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

Granite

Phaneritic Plutonic Felsic Rock (SiO2, KAlSi3O8, NaAlSi3O8)

Hardness: 6-7 Mohs; Color: Mottled grey, white, and black; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse crystals visible to eye); Specific Gravity: 2.63-2.75

Hardness
6-7 Mohs
Color
Mottled grey, white, and black
Luster
Vitreous to dull
Identified More igneous
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Physical properties

Hardness: 6-7 Mohs; Color: Mottled grey, white, and black; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse crystals visible to eye); Specific Gravity: 2.63-2.75

Formation & geological history

Formed from the slow crystallization of magma below Earth's surface. Primarily composed of quartz, feldspar, and mica. Formation ages can range from billions of years (cratons) to relatively young geological periods.

Uses & applications

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

Geological facts

Granite makes up a large part of the Earth's continental crust. Mount Rushmore is carved into a granite batholith. It is one of the hardest and most durable common stones, resistant to weathering.

Field identification & locations

Identify by its 'salt and pepper' appearance and visible interlocking mineral grains. Commonly found in mountainous regions or where ancient continental crust is exposed. Look for the presence of translucent quartz and shiny mica flakes.