Rock Identifier
Tumbled labradorite (Labradorite, a plagioclase feldspar: approximately (Ca,Na)(Al,Si)₄O₈) — mineral
mineral

Tumbled labradorite

Labradorite, a plagioclase feldspar: approximately (Ca,Na)(Al,Si)₄O₈

AI-generated identification · may be incorrect

Hardness 6–6.5 Mohs; typically gray to blue-green with vitreous luster and a triclinic crystal structure. The pale body and dark internal lines are visible here, though characteristic iridescent flashes are not apparent in this lighting.

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Physical properties

Hardness 6–6.5 Mohs; typically gray to blue-green with vitreous luster and a triclinic crystal structure. The pale body and dark internal lines are visible here, though characteristic iridescent flashes are not apparent in this lighting.

Formation & geological history

Forms as a feldspar in cooling igneous rocks, especially anorthosite and gabbro; specimens can be Precambrian, with age depending on their source deposit.

Uses & applications

Tumbled pieces are used in jewelry, ornaments, and mineral collections; labradorite is also used as decorative facing stone.

Geological facts

Its shifting, iridescent color effect is called labradorescence and comes from light interference within microscopic layers in the feldspar.

Field identification & locations

Often identified by gray feldspar with bright blue, green, or gold flashes when tilted under light. Major sources include Canada’s Labrador region, Madagascar, Finland, and Norway.