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

Labradorite in Matrix

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

Hardness: 6.0-6.5 Mohs. Color: Gray-green to dark gray matrix with signature labradorescence (blue/green/gold sheen). Luster: Vitreous to pearly. Crystal structure: Triclinic. Cleavage: Perfect in two directions.

Hardness
6
Luster
Vitreous to pearly
Identified More mineral

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Physical properties

Hardness: 6.0-6.5 Mohs. Color: Gray-green to dark gray matrix with signature labradorescence (blue/green/gold sheen). Luster: Vitreous to pearly. Crystal structure: Triclinic. Cleavage: Perfect in two directions.

Formation & geological history

Forms in mafic igneous rocks such as basalt or gabbro, and specifically in anorthosites. It crystallizes from cooling magma and develops its characteristic iridescent lamellae through a process called subsolidus exsolution.

Uses & applications

Polished into gemstones for jewelry, carved into decorative objects, and used in high-end countertops or architecture. Large, rough specimens are popular for geological collections.

Geological facts

The optical effect 'labradorescence' is caused by light reflecting off microscopic layers of different feldspar compositions within the stone. Inuit legends state the northern lights were trapped within rocks until a warrior freed them with a spear.

Field identification & locations

Identify by rotating in the light to find the 'flash' of color (schiller effect) and checking for two planes of cleavage. Found commonly in Labrador (Canada), Madagascar, Finland (Spectrolite), and Russia.