Rock Identifier
Weathered gray metamorphic rock, likely gneiss or schist (Probable quartz–feldspar–mica gneiss/schist; exact identification requires a fresh surface and tests) — metamorphic
metamorphic

Weathered gray metamorphic rock, likely gneiss or schist

Probable quartz–feldspar–mica gneiss/schist; exact identification requires a fresh surface and tests

AI-generated identification · may be incorrect

Gray, coarse-grained, weakly foliated appearance with tan weathering rind; likely Mohs 6–7, vitreous to dull luster, quartz/feldspar-rich with mica, and no obvious cleavage at this viewing angle.

Identified More metamorphic
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Physical properties

Gray, coarse-grained, weakly foliated appearance with tan weathering rind; likely Mohs 6–7, vitreous to dull luster, quartz/feldspar-rich with mica, and no obvious cleavage at this viewing angle.

Formation & geological history

Formed when preexisting igneous or sedimentary rock underwent substantial heat and pressure, producing recrystallization and foliation; age cannot be determined from the photograph and may range from Precambrian to younger.

Uses & applications

Commonly used as crushed aggregate, dimension stone, landscaping rock, and occasionally for decorative slabs; this weathered specimen has little commercial value.

Geological facts

Gneiss typically shows light–dark mineral banding, while schist has more conspicuous platy mica; the visible texture is consistent with either, but the image is insufficient for a confident species-level identification.

Field identification & locations

Look for planar mineral alignment, quartz hardness, feldspar grains, and mica flakes; a streak, acid test, fresh break, and hand lens would help distinguish it from granite or weathered basalt. Common worldwide in exposed mountain belts and continental shields.