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

Pink Granite

Phaneritic Plutonic Felsic Rock (Granite)

Hardness: 6-7 Mohs; Color: Pink, orange, red with grey/white and black specks; Luster: Vitreous to dull; Crystal structure: Phaneritic (large, visible grains); Cleavage: Perfect on feldspar grains; Specific gravity: 2.63-2.75

Hardness
6-7 Mohs
Color
Pink, orange, red with grey/white and black specks
Luster
Vitreous to dull
Identified More igneous

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Physical properties

Hardness: 6-7 Mohs; Color: Pink, orange, red with grey/white and black specks; Luster: Vitreous to dull; Crystal structure: Phaneritic (large, visible grains); Cleavage: Perfect on feldspar grains; Specific gravity: 2.63-2.75

Formation & geological history

Formed from the slow cooling and crystallization of magma deep underground (intrusive). Predominantly composed of orthoclase feldspar, quartz, and mica/amphibole. Found in continental crust across all geological ages, often in batholiths.

Uses & applications

Extensively used in construction for countertops, flooring, monuments, and curbing. Used as crushed stone for road base and aggregate. Highly valued as an ornamental stone in architecture.

Geological facts

The pink color is specifically due to a high concentration of potassium-rich orthoclase feldspar. Mount Rushmore is carved into a granite batholith. It is one of the oldest and most abundant rocks on Earth's continental crust.

Field identification & locations

Identify by its interlocking 'salt and pepper' crystalline texture and pinkish orthoclase content. Found in mountainous or shield regions like the Scottish Highlands, the Rockies, or the Canadian Shield. Unlike sandstone, it won't crumble between fingers.