Rock Identifier
Likely granite or granitic gneiss (Granite: quartz + feldspar + mica; possibly foliated into gneiss) — igneous
igneous

Likely granite or granitic gneiss

Granite: quartz + feldspar + mica; possibly foliated into gneiss

AI-generated identification · may be incorrect

Light gray, coarse-grained, with visible pale feldspar/quartz and darker biotite; vitreous quartz and blocky feldspar, generally Mohs 6–7, no strong cleavage in the whole rock, specific gravity about 2.6–2.8.

Identified More igneous
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Physical properties

Light gray, coarse-grained, with visible pale feldspar/quartz and darker biotite; vitreous quartz and blocky feldspar, generally Mohs 6–7, no strong cleavage in the whole rock, specific gravity about 2.6–2.8.

Formation & geological history

Crystallized slowly from silica-rich magma deep in the continental crust, commonly during Precambrian to Phanerozoic mountain-building; if gneissic, later subjected to intense heat and pressure.

Uses & applications

Widely used as dimension stone, countertops, monuments, aggregate, and building stone; ordinary hand specimens have little commercial value.

Geological facts

The image resolution and lighting prevent confident separation of granite from weathered gneiss or another feldspar-rich rock.

Field identification & locations

Look for interlocking crystals, glassy gray quartz, white or pink feldspar, and black mica; granite lacks layering, whereas gneiss shows mineral banding. Common worldwide, especially in continental shields and mountain belts.