Rock Identifier
Granite (Phaneritic Felsic Igneous Rock) — igneous
igneous

Granite

Phaneritic Felsic Igneous Rock

Hardness: 6-7 (Mohs scale); Color: Salt and pepper (pinkish-brown and black grains); Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained); Cleavage: None (minerals within exhibit cleavage independently); Specific gravity: 2.63 - 2.75

Hardness
6-7 (Mohs scale)
Color
Salt and pepper (pinkish-brown and black grains)
Luster
Vitreous to dull
Identified More igneous

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Physical properties

Hardness: 6-7 (Mohs scale); Color: Salt and pepper (pinkish-brown and black grains); Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained); Cleavage: None (minerals within exhibit cleavage independently); Specific gravity: 2.63 - 2.75

Formation & geological history

Formed through the slow crystallization of magma below the Earth's surface (intrusive). The large grains indicate a long cooling period. It can date back over 4 billion years in the Earth's crust.

Uses & applications

Extensively used in construction for countertops, floor tiles, paving stones, curbing, monuments, and as aggregate for roads.

Geological facts

Granite makes up a large portion of the Earth's continental crust. Famous locations like Yosemite's Half Dome and Mount Rushmore are made entirely of granite.

Field identification & locations

Identify in the field by its visible interlocking crystals of quartz (clear/grey), feldspar (tan/pink), and mica (black/shiny). It is commonly found in mountain ranges and continental shields. Collectors look for unique mineral inclusions like tourmaline or large feldspar crystals.