Rock Identifier
Granite (Granite (composed of Quartz, Alkali Feldspar, and Plagioclase)) — igneous
igneous

Granite

Granite (composed of Quartz, Alkali Feldspar, and Plagioclase)

Hardness: 6-7 Mohs; Color: Gray, salt-and-pepper, or white with dark flecks; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained crystalline); Cleavage: None (grains have individual cleavage); Specific gravity: 2.63-2.75

Hardness
6-7 Mohs
Color
Gray, salt-and-pepper, or white with dark flecks
Luster
Vitreous to dull
Identified More igneous

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Physical properties

Hardness: 6-7 Mohs; Color: Gray, salt-and-pepper, or white with dark flecks; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained crystalline); Cleavage: None (grains have individual cleavage); Specific gravity: 2.63-2.75

Formation & geological history

Formed through the slow crystallization of magma below Earth's surface (intrusive). Most continental granite dates from the Precambrian to the Cenozoic eras, typically forming in continental arcs or orogenic belts.

Uses & applications

Widely used in construction for countertops, floor tiles, paving stones, curbing, and monuments due to its durability and resistance to weathering.

Geological facts

Granite makes up much of the Earth's continental crust. Famous landmarks like Mount Rushmore and Yosemite's Half Dome are composed entirely of granite.

Field identification & locations

Identify in the field by its coarse, interlocking crystalline texture where individual minerals (clear quartz, white/pink feldspar, dark mica) are visible to the naked eye. Found globally in mountainous regions and shield areas.