Rock Identifier
Granite (Felsic intrusive igneous rock) — igneous
igneous

Granite

Felsic intrusive igneous rock

Hardness: 6-7 Mohs; Color: Pink, white, and gray speckled; Luster: Dull to vitreous; Crystal structure: Phaneritic (coarse-grained) containing quartz, feldspar, and mica; Specific gravity: 2.63-2.75

Hardness
6-7 Mohs
Color
Pink, white, and gray speckled
Luster
Dull to vitreous
Identified More igneous
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Physical properties

Hardness: 6-7 Mohs; Color: Pink, white, and gray speckled; Luster: Dull to vitreous; Crystal structure: Phaneritic (coarse-grained) containing quartz, feldspar, and mica; Specific gravity: 2.63-2.75

Formation & geological history

Formed from the slow crystallization of magma below Earth's surface. These plutonic rocks can range in age from the Precambrian to recent periods, typically found in continental crust and mountain belts.

Uses & applications

Extensively used in construction for countertops, floor tiles, paving stone, monuments, and as crushed stone for road base. Popular in the lapidary arts for decorative spheres and bookends.

Geological facts

Granite is the most common rock found on Earth's continental crust. It is incredibly durable and because of its density it can withstand significant weathering over thousands of years.

Field identification & locations

Identify by its crystalline texture where individual minerals (pink feldspar, clear quartz, dark mica) are visible to the naked eye. Commonly found in mountain ranges and glacial deposits.