Rock Identifier
Polished labradorite cabochons (Labradorite, calcium-rich plagioclase feldspar (approximately (Ca,Na)(Al,Si)₄O₈)) — mineral
mineral

Polished labradorite cabochons

Labradorite, calcium-rich plagioclase feldspar (approximately (Ca,Na)(Al,Si)₄O₈)

AI-generated identification · may be incorrect

Dark gray to black, polished, with gray-blue iridescent flashes (labradorescence); hardness 6–6.5 Mohs, vitreous luster, triclinic crystal structure, two good cleavage directions, specific gravity about 2.68–2.72.

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Physical properties

Dark gray to black, polished, with gray-blue iridescent flashes (labradorescence); hardness 6–6.5 Mohs, vitreous luster, triclinic crystal structure, two good cleavage directions, specific gravity about 2.68–2.72.

Formation & geological history

Forms in mafic igneous rocks such as basalt, gabbro, and anorthosite as magma cools; most specimens formed during Precambrian to younger geological episodes. These pieces are cut and polished cabochons.

Uses & applications

Used for jewelry, carvings, cabochons, decorative stone, and collectors’ specimens; attractive blue or multicolor flash increases value.

Geological facts

Labradorescence results from light interference within microscopic exsolution layers in the feldspar, not from surface coating.

Field identification & locations

Identify by gray-black body color, cleavage, moderate hardness, and shifting blue-green-gold flash when tilted under a point light; major sources include Madagascar, Finland, Canada, Norway, and Russia.