Rock Identifier
Granite or granitic rock fragment (Coarse-grained felsic intrusive rock, chiefly quartz, feldspar, and mica/amphibole) — igneous
igneous

Granite or granitic rock fragment

Coarse-grained felsic intrusive rock, chiefly quartz, feldspar, and mica/amphibole

AI-generated identification · may be incorrect

Gray-green, mottled, and granular with a dull to weakly vitreous luster; visible interlocking crystals suggest hardness about 6–7 Mohs. Exact mineral proportions and cleavage cannot be confirmed from the image.

Identified More igneous
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Physical properties

Gray-green, mottled, and granular with a dull to weakly vitreous luster; visible interlocking crystals suggest hardness about 6–7 Mohs. Exact mineral proportions and cleavage cannot be confirmed from the image.

Formation & geological history

Likely crystallized slowly from silica-rich magma deep in continental crust, commonly during Precambrian to Phanerozoic mountain-building; the fragment was later weathered or broken from an outcrop.

Uses & applications

Used extensively as crushed aggregate, building stone, countertops, monuments, and decorative material; this small irregular fragment has negligible commercial value.

Geological facts

The dark grains may be biotite, amphibole, or altered minerals, while the pale grains are likely feldspar and quartz. Greenish coloration could indicate epidote or weathering, so it may technically be granodiorite or altered granite.

Field identification & locations

Identify it by its coarse, interlocking crystal texture, lack of layering, and inability to scratch with a steel knife (though individual minerals may differ); common worldwide in continental shields and mountain belts.