Rock Identifier
Granite (Granite (Felsic Plutonic Rock)) — igneous
igneous

Granite

Granite (Felsic Plutonic Rock)

Hardness: 6-7 on Mohs scale; Color: Gray, salt-and-pepper (white k-feldspar, gray quartz, black biotite/hornblende); Luster: Vitreous to dull; Crystal structure: Phaneritic (coarsegrained) granular; Cleavage: None (grains fracture)

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

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Physical properties

Hardness: 6-7 on Mohs scale; Color: Gray, salt-and-pepper (white k-feldspar, gray quartz, black biotite/hornblende); Luster: Vitreous to dull; Crystal structure: Phaneritic (coarsegrained) granular; Cleavage: None (grains fracture)

Formation & geological history

Formed from the slow crystallization of magma below Earth's surface (intrusive). They belong to many geological ages, from the Archean to the Cenozoic, typically in continental crust mountain belts.

Uses & applications

Extensively used in construction for countertops, floor tiles, paving stones, curbing, monuments, and as crushed stone or aggregate for road building.

Geological facts

Granite is the most common igneous rock found on Earth's continental crust. El Capitan in Yosemite National Park is one of the world's most famous giant granite monoliths.

Field identification & locations

Identify by its interlocking 'salt and pepper' crystalline texture where minerals are large enough to see with the naked eye. Found in continental volcanic arcs and mountain roots. Common in various regions globally.