Rock Identifier
Granite (Phaneritic Igneous Rock (primarily Quartz, Feldspar, and Mica)) — igneous
igneous

Granite

Phaneritic Igneous Rock (primarily Quartz, Feldspar, and Mica)

Hardness: 6-7 (Mohs scale); Color: White, gray, and pink with dark flecks; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained); Cleavage: Imperfect; Specific gravity: 2.63-2.75

Hardness
6-7 (Mohs scale)
Color
White, gray, and pink with dark flecks
Luster
Vitreous to dull
Identified More igneous

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Physical properties

Hardness: 6-7 (Mohs scale); Color: White, gray, and pink with dark flecks; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained); Cleavage: Imperfect; Specific gravity: 2.63-2.75

Formation & geological history

Formed from the slow subterranean cooling and crystallization of magma. Common in continental crust and mountain ranges, dating from the Archean Eon to the Cenozoic Era.

Uses & applications

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

Geological facts

Granite is the most common igneous rock found on Earth's continents. It earns its name from the Latin word 'granum', meaning a grain, in reference to its coarse-grained structure.

Field identification & locations

Identify by its interlocking 'salt and pepper' crystalline texture and extreme hardness (it will scratch glass). Found in mountain cores and batholiths worldwide.