Rock Identifier
Likely granitic rock fragment (Granite or granodiorite; quartz–feldspar–mica aggregate) — igneous
igneous

Likely granitic rock fragment

Granite or granodiorite; quartz–feldspar–mica aggregate

AI-generated identification · may be incorrect

Coarse-grained, speckled gray-and-white appearance with dark biotite or hornblende; typically Mohs 6–7, vitreous to dull luster, interlocking crystals, and no cleavage as a whole rock. Exact identification is limited by the image’s blur and small specimen size.

Identified More igneous
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Physical properties

Coarse-grained, speckled gray-and-white appearance with dark biotite or hornblende; typically Mohs 6–7, vitreous to dull luster, interlocking crystals, and no cleavage as a whole rock. Exact identification is limited by the image’s blur and small specimen size.

Formation & geological history

Intrusive igneous rock formed when silica-rich magma cooled slowly underground, producing visible crystals; commonly Paleozoic to Precambrian in exposed continental crust, though age depends on locality.

Uses & applications

Widely used as dimension stone, countertops, monuments, aggregate, and decorative landscaping rock; ordinary hand specimens generally have little market value.

Geological facts

Granite is defined by abundant quartz and alkali feldspar, while granodiorite contains more plagioclase; the dark minerals commonly represent biotite or amphibole.

Field identification & locations

Look for interlocking white/pink feldspar, translucent gray quartz, and black mica or amphibole in a granular texture; common in continental mountain belts, road cuts, and glacial deposits. A streak, acid, and hardness test can help distinguish it from weathered basalt or artificial aggregate.