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

Pink Granite

Phaneritic Plutonic Felsic Igneous Rock (Granite)

Hardness: 6–7 Mohs; Color: Pink, salmon, or reddish due to high potassium feldspar content, mixed with gray quartz and black biotite/hornblende; Luster: Dull to vitreous; Structure: Phaneritic (coarse-grained, visible crystals);…

Hardness
6–7 Mohs
Luster
Dull to vitreous
Identified More igneous

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Physical properties

Hardness: 6–7 Mohs; Color: Pink, salmon, or reddish due to high potassium feldspar content, mixed with gray quartz and black biotite/hornblende; Luster: Dull to vitreous; Structure: Phaneritic (coarse-grained, visible crystals); Cleavage: Individual mineral grains show cleavage (feldspar) or conchoidal fracture (quartz).

Formation & geological history

Formed through the slow cooling and crystallization of molten magma deep within the Earth's crust (plutonic). This process allows large crystals to grow. Granite can date from the Archean Eon to the Cenozoic, commonly found in continental crustal shields and mountain ranges.

Uses & applications

Extensively used in construction for countertops, floor tiles, and paving stones. It is also used in monument carving, as crushed stone for road base, and as decorative landscaping rock.

Geological facts

Granite is the most common igneous rock found on Earth's continents. The 'pink' color specifically indicates a high concentration of orthoclase feldspar. Mount Rushmore is carved into a massive granite batholith.

Field identification & locations

Identify in the field by its 'salt and pepper' or 'speckled' appearance and coarse mineral grains that are interlocked. Common in mountainous regions like the Appalachians, Rockies, or the Scottish Highlands. Look for the absence of layering (unlike sedimentary rocks) and high resistance to scratching.