Rock Identifier
Likely polished labradorite (small tumbled stone) (Labradorite, a plagioclase feldspar; approximately (Ca,Na)(Al,Si)₄O₈) — mineral
mineral

Likely polished labradorite (small tumbled stone)

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

AI-generated identification · may be incorrect

Gray-brown with a muted golden-blue sheen consistent with labradorescence; vitreous luster, triclinic crystals, Mohs hardness 6–6.5, and two cleavage directions. The photo is dim, so identification is uncertain.

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Physical properties

Gray-brown with a muted golden-blue sheen consistent with labradorescence; vitreous luster, triclinic crystals, Mohs hardness 6–6.5, and two cleavage directions. The photo is dim, so identification is uncertain.

Formation & geological history

Forms as calcium-sodium feldspar in cooling igneous rocks, especially anorthosite and gabbro; deposits occur in Canada, Madagascar, Finland, and elsewhere. Its age depends on the host rock.

Uses & applications

Used for polished specimens, beads, cabochons, and decorative stone; feldspar is also an important industrial raw material.

Geological facts

Labradorescence is produced by light interference within microscopic, layered structures in the feldspar.

Field identification & locations

Rotate it under a bright light: labradorite typically flashes blue, green, or gold across otherwise subdued gray surfaces. A photograph alone cannot confirm the mineral.