Rock Identifier
Foliated metamorphic rock, likely gneiss or mica schist (Quartz–feldspar–mica metamorphic rock; exact identification is uncertain from the photograph) — metamorphic
metamorphic

Foliated metamorphic rock, likely gneiss or mica schist

Quartz–feldspar–mica metamorphic rock; exact identification is uncertain from the photograph

AI-generated identification · may be incorrect

Gray, white, and black banded material with a sparkly micaceous luster and irregular foliation; likely hardness about 5–7, with quartz and feldspar grains and mica cleavage. Specific gravity is approximately 2.6–2.8.

Identified More metamorphic
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Physical properties

Gray, white, and black banded material with a sparkly micaceous luster and irregular foliation; likely hardness about 5–7, with quartz and feldspar grains and mica cleavage. Specific gravity is approximately 2.6–2.8.

Formation & geological history

Formed when preexisting igneous or sedimentary rock underwent intense heat and pressure, recrystallizing and aligning minerals; commonly Precambrian to Paleozoic in age.

Uses & applications

Used as crushed aggregate, building stone, landscaping rock, and occasionally decorative dimension stone; attractive pieces may be collected but are generally low value.

Geological facts

Gneiss typically shows compositional banding, whereas schist has more strongly aligned, flaky mica; this specimen appears intermediate or weathered.

Field identification & locations

Look for alternating light and dark mineral bands, visible mica flakes, and a crystalline rather than glassy texture. Common in ancient mountain belts and glaciated terrains worldwide.