Rock Identifier
Granite (Phaneritic intrusive igneous rock (composition: Quartz, Feldspar, Mica)) — igneous
igneous

Granite

Phaneritic intrusive igneous rock (composition: Quartz, Feldspar, Mica)

Hardness: 6-7 Mohs; Color: Mottled white, pink, grey, and black; Luster: Dull to pearly; Structure: Phaneritic (large, visible crystals); Cleavage: Predominantly feldspar cleavage planes; Specific Gravity: 2.63 to 2.75

Hardness
6-7 Mohs
Color
Mottled white, pink, grey, and black
Luster
Dull to pearly
Identified More igneous

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Physical properties

Hardness: 6-7 Mohs; Color: Mottled white, pink, grey, and black; Luster: Dull to pearly; Structure: Phaneritic (large, visible crystals); Cleavage: Predominantly feldspar cleavage planes; Specific Gravity: 2.63 to 2.75

Formation & geological history

Formed by the slow cooling of silica-rich magma deep underground (plutonic). Most terrestrial granite formed during the Precambrian and Paleozoic eras in continental crust environments.

Uses & applications

Extensively used in construction for countertops, floor tiles, paving stones, curbing, and monuments due to its durability and aesthetic appeal.

Geological facts

Granite makes up the majority of the Earth's continental crust. Mount Rushmore is carved into a massive granite batholith in South Dakota.

Field identification & locations

Identified by its speckled 'salt and pepper' appearance and hardness. It is commonly found in mountain ranges and ancient shield areas like the Canadian Shield. Collectors look for large crystals or unique color variations.