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

Pink Granite

Granite (Felsic Plutonic Rock)

Hardness: 6 to 7 on Mohs scale; Color: Mottled pink with white, grey, and black specks; Luster: Phaneritic (crystalline) and somewhat dull when unpolished; Crystal Structure: Granular/Coarse-grained; Specific Gravity: 2.63 - 2.75

Hardness
6 to 7 on Mohs scale
Color
Mottled pink with white, grey, and black specks
Luster
Phaneritic (crystalline) and somewhat dull when unpolished
Identified More igneous

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Physical properties

Hardness: 6 to 7 on Mohs scale; Color: Mottled pink with white, grey, and black specks; Luster: Phaneritic (crystalline) and somewhat dull when unpolished; Crystal Structure: Granular/Coarse-grained; Specific Gravity: 2.63 - 2.75

Formation & geological history

Formed through the slow crystallization of magma below the Earth's surface (intrusive). The pink color is derived from a high potassium feldspar (orthoclase) content. It can be found in continental crust spanning billions of years to more recent tectonic events.

Uses & applications

Used widely in construction for countertops, floor tiles, and gravel. Also used for monuments, sculptures, and as a durable building facade material.

Geological facts

Granite is one of the hardest and most common rocks in the Earth's continental crust. Its name comes from the Latin word 'granum', meaning a grain, in reference to its coarse-grained structure.

Field identification & locations

Identify in the field by its interlocking mineral grains (quartz, feldspar, and mica). It lacks any layering or foliation. Commonly found in mountain ranges and eroded continental shields.