Rock Identifier
Granite (Alkali-feldspar Granite) (Felsic Plutonic Rock (Primary minerals: Quartz SiO2, Orthoclase KAlSi3O8, Plagioclase (Na,Ca)AlSi3O8)) — igneous
igneous

Granite (Alkali-feldspar Granite)

Felsic Plutonic Rock (Primary minerals: Quartz SiO2, Orthoclase KAlSi3O8, Plagioclase (Na,Ca)AlSi3O8)

Hardness: 6-7 Mohs; Color: Pinkish-red, white/clear, and dark grey; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained/visible crystals); Cleavage: None in quartz, perfect in feldspar; Specific gravity: 2.63 - 2.75

Hardness
6-7 Mohs
Color
Pinkish-red, white/clear, and dark grey
Luster
Vitreous to dull
Identified More igneous

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness: 6-7 Mohs; Color: Pinkish-red, white/clear, and dark grey; Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained/visible crystals); Cleavage: None in quartz, perfect in feldspar; Specific gravity: 2.63 - 2.75

Formation & geological history

Formed through the slow cooling and crystallization of silica-rich magma deep within the Earth's crust (plutonic). Found in continental tectonic plates; often Proterozoic or Paleozoic in age for surface exposures.

Uses & applications

Used extensively in construction for countertops, floor tiles, and gravel. It is also a popular material for monuments, sculptures, and as a decorative landscaping stone.

Geological facts

Granite makes up the majority of Earth's continental crust. Mount Rushmore is carved into a giant granite formation in the Black Hills. Pink hues are specifically caused by high concentrations of potassium feldspar (orthoclase).

Field identification & locations

Identify in the field by looking for a 'salt and pepper' or interlocking crystalline texture where common minerals like quartz and feldspar are visible to the naked eye. Found in mountain ranges and glacial deposits worldwide.