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

Labradorite

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

AI-generated identification · may be incorrect

Hardness of 6 to 6.5 on the Mohs scale, typically gray-green to dark grey with distinctive chatoyancy or labradorescence showing iridescent blue and gold flashes, vitreous luster, and perfect cleavage in two directions.

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Physical properties

Hardness of 6 to 6.5 on the Mohs scale, typically gray-green to dark grey with distinctive chatoyancy or labradorescence showing iridescent blue and gold flashes, vitreous luster, and perfect cleavage in two directions.

Formation & geological history

Forms in mafic igneous rocks like gabbro, basalt, and anorthosite through slow cooling of magma deep within the Earth's crust.

Uses & applications

Used primarily as a decorative dimension stone, in high-end jewelry, and as a popular collector specimen due to its optical phenomenon.

Geological facts

First discovered on Paul Island in Labrador, Canada, in 1770, labradorite's colorful flash is caused by light interference within microscopic lamellar intergrowths.

Field identification & locations

Readily identified in the field by its distinct lamellar twinning striations on cleavage planes and characteristic dark body color with colorful spectral flashes. Commonly sourced from Canada, Madagascar, and Finland.