Rock Identifier
Granite (Granite (comprised primarily of Quartz (SiO2), Feldspar (KAlSi3O8), and Mica (KAl2(AlSi3O10)(OH)2))) — igneous
igneous

Granite

Granite (comprised primarily of Quartz (SiO2), Feldspar (KAlSi3O8), and Mica (KAl2(AlSi3O10)(OH)2))

Hardness: 6-7 Mohs; Color: Salt and pepper appearance with white/grey quartz and pink/cream feldspar; Luster: Vitreous to pearly; Crystal structure: Phaneritic (coarse-grained); Specific gravity: 2.63 to 2.75

Hardness
6-7 Mohs
Luster
Vitreous to pearly
Identified More igneous

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Physical properties

Hardness: 6-7 Mohs; Color: Salt and pepper appearance with white/grey quartz and pink/cream feldspar; Luster: Vitreous to pearly; Crystal structure: Phaneritic (coarse-grained); Specific gravity: 2.63 to 2.75

Formation & geological history

Formed through the slow crystallization of magma below the Earth's surface (plutonic). Found in continental crust within mountain ranges and batholiths, often dating back hundreds of millions to billions of years.

Uses & applications

Dominantly used in construction for countertops, floor tiles, paving stones, curbing, and monuments. Highly valued for its durability and aesthetic appeal.

Geological facts

Granite makes up a large portion of the Earth's continental crust. El Capitan in Yosemite National Park is one of the most famous massive granite monoliths in the world.

Field identification & locations

Identify in the field by its visible, interlocking crystals of quartz and feldspar. Found globally in mountainous regions. Collectors look for unique phenocrysts (large crystals) or unusual mineral inclusions.