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

Granite

Coarse-grained granitic rock, chiefly quartz, alkali feldspar, plagioclase, and biotite/hornblende

AI-generated identification · may be incorrect

Hardness about 6–7 Mohs; mottled white, gray, pink, black, and greenish colors with a granular crystalline texture and vitreous-to-pearly luster. It has interlocking crystals, no regular cleavage as a rock, and specific gravity around 2.6–2.7.

Identified More igneous
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Physical properties

Hardness about 6–7 Mohs; mottled white, gray, pink, black, and greenish colors with a granular crystalline texture and vitreous-to-pearly luster. It has interlocking crystals, no regular cleavage as a rock, and specific gravity around 2.6–2.7.

Formation & geological history

Forms when silica-rich magma cools slowly deep in the continental crust, allowing large crystals to grow; typical ages range from Precambrian to Cenozoic. This rounded specimen is likely weathered or tumbled granite.

Uses & applications

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

Geological facts

Visible quartz is commonly translucent gray, feldspar is white or pink, and dark flakes are biotite or amphibole. Its coarse texture distinguishes it from volcanic rhyolite.

Field identification & locations

Common worldwide, including India, Brazil, the United States, Canada, and Scandinavia. Identify it by interlocking quartz and feldspar crystals and its resistance to scratching; acid produces no reaction.