Rock Identifier
Granite (Granitoid (KAlSi3O8 – NaAlSi3O8 – CaAl2Si2O8 + SiO2)) — igneous
igneous

Granite

Granitoid (KAlSi3O8 – NaAlSi3O8 – CaAl2Si2O8 + SiO2)

Hardness: 6-7 Mohs; Color: Mottled pink, white, gray, and black; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained visible crystals); Cleavage: Poor; Specific Gravity: 2.63 to 2.75

Hardness
6-7 Mohs
Color
Mottled pink, white, gray, and black
Luster
Vitreous to dull
Identified More igneous

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Physical properties

Hardness: 6-7 Mohs; Color: Mottled pink, white, gray, and black; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained visible crystals); Cleavage: Poor; Specific Gravity: 2.63 to 2.75

Formation & geological history

Formed by the slow crystallization of silica-rich magma beneath the Earth's surface (intrusive). They can be found in continental crust dating back billions of years to the Precambrian era.

Uses & applications

Extensively used in construction for countertops, floor tiles, paving stone, curbing, and monuments. Also used as crushed stone for road base and railroad ballast.

Geological facts

Granite is the most common igneous rock found on Earth's continental surface. The famous peaks of Yosemite National Park (like Half Dome) and Mount Rushmore are made entirely of granite.

Field identification & locations

Identify in the field by the 'salt and pepper' appearance of interlocking crystals of quartz (clear/gray), feldspar (pink/white), and mica (black). Commonly found in mountain ranges or Shield areas. Collectors look for unique inclusions or rare pegmatite formations.