Rock Identifier
Lichen-covered metamorphic rock, likely gneiss (Quartz–feldspar–mica gneiss (identification tentative from the surface image)) — metamorphic
metamorphic

Lichen-covered metamorphic rock, likely gneiss

Quartz–feldspar–mica gneiss (identification tentative from the surface image)

AI-generated identification · may be incorrect

Gray, coarse-grained, with pale quartz/feldspar patches and possible wavy mineral banding; hardness about 6–7 Mohs, vitreous quartz and cleavage-bearing feldspar. The surface is heavily obscured by lichens, so composition and texture are uncertain.

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Physical properties

Gray, coarse-grained, with pale quartz/feldspar patches and possible wavy mineral banding; hardness about 6–7 Mohs, vitreous quartz and cleavage-bearing feldspar. The surface is heavily obscured by lichens, so composition and texture are uncertain.

Formation & geological history

Gneiss forms when pre-existing rocks are recrystallized and compositionally segregated under high heat and pressure during regional metamorphism; its age depends on the locality and cannot be determined from the image.

Uses & applications

Gneiss is used as dimension stone, paving and landscaping aggregate, and occasionally as decorative building stone.

Geological facts

The pale circular patches may be mineral-rich domains or weathered features; the lichens are biological growth, not part of the rock.

Field identification & locations

Look for persistent alternating light and dark mineral bands on a fresh surface and test hardness with a steel tool; lichens make this view inconclusive. Gneiss occurs widely in ancient continental basement and mountain belts.