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

Granite

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

AI-generated identification · may be incorrect

Hardness about 6–7 Mohs; light gray with black and whitish grains, granular texture, and vitreous-to-dull luster. Crystals are interlocking and show no prominent cleavage as a whole, though feldspar and mica do.

Identified More igneous
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Physical properties

Hardness about 6–7 Mohs; light gray with black and whitish grains, granular texture, and vitreous-to-dull luster. Crystals are interlocking and show no prominent cleavage as a whole, though feldspar and mica do.

Formation & geological history

Forms when silica-rich magma cools slowly deep underground, producing visible crystals; most examples formed during Precambrian to Phanerozoic mountain-building events.

Uses & applications

Widely used for countertops, monuments, building stone, paving, and aggregate; attractive polished pieces are collected but usually have modest value.

Geological facts

The specimen’s visible quartz-like gray grains, pale feldspar, and dark mafic minerals are characteristic of granite, though granodiorite is also possible from a photograph.

Field identification & locations

Identify it by its coarse interlocking grains, hardness, and lack of layering or foliation; common worldwide in continental crust, especially mountain belts and ancient shields.