Rock Identifier
Granite (Phaneritic Felsic Igneous Rock (primarily Quartz, Feldspar, and Mica)) — igneous
igneous

Granite

Phaneritic Felsic Igneous Rock (primarily Quartz, Feldspar, and Mica)

Hardness: 6–7 on Mohs scale; Color: Speckled gray, white, and black; Luster: Vitreous to dull; Crystal structure: Phaneritic (large, visible interlocking grains); Cleavage: Indistinct; Specific gravity: 2.63 - 2.75

Hardness
6–7 on Mohs scale
Color
Speckled gray, white, and black
Luster
Vitreous to dull
Identified More igneous

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness: 6–7 on Mohs scale; Color: Speckled gray, white, and black; Luster: Vitreous to dull; Crystal structure: Phaneritic (large, visible interlocking grains); Cleavage: Indistinct; Specific gravity: 2.63 - 2.75

Formation & geological history

Formed through the slow crystallization of magma below the Earth's surface (intrusive). They are typically found in batholiths and continental crust, with ages ranging from billions of years (Precambrian) to more recent tectonic events.

Uses & applications

Extensively used in construction as dimension stone, floor tiles, kitchen countertops, and as crushed stone for road base or railway ballast.

Geological facts

Granite is the most common rock in the Earth's continental crust. Mount Rushmore is carved into a massive granite batholith in the Black Hills of South Dakota.

Field identification & locations

Identify in the field by its interlocking 'salt and pepper' crystalline texture and extreme hardness (cannot be scratched by a steel blade). Common in mountain ranges and eroded shield areas worldwide.