considered especially desirable.
Field identification & locations
Identify it by its dark body, feldspar-like cleavage, moderate hardness, and changing blue flash when tilted under directional light; avoid confusing it with glossy obsidian or coated glass.
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