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

Labradorite

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

Hardness: 6-6.5 Mohs. Color: Gray-green to dark gray with iridescent play of colors (labradorescence). Luster: Vitreous to pearly. Crystal system: Triclinic. Cleavage: Perfect in two directions. Specific gravity: 2.68-2.72.

Hardness
6-6
Luster
Vitreous to pearly
Identified More mineral

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Physical properties

Hardness: 6-6.5 Mohs. Color: Gray-green to dark gray with iridescent play of colors (labradorescence). Luster: Vitreous to pearly. Crystal system: Triclinic. Cleavage: Perfect in two directions. Specific gravity: 2.68-2.72.

Formation & geological history

Forms in mafic igneous rocks such as basalt, gabbro, and norite, as well as in some metamorphic rocks and anorthosites. Its unique iridescence is caused by the lamellar twinning of different feldspar compositions during cooling.

Uses & applications

Predominantly used as a gemstone in jewelry, for decorative carvings, as a collection specimen, and occasionally in high-end architectural tiles or countertops.

Geological facts

First identified in Labrador, Canada, in 1770. The spectacular flash of color is known as 'labradorescence' and is not a surface color but a light-scattering effect occurring within microscopic layers of the mineral.

Field identification & locations

Identify in the field by rotating the stone under light to see a sudden 'flash' of blue, green, or gold. Often found in Canada, Madagascar, Finland, and Norway. High-grade specimens from Finland are specifically called Spectrolite.