
igneous
Granite or granitic rock fragment
Coarse-grained felsic intrusive rock, chiefly quartz, feldspar, and mica/amphibole
AI-generated identification · may be incorrectGray-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.
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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.