Rock Identifier
Granite (Phaneritic Plutonic Felsic Rock (SiO2, KAlSi3O8, NaAlSi3O8, CaAl2Si2O8)) — igneous
igneous

Granite

Phaneritic Plutonic Felsic Rock (SiO2, KAlSi3O8, NaAlSi3O8, CaAl2Si2O8)

Hardness: 6-7 on Mohs scale; Color: Salt and pepper/mottled white, grey, and black; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained visible crystals); Cleavage: Indistinct; Specific gravity: 2.65-2.75.

Hardness
6-7 on Mohs scale
Color
Salt and pepper/mottled white, grey, and black
Luster
Vitreous to dull
Identified More igneous

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Physical properties

Hardness: 6-7 on Mohs scale; Color: Salt and pepper/mottled white, grey, and black; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained visible crystals); Cleavage: Indistinct; Specific gravity: 2.65-2.75.

Formation & geological history

Formed by the slow crystallization of magma below the Earth's surface in continental crust. These intrusive plutons can range from billions of years old to relatively young in geological terms.

Uses & applications

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

Geological facts

Granite makes up a large portion of the Earth's continental crust. Because it is so hard and dense, it can be polished to a mirror finish, a property valued in architecture.

Field identification & locations

Identify in the field by looking for a coarse-grained, interlocking texture of light-colored minerals (quartz/feldspar) and dark minerals (biotite/hornblende). It is found worldwide in mountainous or cratonic regions.