Rock Identifier
Granite (Plutonic Igneous Rock (composed primarily of Quartz, Feldspar, and Mica)) — igneous
igneous

Granite

Plutonic Igneous Rock (composed primarily of Quartz, Feldspar, and Mica)

Hardness: 6-7 on Mohs scale; Color: Mottled gray, white, and tan; Luster: Vitreous to dull; Crystal Structure: Phaneritic (coarse-grained) crystalline; Cleavage: None (fractures irregularly); Specific Gravity: 2.63-2.75

Hardness
6-7 on Mohs scale
Color
Mottled gray, white, and tan
Luster
Vitreous to dull
Identified More igneous

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Physical properties

Hardness: 6-7 on Mohs scale; Color: Mottled gray, white, and tan; Luster: Vitreous to dull; Crystal Structure: Phaneritic (coarse-grained) crystalline; Cleavage: None (fractures irregularly); Specific Gravity: 2.63-2.75

Formation & geological history

Formed from the slow crystallization of magma below Earth's surface. High in silica and alkali metals, these intrusive rocks cool over thousands of years to create large visible crystals. Found throughout Earth's crust across all geological ages.

Uses & applications

Extensively used in construction for countertops, floor tiles, paving stones, and memorial monuments. Industrial uses include use as an aggregate in concrete and railroad ballast.

Geological facts

Granite makes up a large part of the continental crust. Half Dome in Yosemite National Park is one of the world's most famous granite monoliths. It is one of the hardest and most durable rocks common on the surface.

Field identification & locations

Identify by its 'salt and pepper' appearance and visible interlocking crystals. It is ubiquitous in mountainous regions and areas with exposed bedrock. Collectors look for unique mineral inclusions like tourmaline or garnets.