Rock Identifier
Granite (likely) (Granite, a coarse-grained felsic intrusive igneous rock composed mainly of quartz, feldspar, and mica) — igneous
igneous

Granite (likely)

Granite, a coarse-grained felsic intrusive igneous rock composed mainly of quartz, feldspar, and mica

AI-generated identification · may be incorrect

Small, rough, pale cream-and-tan specimen with dark mineral flecks and a granular texture. Granite typically has Mohs hardness 6–7, a vitreous-to-dull luster, interlocking crystals, and no cleavage as a whole rock.

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Physical properties

Small, rough, pale cream-and-tan specimen with dark mineral flecks and a granular texture. Granite typically has Mohs hardness 6–7, a vitreous-to-dull luster, interlocking crystals, and no cleavage as a whole rock.

Formation & geological history

Forms when silica-rich magma cools slowly underground, allowing visible crystals to grow; granites occur in continental crust across a wide range of geological ages.

Uses & applications

Used for building stone, paving, countertops, monuments, and decorative or educational specimens.

Geological facts

Granite’s visible grains are usually quartz and feldspar, with dark biotite or hornblende providing contrast.

Field identification & locations

The light color, speckling, and interlocking grains suggest granite, though the small, partly obscured sample prevents confident identification. Look for hard glassy quartz grains and feldspar; common sources include continental mountain belts and exposed batholiths.