Rock Identifier
Granite (Granite (Phaneritic Quartz-Feldspar Felsic Rock)) — igneous
igneous

Granite

Granite (Phaneritic Quartz-Feldspar Felsic Rock)

Hardness: 6-7 on Mohs scale; Color: Salt-and-pepper (white, grey, and black); Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained crystals visible to the naked eye); Cleavage: Indistinct in the rock overall, though individual mica/feldspar grains may show it; Specific gravity: 2.65 to 2.75.

Hardness
6-7 on Mohs scale
Color
Salt-and-pepper (white, grey, and black)
Luster
Vitreous to dull
Identified More igneous

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Physical properties

Hardness: 6-7 on Mohs scale; Color: Salt-and-pepper (white, grey, and black); Luster: Vitreous to dull; Crystal structure: Phaneritic (coarse-grained crystals visible to the naked eye); Cleavage: Indistinct in the rock overall, though individual mica/feldspar grains may show it; Specific gravity: 2.65 to 2.75.

Formation & geological history

Formed by the slow crystallization of magma below Earth's surface (intrusive). It is predominantly found in the continental crust and forms in large masses called batholiths. It exists across all geological ages, from the Precambrian to Cenozoic.

Uses & applications

Extensively used in construction for countertops, floor tiles, paving stones, and curbing. It is also used in monuments, bridges, and as crushed stone for road base and railroad ballast. Highly valued in landscaping and architecture for its durability.

Geological facts

Granite makes up a large part of the continental crust. Because it is so hard and durable, it was the preferred building material for the ancient Egyptian pyramids' inner chambers and many of the world's most enduring monuments. It is the signature rock of the continents, as it is rarely found on the ocean floor.

Field identification & locations

Identify in the field by its interlocking coarse crystals and 'speckled' appearance. Look for the presence of translucent quartz, opaque white or pink feldspar, and black specks of mica or hornblende. It is found globally in mountainous regions where deep-seated igneous rocks have been exposed by erosion (e.g., the Sierra Nevada, the Alps, or the Scottish Highlands).