Rock Identifier
Granite (Phaneritic Plutonic Igneous Rock (composed of Quartz, Alkali Feldspar, and Plagioclase)) — igneous
igneous

Granite

Phaneritic Plutonic Igneous Rock (composed of Quartz, Alkali Feldspar, and Plagioclase)

Hardness: 6-7 Mohs; Color: Pink/Orange (orthoclase), white/gray (quartz), and black (biotite/hornblende); Luster: Vitreous to pearly; Structure: Phaneritic (coarse-grained) crystalline; Cleavage: None in the rock itself, though individual feldspar grains show cleavage.

Hardness
6-7 Mohs
Luster
Vitreous to pearly
Identified More igneous

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Physical properties

Hardness: 6-7 Mohs; Color: Pink/Orange (orthoclase), white/gray (quartz), and black (biotite/hornblende); Luster: Vitreous to pearly; Structure: Phaneritic (coarse-grained) crystalline; Cleavage: None in the rock itself, though individual feldspar grains show cleavage.

Formation & geological history

Formed through the slow crystallization of magma below Earth's surface (intrusive). It is typically associated with continental crust and mountain-building events. Geological age can range from Archean to Cenozoic.

Uses & applications

Used extensively in construction for countertops, floor tiles, paving stones, and monuments due to its durability and aesthetic appeal. Also used as crushed stone for road base.

Geological facts

Granite makes up a large portion of the Earth's continental crust. Mount Rushmore is carved into a granite batholith. It is one of the hardest and most durable common stones, making it resistant to weathering.

Field identification & locations

Identify in the field by its 'salt and pepper' or mottled appearance with visible, interlocking crystals of different colors. It is found in large plutons or mountain ranges globally, such as the Sierra Nevada or the Scottish Highlands.