Rock Identifier
Polished blue-gray stone, possibly labradorite or blue-gray granite (Uncertain from image; possible plagioclase-rich rock containing labradorite (NaAlSi₃O₈–CaAl₂Si₂O₈)) — mineral
mineral

Polished blue-gray stone, possibly labradorite or blue-gray granite

Uncertain from image; possible plagioclase-rich rock containing labradorite (NaAlSi₃O₈–CaAl₂Si₂O₈)

AI-generated identification · may be incorrect

Small, smoothly polished specimen with blue-gray to olive-brown coloration and reflective highlights. Likely Mohs hardness 6–6.5, vitreous to waxy luster, and no visible cleavage or crystal structure because the surface is polished.

Identified More mineral
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Physical properties

Small, smoothly polished specimen with blue-gray to olive-brown coloration and reflective highlights. Likely Mohs hardness 6–6.5, vitreous to waxy luster, and no visible cleavage or crystal structure because the surface is polished.

Formation & geological history

If labradorite-bearing, it formed by slow cooling of feldspar-rich igneous magma, commonly in Precambrian intrusive rocks. The specimen has been cut and polished; geological age cannot be determined visually.

Uses & applications

Used mainly as a decorative stone, cabochon, or mineral-collection specimen; labradorite is also used in jewelry and architectural accents.

Geological facts

The blue flash of labradorite is called labradorescence, produced by light interference within feldspar lamellae; the image does not show enough flash for confident identification.

Field identification & locations

Check for shifting blue, green, or gold flashes when tilted; test hardness against glass and inspect an unpolished edge for feldspar cleavage. Common sources include Madagascar, Finland, Canada, Norway, and the United States.