Rock Identifier
Granite (Phaneritic Felsic Igneous Rock) — igneous
igneous

Granite

Phaneritic Felsic Igneous Rock

Hardness of 6 on the Mohs scale; speckled pink, white, gray, and black color; vitreous to dull luster; phaneritic (coarse-grained) crystal structure; composed primarily of quartz, alkali feldspar, and plagioclase with biotite and amphibole; specific gravity around 2.65 to 2.75.

Identified More igneous
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Physical properties

Hardness of 6 on the Mohs scale; speckled pink, white, gray, and black color; vitreous to dull luster; phaneritic (coarse-grained) crystal structure; composed primarily of quartz, alkali feldspar, and plagioclase with biotite and amphibole; specific gravity around 2.65 to 2.75.

Formation & geological history

Formed from the slow cooling and crystallization of magma rich in silica and alkali metal oxides beneath the Earth's surface over millions of years.

Uses & applications

Widely used in construction for dimension stone, architectural facings, floor tiles, counter tops, and monuments.

Geological facts

Granite is the most common rock of the Earth's continental crust and forms the core of many major mountain ranges.

Field identification & locations

Easily identified by its distinct interlocking, coarse-grained crystals of pink/white feldspar, glassy clear quartz, and dark biotite or hornblende. Found globally in shield areas and mountainous regions.