Rock Identifier
Granite (Phaneritic intrusive felsic igneous rock) — igneous
igneous

Granite

Phaneritic intrusive felsic igneous rock

Hardness: 6-7 Mohs; Color: Mottled gray, black, and white; Luster: Vitreous to dull; Crystal structure: Phaneritic (visible crystals of quartz, feldspar, and mica); Specific gravity: 2.63-2.75.

Hardness
6-7 Mohs
Color
Mottled gray, black, and white
Luster
Vitreous to dull
Identified More igneous
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Physical properties

Hardness: 6-7 Mohs; Color: Mottled gray, black, and white; Luster: Vitreous to dull; Crystal structure: Phaneritic (visible crystals of quartz, feldspar, and mica); Specific gravity: 2.63-2.75.

Formation & geological history

Formed by the slow crystallization of silica-rich magma below the Earth's surface. This intrusive process allows for the growth of large, visible mineral grains. Many granites date back to the Precambrian or Paleozoic eras.

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 makes up a large portion of the Earth's continental crust. It is one of the hardest natural stones, making it highly resistant to weathering and erosion.

Field identification & locations

Identified by its 'salt and pepper' appearance and visible interlocking crystals of quartz and feldspar. Commonly found in mountainous regions and areas where ancient continental crust is exposed.