Rock Identifier
Granite (Granite; chiefly quartz (SiO₂), alkali feldspar and plagioclase, with minor biotite/hornblende) — igneous
igneous

Granite

Granite; chiefly quartz (SiO₂), alkali feldspar and plagioclase, with minor biotite/hornblende

AI-generated identification · may be incorrect

Coarse-grained, gray, speckled texture with vitreous quartz and feldspar; Mohs hardness ~6–7, nonfoliated, massive, with poor cleavage as a whole and specific gravity ~2.63–2.75.

Identified More igneous
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Physical properties

Coarse-grained, gray, speckled texture with vitreous quartz and feldspar; Mohs hardness ~6–7, nonfoliated, massive, with poor cleavage as a whole and specific gravity ~2.63–2.75.

Formation & geological history

A felsic intrusive igneous rock formed by slow cooling and crystallization of silica-rich magma deep in continental crust, commonly during Precambrian to Phanerozoic mountain-building events.

Uses & applications

Widely used for countertops, monuments, floor and building stone, paving, aggregate, and architectural cladding; attractive polished varieties have decorative value.

Geological facts

The visible interlocking crystals indicate slow underground cooling. Gray granite can resemble granodiorite or gneiss; exact identification may require examining mineral proportions and texture.

Field identification & locations

Identify by its granular interlocking quartz–feldspar–mica texture, lack of layering, and inability to scratch with a steel knife. Common worldwide, including India, Brazil, Scandinavia, Canada, and the United States.