Rock Identifier
Polished banded stone, likely labradorite or gneiss (Probably feldspar-rich gneiss; possible labradorite-bearing rock (plagioclase feldspar, chiefly (Ca,Na)(Al,Si)₄O₈)) — metamorphic
metamorphic

Polished banded stone, likely labradorite or gneiss

Probably feldspar-rich gneiss; possible labradorite-bearing rock (plagioclase feldspar, chiefly (Ca,Na)(Al,Si)₄O₈)

AI-generated identification · may be incorrect

Gray-green, rounded and polished, with pale and golden irregular bands or flashes; likely hardness 6–6.5, vitreous to dull luster, granular crystal structure, and poor cleavage visible only microscopically.

Identified More metamorphic
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Physical properties

Gray-green, rounded and polished, with pale and golden irregular bands or flashes; likely hardness 6–6.5, vitreous to dull luster, granular crystal structure, and poor cleavage visible only microscopically.

Formation & geological history

If gneiss, it formed by high-grade metamorphism of feldspar- and quartz-rich rock during Precambrian or younger mountain-building events. If labradorite-rich, the color play results from light interference in layered plagioclase crystals.

Uses & applications

Used as a decorative stone, cabochon, worry stone, or collectible; similar feldspathic rocks are also used for architectural slabs and aggregate.

Geological facts

The photograph is out of focus, so exact identification is uncertain; the golden-blue sheen may represent labradorescence rather than true banding.

Field identification & locations

Look for feldspar flashes that shift with viewing angle, a glassy feel, and resistance to scratching by a steel knife; common sources include Madagascar, Finland, Canada, Norway, and India. A gemological test or clearer image is needed for confirmation.