Rock Identifier
Granite (Granite (Felsic Plutonic Rock)) — igneous
igneous

Granite

Granite (Felsic Plutonic Rock)

Hardness: 6-7 (Mohs scale); Color: Mottled grey, white, and black with visible crystals; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained); Cleavage: Indistinct; Specific gravity: 2.63-2.75.

Hardness
6-7 (Mohs scale)
Color
Mottled grey, white, and black with visible crystals
Luster
Vitreous to dull
Identified More igneous

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Physical properties

Hardness: 6-7 (Mohs scale); Color: Mottled grey, white, and black with visible crystals; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained); Cleavage: Indistinct; Specific gravity: 2.63-2.75.

Formation & geological history

Formed through the slow crystallization of magma below Earth's surface. It is a plutonic rock that cools over thousands to millions of years, allowing large mineral crystals to grow. Found in continental crust ranging from Precambrian to Cenozoic ages.

Uses & applications

Primary use in construction as dimension stone (countertops, flooring, monuments), aggregate for road base, and decorative landscaping. It is also a popular specimen for educational geology kits.

Geological facts

Granite is the most common rock in Earth's continental crust and is what makes up the core of many major mountain ranges. The famous El Capitan in Yosemite National Park is a massive monolith of granite.

Field identification & locations

Identify in the field by its speckled, 'salt and pepper' appearance and visible interlocking crystals of quartz, feldspar, and mica. Commonly found in mountainous regions or areas with exposed batholiths. It will not scratch with a copper penny but will scratch glass.