Rock Identifier
Labradorite (Plagioclase Feldspar (Na,Ca)(Al,Si)4O8) — mineral
mineral

Labradorite

Plagioclase Feldspar (Na,Ca)(Al,Si)4O8

AI-generated identification · may be incorrect

Hardness of 6-6.5 on the Mohs scale, exhibits vitreous luster and a characteristic iridescent play of colors known as labradorescence. It crystallizes in the triclinic system with perfect cleavage in two directions.

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Physical properties

Hardness of 6-6.5 on the Mohs scale, exhibits vitreous luster and a characteristic iridescent play of colors known as labradorescence. It crystallizes in the triclinic system with perfect cleavage in two directions.

Formation & geological history

Forms primarily in mafic igneous rocks such as basalt and gabbro through slow cooling of magma, allowing the separation of lamellae that cause optical interference.

Uses & applications

Extensively used as a gemstone in high-end jewelry, carved into decorative objects, and occasionally as a dimension stone.

Geological facts

Named after the Labrador peninsula in Canada where it was first discovered in 1770. Its stunning iridescence is caused by light diffraction between microscopic mineral layers.

Field identification & locations

Readily identified by its dark grey to black body color combined with vibrant flashes of blue, green, or gold when rotated in light. Found in Canada, Madagascar, Finland, and Australia.