Rock Identifier
Granite (Phaneritic Plutonic Felsic Rock (primarily Quartz (SiO2), Alkali Feldspar, and Plagioclase Feldspar)) — igneous
igneous

Granite

Phaneritic Plutonic Felsic Rock (primarily Quartz (SiO2), Alkali Feldspar, and Plagioclase Feldspar)

Hardness: 6-7 on Mohs scale; Color: Pink, white, gray, and black mottled; Luster: Dull to vitreous; Crystal Structure: Phaneritic (large, visible interlocking crystals); Specific Gravity: 2.63 - 2.75

Hardness
6-7 on Mohs scale
Color
Pink, white, gray, and black mottled
Luster
Dull to vitreous
Identified More igneous

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Physical properties

Hardness: 6-7 on Mohs scale; Color: Pink, white, gray, and black mottled; Luster: Dull to vitreous; Crystal Structure: Phaneritic (large, visible interlocking crystals); Specific Gravity: 2.63 - 2.75

Formation & geological history

Formed through the slow crystallization of magma below Earth's surface (intrusive). This specimen specifically shows a 'pink' granite variety due to high potassium feldspar content. Granite formation occurs across all geological eras, notably during orogenic (mountain-building) events.

Uses & applications

Extensively used in construction for countertops, floor tiles, paving stones, and monuments. Also used as crushed stone for road base and railway ballast.

Geological facts

Granite makes up a large portion of the Earth's continental crust. El Capitan in Yosemite National Park is one of the world's most famous granitic monoliths. It is one of the hardest and most durable common stones available.

Field identification & locations

Identify in the field by its 'salt and pepper' appearance and visible interlocking crystals that are not aligned (unlike gneiss). Found globally in continental mountain ranges and shield areas like the Canadian Shield or the Scottish Highlands.