Rock Identifier
Granite (Phaneritic plutonic rock (dominated by Quartz, Feldspar, and Mica)) — igneous
igneous

Granite

Phaneritic plutonic rock (dominated by Quartz, Feldspar, and Mica)

Hardness: 6-7 on Mohs scale. Color: Mottled pink, white, and grey. Luster: Dull to vitreous. Crystal structure: Phaneritic (visible crystals). Cleavage: None (fractures irregularly). Specific gravity: 2.63 to 2.75.

Hardness
6-7 on Mohs scale
Color
Mottled pink, white, and grey
Luster
Dull to vitreous
Identified More igneous

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Physical properties

Hardness: 6-7 on Mohs scale. Color: Mottled pink, white, and grey. Luster: Dull to vitreous. Crystal structure: Phaneritic (visible crystals). Cleavage: None (fractures irregularly). Specific gravity: 2.63 to 2.75.

Formation & geological history

Formed by the slow crystallization of magma below Earth's surface in plutonic environments. Most granite formations date back to the Precambrian or Paleozoic eras.

Uses & applications

Extensively used in construction for countertops, floor tiles, paving stone, curbing, and as a decorative stone in monuments. High value as an industrial building material.

Geological facts

Granite makes up a large portion of the Earth's continental crust. It is one of the hardest and most durable natural stones, which is why it has been used since ancient Egypt for obelisks and pyramids.

Field identification & locations

Identify in the field by its 'salt and pepper' appearance and visible interlocking crystals. Commonly found in mountainous regions or where glacial activity has deposited 'erratics.'