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; Color: Salt-and-pepper (white, gray, black); Luster: Dull to vitreous; Structure: Phaneritic (coarse-grained visible crystals); Cleavage: Distinct in feldspar grains; Specific gravity: 2.63-2.75.

Hardness
6-7 Mohs
Color
Salt-and-pepper (white, gray, black)
Luster
Dull to vitreous
Identified More igneous

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Physical properties

Hardness: 6-7 Mohs; Color: Salt-and-pepper (white, gray, black); Luster: Dull to vitreous; Structure: Phaneritic (coarse-grained visible crystals); Cleavage: Distinct in feldspar grains; Specific gravity: 2.63-2.75.

Formation & geological history

Formed from the slow cooling and crystallization of felsic magma deep beneath the Earth's surface (plutonic). Found in continental crust, often appearing in mountain roots or batholiths formed millions of years ago.

Uses & applications

Extensively used in construction for countertops, flooring, monuments, and as crushed stone for road base and railway ballast due to its durability.

Geological facts

Granite makes up the majority of the Earth's continental crust. Mount Rushmore is carved into a massive outcropping of granite. It is one of the hardest and most durable common stones on Earth.

Field identification & locations

Identify by its 'salt and pepper' look with interlocking visible crystals of white/gray quartz and pink or white feldspar. Found globally in mountainous regions and areas of exposed bedrock.