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

Polished labradorite

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

AI-generated identification · may be incorrect

Hardness 6–6.5 Mohs; gray-green to smoky body color, vitreous luster, triclinic crystals, and two cleavage directions. The blue, green, and gold flashes are labradorescence caused by light interference in microscopic feldspar lamellae.

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Physical properties

Hardness 6–6.5 Mohs; gray-green to smoky body color, vitreous luster, triclinic crystals, and two cleavage directions. The blue, green, and gold flashes are labradorescence caused by light interference in microscopic feldspar lamellae.

Formation & geological history

Forms in mafic igneous rocks such as anorthosite, gabbro, and basaltic intrusions as molten rock cools; many gem-quality deposits are Precambrian. The pictured piece is shaped and polished.

Uses & applications

Used for cabochons, beads, carvings, ornamental stone, countertops, and mineral collecting. Strong, colorful labradorescence increases jewelry and collector appeal.

Geological facts

Labradorite is a variety of plagioclase feldspar, not a separate crystal system. Its optical flash changes dramatically with viewing angle and surface orientation.

Field identification & locations

Identify it by its dark gray body, feldspar cleavage, moderate hardness, and vivid angle-dependent flashes; common sources include Labrador, Canada, Madagascar, Finland, Norway, and Russia. It is softer than quartz, so avoid scratching and harsh abrasives.