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: Light gray to tan with salt-and-pepper flecks; Luster: Dull to vitreous; Structure: Phaneritic (coarse-grained); Specific Gravity: 2.63 to 2.75.

Hardness
6-7 on Mohs scale
Color
Light gray to tan with salt-and-pepper flecks
Luster
Dull to vitreous
Identified More igneous

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Physical properties

Hardness: 6-7 on Mohs scale; Color: Light gray to tan with salt-and-pepper flecks; Luster: Dull to vitreous; Structure: Phaneritic (coarse-grained); Specific Gravity: 2.63 to 2.75.

Formation & geological history

Formed from the slow crystallization of magma below Earth's surface. It is a plutonic rock found in continental crust, often dating from the Precambrian to Cenozoic eras.

Uses & applications

Used extensively in construction (curbing, pavers), interior design (countertops, floor tiles), and as dimension stone for monuments and public buildings.

Geological facts

Granite makes up a large part of the Earth's continental crust. Mount Rushmore is carved into a granite batholith in the Black Hills of South Dakota.

Field identification & locations

Identify in the field by its interlocking visible crystals of light-colored minerals (quartz/feldspar) and dark minerals (biotite/amphibole). It is found globally in mountain ranges and eroded shield areas.