Rock Identifier
Granite (Phaneritic intrusive igneous rock (Composition: Quartz, Feldspar, Mica)) — igneous
igneous

Granite

Phaneritic intrusive igneous rock (Composition: Quartz, Feldspar, Mica)

Hardness: 6-7 Mohs; Color: Pinkish-tan with black biotite spots; Luster: Dull to vitreous; Structure: Phaneritic (coarse-grained) crystalline; Cleavage: None (fractures)

Hardness
6-7 Mohs
Color
Pinkish-tan with black biotite spots
Luster
Dull to vitreous
Identified More igneous

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Physical properties

Hardness: 6-7 Mohs; Color: Pinkish-tan with black biotite spots; Luster: Dull to vitreous; Structure: Phaneritic (coarse-grained) crystalline; Cleavage: None (fractures)

Formation & geological history

Formed by the slow crystallization of magma below Earth's surface. These specimens are often millions to billions of years old and frequently rounded by river or glacial transport.

Uses & applications

Used extensively in construction (countertops, flooring), monuments, curbing, and as aggregate. Polished specimens are used for decorative purposes.

Geological facts

Granite makes up a large portion of the Earth's continental crust. It is one of the hardest and most durable natural stones, which is why it is used for Egyptian pyramids and modern skyscrapers alike.

Field identification & locations

Identify in the field by its 'salt and pepper' appearance and visible interlocking crystals of quartz and feldspar. Commonly found in mountainous regions or as glacial erratics in riverbeds.