Rock Identifier
Granite (Phaneritic Felsic Igneous Rock (primarily SiO2, Al2O3, K2O, Na2O)) — igneous
igneous

Granite

Phaneritic Felsic Igneous Rock (primarily SiO2, Al2O3, K2O, Na2O)

Hardness: 6-7 on Mohs scale; Color: typically mottled pink, white, gray, and black; Luster: vitreous to dull; Crystal Structure: phaneritic (visible coarse-grained crystals); Cleavage: none (irregular fracture); Specific Gravity: 2.63 to 2.75

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

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Physical properties

Hardness: 6-7 on Mohs scale; Color: typically mottled pink, white, gray, and black; Luster: vitreous to dull; Crystal Structure: phaneritic (visible coarse-grained crystals); Cleavage: none (irregular fracture); Specific Gravity: 2.63 to 2.75

Formation & geological history

Formed through the slow crystallization of magma below Earth's surface (intrusive). Geological age varies widely from Archean to recent, depending on the specific pluton.

Uses & applications

Extensively used in construction for countertops, floor tiles, paving stones, and monuments due to its durability and aesthetic appeal.

Geological facts

Granite makes up a large portion 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 on the planet.

Field identification & locations

Identified in the field by its 'salt and pepper' appearance and interlocking visible crystals of quartz, feldspar, and mica. Found globally in mountainous regions and exposed shields. Collectors look for unique vein patterns or large phenocrysts (porphyritic texture).