Rock Identifier
Granite (Phaneritic plutonic rock (composed of quartz, feldspar, and mica)) — igneous
igneous

Granite

Phaneritic plutonic rock (composed of quartz, feldspar, and mica)

Hardness: 6-7 Mohs; Color: Pinkish-tan with dark specks; Luster: Dull to vitreous; Crystal structure: Phaneritic (coarse-grained); Cleavage: Imperfect; Specific gravity: 2.63-2.75

Hardness
6-7 Mohs
Color
Pinkish-tan with dark specks
Luster
Dull to vitreous
Identified More igneous
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Physical properties

Hardness: 6-7 Mohs; Color: Pinkish-tan with dark specks; Luster: Dull to vitreous; Crystal structure: Phaneritic (coarse-grained); Cleavage: Imperfect; Specific gravity: 2.63-2.75

Formation & geological history

Formed from the slow cooling of silica-rich magma deep underground. This specimen appears to be a weathered or water-worn intrusive igneous rock common in continental crust formations.

Uses & applications

Used extensively in construction for countertops, floor tiles, paving stones, and monument sculpting due to its durability and aesthetic appeal.

Geological facts

Granite is the primary rock of Earth's continental crust. It is one of the hardest natural substances and has been used throughout history by various civilizations, including for the pyramids of Egypt.

Field identification & locations

Identified by its visible interlocking crystals of different colors (pink/white feldspar, clear quartz, and black mica). Found globally in mountain ranges and eroded shields.