Rock Identifier
Granite (Granite (Felsic Plutonic Rock)) — igneous
igneous

Granite

Granite (Felsic Plutonic Rock)

Hardness: 6-7 Mohs; Color: Pink, white, gray, black; Luster: Vitreous to dull; Structure: Phaneritic (coarse-grained); Cleavage: None (individual minerals have cleavage); Specific Gravity: 2.63 - 2.75

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

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Physical properties

Hardness: 6-7 Mohs; Color: Pink, white, gray, black; Luster: Vitreous to dull; Structure: Phaneritic (coarse-grained); Cleavage: None (individual minerals have cleavage); Specific Gravity: 2.63 - 2.75

Formation & geological history

Formed through the slow crystallization of magma below Earth's surface. It is a coarse-grained intrusive rock typically formed in continental crust over millions of years.

Uses & applications

Extensively used in construction for countertops, floor tiles, paving stone, monuments, and as aggregate in road building. Also a popular specimen for educational geology kits.

Geological facts

Granite makes up a large portion of the Earth's continental crust. Mount Rushmore and the base of the Statue of Liberty are both made primarily of granite-related stone.

Field identification & locations

Identify by its interlocking 'salt and pepper' appearance of quartz, feldspar, and mica. It is found in large mountain ranges and shield areas globally. Collectors look for large crystals of feldspar or mica.