Rock Identifier
Likely weathered gneiss or mica-rich schist (Foliated metamorphic rock, probably quartz–feldspar–biotite gneiss/schist) — metamorphic
metamorphic

Likely weathered gneiss or mica-rich schist

Foliated metamorphic rock, probably quartz–feldspar–biotite gneiss/schist

AI-generated identification · may be incorrect

Gray, coarse-grained, irregularly foliated specimen with pale quartz/feldspar and dark mica or amphibole; likely Mohs hardness 5–7, vitreous to pearly luster, and no obvious cleavage at this scale.

Identified More metamorphic
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Physical properties

Gray, coarse-grained, irregularly foliated specimen with pale quartz/feldspar and dark mica or amphibole; likely Mohs hardness 5–7, vitreous to pearly luster, and no obvious cleavage at this scale.

Formation & geological history

Formed when pre-existing rock was subjected to elevated temperature and pressure during regional metamorphism, commonly hundreds of millions to billions of years ago. Exact identification and age require a closer, sharper view or laboratory testing.

Uses & applications

Generally used as decorative stone, aggregate, or landscape rock; this small piece has little commercial value but may be a useful teaching or collection specimen.

Geological facts

The planar light–dark banding or alignment of minerals records directed tectonic pressure and distinguishes foliated metamorphic rocks from many igneous rocks.

Field identification & locations

Common in mountain belts and exposed ancient continental shields worldwide. Look for mineral alignment, alternating light and dark bands, and resistance to scratching; a streak, hand lens, and fresh broken surface would improve identification.