Rock Identifier
Pink Granite (Phaneritic Felsic Igneous Rock) — igneous
igneous

Pink Granite

Phaneritic Felsic Igneous Rock

Hardness: 6-7 Mohs; Color: Mottled pink, black, and white; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained); Specific Gravity: 2.63-2.75

Hardness
6-7 Mohs
Color
Mottled pink, black, and white
Luster
Vitreous to dull
Identified More igneous
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Physical properties

Hardness: 6-7 Mohs; Color: Mottled pink, black, and white; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained); Specific Gravity: 2.63-2.75

Formation & geological history

Formed from the slow cooling and solidification of magma deep within the Earth's crust (plutonic). The pink color comes from potassium feldspar (orthoclase). Found in continental crust across all geological ages.

Uses & applications

Construction (countertops, monuments), architectural stone, aggregate, and small polished specimens for collectors.

Geological facts

Granite is the most common rock found in the Earth's continental crust. Its pink color specifically indicates a high concentration of potassium-rich feldspar compared to grey granites.

Field identification & locations

Identify by its interlocking crystalline texture and hard mineral components that scratch glass. Found commonly in mountainous regions or glacial deposits. Collectors often find these as tumbled river stones.