Rock Identifier
Granite (Phaneritic Felsic Igneous Rock (composed primarily of Quartz, Feldspar, and Mica)) — igneous
igneous

Granite

Phaneritic Felsic Igneous Rock (composed primarily of Quartz, Feldspar, and Mica)

Hardness: 6-7 on Mohs scale. Color: Tan, brown, and grey with black specks. Luster: Vitreous to dull. Crystal structure: Phaneritic (coarse-grained visible crystals). Cleavage: Imperfect. Specific Gravity: 2.63-2.75.

Hardness
6-7 on Mohs scale
Color
Tan, brown, and grey with black specks
Luster
Vitreous to dull
Identified More igneous
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Physical properties

Hardness: 6-7 on Mohs scale. Color: Tan, brown, and grey with black specks. Luster: Vitreous to dull. Crystal structure: Phaneritic (coarse-grained visible crystals). Cleavage: Imperfect. Specific Gravity: 2.63-2.75.

Formation & geological history

Formed through the slow crystallization of magma below the Earth's surface (intrusive). The coarse grains indicate it cooled over a long period. Generally associated with continental crust formation across billions of years of geological history.

Uses & applications

Extensively used in construction for countertops, floor tiles, paving stones, curbing, and monuments due to its durability and aesthetic appeal.

Geological facts

Granite is one of the most common rocks on the Earth's surface and makes up a large portion of the continental crust. The word 'granite' comes from the Latin 'granum', meaning a grain, in reference to its coarse-grained structure.

Field identification & locations

Identify in the field by its hard, granular texture and salt-and-pepper appearance. It will not be scratched by a steel knife. Commonly found in plutons and mountain ranges worldwide.