Rock Identifier
Granite (Phaneritic plutonic rock (Quartz, Feldspar, Mica)) — igneous
igneous

Granite

Phaneritic plutonic rock (Quartz, Feldspar, Mica)

Hardness: 6-7 on Mohs scale; Color: Grey, white, pink, and black salt-and-pepper look; Luster: Dull to vitreous; Crystal structure: Phaneritic (coarse-grained); Cleavage: Indistinct; Specific Gravity: 2.63–2.75

Hardness
6-7 on Mohs scale
Color
Grey, white, pink, and black salt-and-pepper look
Luster
Dull to vitreous
Identified More igneous

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Physical properties

Hardness: 6-7 on Mohs scale; Color: Grey, white, pink, and black salt-and-pepper look; Luster: Dull to vitreous; Crystal structure: Phaneritic (coarse-grained); Cleavage: Indistinct; Specific Gravity: 2.63–2.75

Formation & geological history

Formed through slow crystallization of magma below the Earth's surface (plutonic). Found in continental crust, often in the cores of mountain ranges.

Uses & applications

Used extensively in construction for countertops, floor tiles, curbing, monuments, and as crushed stone for road base.

Geological facts

Granite makes up a large part of the Earth's continental crust. Because it is so hard and durable, it has been used by civilizations for millennia, including the Ancient Egyptians for statues and pyramids.

Field identification & locations

Identify by its interlocking crystalline texture where grains are visible to the naked eye. Look for a mix of clear/white quartz, opaque feldspar, and dark biotite or hornblende grains. Common in mountainous regions and glacial deposits.