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

Granite

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

Hardness: 6-7 on Mohs scale. Color: Mottled buff, pink, white, and gray with dark specks. Luster: Vitreous to dull. Structure: Phaneritic (coarse-grained) crystalline. Cleavage: Indistinct in bulk, but feldspar grains show two planes at 90 degrees.

Hardness
6-7 on Mohs scale
Color
Mottled buff, pink, white, and gray with dark specks
Luster
Vitreous to dull
Identified More igneous

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Physical properties

Hardness: 6-7 on Mohs scale. Color: Mottled buff, pink, white, and gray with dark specks. Luster: Vitreous to dull. Structure: Phaneritic (coarse-grained) crystalline. Cleavage: Indistinct in bulk, but feldspar grains show two planes at 90 degrees.

Formation & geological history

Formed from the slow crystallization of magma below Earth's surface (intrusive). Geological age varies from Archean to Cenozoic depending on the specific batholith; common in continental crust platforms.

Uses & applications

Extensively used in construction for countertops, floor tiles, paving stones, and memorial monuments. Also used as crushed stone (aggregate) for road base and concrete.

Geological facts

Granite makes up the majority of the Earth's continental crust. Mount Rushmore is carved into a massive granite batholith in South Dakota. Because it contains trace amounts of uranium, some granite can emit small amounts of radon gas.

Field identification & locations

Identify in the field by its 'salt and pepper' appearance and visible interlocking crystals of quartz (translucent) and feldspar (opaque/pink/white). Common in mountainous regions and shield areas. It is very resistant to weathering.