Rock Identifier
Granite (Phaneritic Felsic Igneous Rock (composed primarily of Quartz and Alkali Feldspar)) — igneous
igneous

Granite

Phaneritic Felsic Igneous Rock (composed primarily of Quartz and Alkali Feldspar)

Hardness: 6-7 (Mohs scale); Color: Pinkish-red due to K-feldspar, with white, gray, and black speckles; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained visible crystals); Specific gravity: 2.63-2.75

Hardness
6-7 (Mohs scale)
Luster
Vitreous to dull
Identified More igneous

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Physical properties

Hardness: 6-7 (Mohs scale); Color: Pinkish-red due to K-feldspar, with white, gray, and black speckles; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained visible crystals); Specific gravity: 2.63-2.75

Formation & geological history

Formed from the slow crystallization of magma below Earth's surface (intrusive). Most granite is associated with continental crust formation across various geological eons, often found in mountain belts.

Uses & applications

Commonly used in construction for countertops, floor tiles, paving stones, and monuments. Also used as crushed stone/aggregate for road base and railroad ballast.

Geological facts

Granite makes up the majority of Earth's continental crust. El Capitan in Yosemite National Park is one of the most famous granite monoliths in the world.

Field identification & locations

Identify in the field by its 'salt and pepper' look and interlocked visible crystals. It is extremely hard and cannot be scratched by a steel knife. Found in plutons, batholiths, and exposed mountain ranges.