Rock Identifier
Granite (Coarse-grained felsic intrusive igneous rock; chiefly quartz, alkali feldspar, plagioclase, and biotite/hornblende) — igneous
igneous

Granite

Coarse-grained felsic intrusive igneous rock; chiefly quartz, alkali feldspar, plagioclase, and biotite/hornblende

AI-generated identification · may be incorrect

Typically Mohs 6–7; pinkish-tan, gray, and black speckled appearance, with a granular texture and vitreous quartz plus feldspar luster. Crystals are interlocking and show no preferred cleavage as a whole, though individual minerals may cleave.

Identified More igneous
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Physical properties

Typically Mohs 6–7; pinkish-tan, gray, and black speckled appearance, with a granular texture and vitreous quartz plus feldspar luster. Crystals are interlocking and show no preferred cleavage as a whole, though individual minerals may cleave.

Formation & geological history

Forms when silica-rich magma slowly cools underground, allowing visible crystals to grow; commonly Paleozoic to Precambrian in exposed continental crust, though granite occurs in rocks of many ages.

Uses & applications

Used as dimension stone, countertops, monuments, paving, aggregate, and decorative landscaping material; small attractive pieces are inexpensive collector specimens.

Geological facts

The specimen appears granite or a closely related granitic rock, possibly weathered and slightly rounded; pink coloration commonly reflects potassium feldspar.

Field identification & locations

Identify it by visible interlocking quartz and feldspar grains, pink/gray coloration, and hardness sufficient to scratch glass; common worldwide in mountain belts and continental shields.