Rock Identifier
Tumbled blue-gray mineral specimen, likely labradorite (Labradorite, a calcium-rich plagioclase feldspar; approximate formula (Ca,Na)(Al,Si)₄O₈) — mineral
mineral

Tumbled blue-gray mineral specimen, likely labradorite

Labradorite, a calcium-rich plagioclase feldspar; approximate formula (Ca,Na)(Al,Si)₄O₈

AI-generated identification · may be incorrect

Hardness 6–6.5 Mohs; blue-gray body color with possible blue-green iridescent sheen, vitreous to pearly luster, triclinic crystal structure, and two good cleavage directions. The rounded, glossy form indicates tumbling and polishing.

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Physical properties

Hardness 6–6.5 Mohs; blue-gray body color with possible blue-green iridescent sheen, vitreous to pearly luster, triclinic crystal structure, and two good cleavage directions. The rounded, glossy form indicates tumbling and polishing.

Formation & geological history

Labradorite crystallizes from cooling mafic igneous rocks such as basalt, gabbro, and anorthosite, commonly in Precambrian terrains. The specimen’s exact age and locality cannot be determined from the image.

Uses & applications

Used as a decorative stone, carvings, cabochons, jewelry, countertops, and mineral-collection specimens.

Geological facts

Its characteristic color flashes, called labradorescence, result from light interference within microscopic exsolution layers in the feldspar. Strong blue or multicolor flashes generally increase desirability.

Field identification & locations

Identify it by gray translucent-to-opaque feldspar, hardness near 6, cleavage, and changing blue flashes when rotated under a light; common sources include Madagascar, Finland, Canada, Norway, and Mexico.