Rock Identifier
Pink Granite (Phaneritic Acidic Igneous Rock (Rich in K-feldspar)) — igneous
igneous

Pink Granite

Phaneritic Acidic Igneous Rock (Rich in K-feldspar)

Hardness: 6-7 (Mohs scale); Color: Pink, reddish, grey, and black mottled; Luster: Glassy to dull; Crystal structure: Phaneritic (coarse crystals visible); Specific Gravity: 2.63 - 2.75

Hardness
6-7 (Mohs scale)
Color
Pink, reddish, grey, and black mottled
Luster
Glassy to dull
Identified More igneous

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Physical properties

Hardness: 6-7 (Mohs scale); Color: Pink, reddish, grey, and black mottled; Luster: Glassy to dull; Crystal structure: Phaneritic (coarse crystals visible); Specific Gravity: 2.63 - 2.75

Formation & geological history

Formed from the slow cooling of silica-rich magma deep underground (intrusive). Contains potassium feldspar, quartz, and minor mica/amphibole. Typical age ranges from hundreds of millions to billions of years.

Uses & applications

Widely used in construction, countertops, monuments, flooring, and as crushed stone for road building and landscaping.

Geological facts

Pink granite is the state rock of New Hampshire. The pink color is specifically caused by high concentrations of potassium feldspar (orthoclase).

Field identification & locations

Identify by its interlocking 'salt and pepper' crystalline texture and the dominant pink/salmon hue. Found globally in continental crust/cratons. Common in areas like Scotland, Texas, and Scandinavia.