Rock Identifier
Granite (Intrusive Igneous Rock (composed primarily of Quartz: SiO2, Feldspar: KAlSi3O8, and Mica: KAl2(AlSi3O10)(OH)2)) — igneous
igneous

Granite

Intrusive Igneous Rock (composed primarily of Quartz: SiO2, Feldspar: KAlSi3O8, and Mica: KAl2(AlSi3O10)(OH)2)

Hardness: 6-7 on Mohs scale; Color: Phaneritic (visible grains) pattern with white, grey, pink, and black; Luster: Vitreous to dull; Structure: Granular/crystalline; Cleavage: None (bulk rock), Feldspars show cleavage; Gravity: 2.63 - 2.75

Hardness
6-7 on Mohs scale
Luster
Vitreous to dull
Identified More igneous

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Physical properties

Hardness: 6-7 on Mohs scale; Color: Phaneritic (visible grains) pattern with white, grey, pink, and black; Luster: Vitreous to dull; Structure: Granular/crystalline; Cleavage: None (bulk rock), Feldspars show cleavage; Gravity: 2.63 - 2.75

Formation & geological history

Formed from the slow crystallization of magma below Earth's surface. It is an intrusive rock found in continental crust across all geological ages, especially in Precambrian shields.

Uses & applications

Extensively used in construction for countertops, floor tiles, and monument stone. Also used for curbing and crushed stone in infrastructure projects.

Geological facts

Granite is the most common igneous rock found in Earth's continental crust. Mount Rushmore is carved into a massive granite batholith. It is resistant to acid rain and highly durable.

Field identification & locations

Identify by its 'salt and pepper' appearance and visible interlocking crystals. Common in mountain ranges and glacial erratic deposits. Collectors look for unique color variations or large phenocrysts (Porphyritic granite).