Rock Identifier
Granite (Phaneritic Igneous Rock (composed mostly of Quartz, Feldspar, and Mica)) — igneous
igneous

Granite

Phaneritic Igneous Rock (composed mostly of Quartz, Feldspar, and Mica)

Hardness: 6-7 on Mohs scale; Color: Pink, white, gray, and black mottled; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarsegrained/visible crystals); Specific Gravity: 2.65-2.75

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

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Physical properties

Hardness: 6-7 on Mohs scale; Color: Pink, white, gray, and black mottled; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarsegrained/visible crystals); Specific Gravity: 2.65-2.75

Formation & geological history

Formed from the slow subterranean cooling of silica-rich magma (plutonic). Found in continental crust, often dating back hundreds of millions or billions of years.

Uses & applications

Widely used in construction, countertops, monuments, curbing, and as crushed stone for road bases.

Geological facts

Granite makes up a large part of the Earth's continental crust. Mount Rushmore is carved into a massive granite batholith.

Field identification & locations

Identify by its interlocking 'salt and pepper' appearance of different colored minerals; it is extremely hard and cannot be scratched by a steel nail. Common in mountainous regions or glacial deposits.