Rock Identifier
Granite (Granite (Mainly Quartz SiO2, K-Feldspar KAlSi3O8, and Plagioclase)) — igneous
igneous

Granite

Granite (Mainly Quartz SiO2, K-Feldspar KAlSi3O8, and Plagioclase)

Hardness: 6-7 (Mohs scale); Color: Mottled pink, white, and black; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained, visible interlocking crystals); Cleavage: Indistinct on rock, perfect on individual feldspar grains; Specific gravity: 2.63 - 2.75.

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

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Physical properties

Hardness: 6-7 (Mohs scale); Color: Mottled pink, white, and black; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained, visible interlocking crystals); Cleavage: Indistinct on rock, perfect on individual feldspar grains; Specific gravity: 2.63 - 2.75.

Formation & geological history

Formed through the slow crystallization of magma below Earth's surface (intrusive). The visible grains indicate a slow cooling process over thousands to millions of years. It is found in continental crust and often dates to various eras, frequently forming the basement rock of continents.

Uses & applications

Extensively used in construction for countertops, floor tiles, paving stones, curbing, and monuments. Also popular as a collector specimen for teaching petrology.

Geological facts

Granite is one of the hardest and oldest rocks on Earth; some samples are nearly 4 billion years old. It makes up a large portion of the continental crust and forms the core of many major mountain ranges like the Himalayas and the Rockies.

Field identification & locations

Identify in the field by its 'salt and pepper' or mottled appearance and the presence of visible mica (shiny flakes), quartz (clear/grey glassy areas), and feldspar (opaque blocky crystals). It is commonly found in mountain outcrops, river beds, and glacial till.