Rock Identifier
Granite (Granite (Mainly Quartz, Alkali Feldspar, and Plagioclase)) — igneous
igneous

Granite

Granite (Mainly Quartz, Alkali Feldspar, and Plagioclase)

Hardness: 6-7 on Mohs scale; Color: Mottled gray, white, and pinkish/reddish; Luster: Dull to vitreous; Structure: Phaneritic (coarse-grained crystalline); Cleavage: Indistinct; Specific Gravity: 2.63 to 2.75

Hardness
6-7 on Mohs scale
Color
Mottled gray, white, and pinkish/reddish
Luster
Dull to vitreous
Identified More igneous

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Physical properties

Hardness: 6-7 on Mohs scale; Color: Mottled gray, white, and pinkish/reddish; Luster: Dull to vitreous; Structure: Phaneritic (coarse-grained crystalline); Cleavage: Indistinct; Specific Gravity: 2.63 to 2.75

Formation & geological history

Formed through the slow crystallization of magma below Earth's surface (intrusive). They can be formed across various geological ages, notably during orogenic (mountain-building) events.

Uses & applications

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

Geological facts

Granite makes up a large portion of the Earth's continental crust. Mount Rushmore is carved into a granite batholith in South Dakota, USA.

Field identification & locations

Identify in the field by its 'salt and pepper' appearance and visible interlocking crystals of quartz and feldspar. It is commonly found in mountain ranges and ancient continental shields.