Rock Identifier
Granite (Phaneritic plutonic rock (Quartz, Feldspar, Mica)) — igneous
igneous

Granite

Phaneritic plutonic rock (Quartz, Feldspar, Mica)

Hardness: 6-7 Mohs; Color: Pink, gray, white, and black mottled; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained); Cleavage: Dependent on mineral constituents; Specific Gravity: 2.63-2.75

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

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Physical properties

Hardness: 6-7 Mohs; Color: Pink, gray, white, and black mottled; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained); Cleavage: Dependent on mineral constituents; Specific Gravity: 2.63-2.75

Formation & geological history

Formed through the slow crystallization of silica-rich magma below the Earth's surface. Found in continental crust, often appearing in mountain roots and cratons dating from the Precambrian to Cenozoic eras.

Uses & applications

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

Geological facts

Granite makes up a large part of the Earth's continental crust. Unlike oceanic crust which is primarily basalt, continents are 'buoyant' because they are made of less dense granitic rocks.

Field identification & locations

Identify by its interlocking 'salt and pepper' appearance of multicolored crystals (pink potassium feldspar, white plagioclase, glassy quartz, and dark biotite or hornblende). Found globally in mountainous regions.