Granite
Phaneritic intrusive igneous rock (composition: Quartz, Alkali Feldspar, Plagioclase Feldspar)
Rock Type: igneous

Physical Properties
Hardness: 6-7 (Mohs scale); Color: Mottled pink/red, white, and gray; Luster: Vitreous to dull; Crystal structure: Phaneritic (visible interlocking crystals); Cleavage: Indistinct; Specific Gravity: 2.63 - 2.75
Formation & Geological History
Formed from the slow crystallization of magma below Earth's surface. This specimen shows a high concentration of potassium feldspar (orthoclase), giving it the reddish-pink hue. Ages vary globally from Precambrian to Cenozoic.
Uses & Applications
Used extensively in construction for countertops, floor tiles, paving stones, and veneers; also used for monuments, sculptures, and as aggregate for roads.
Geological Facts
Granite makes up a large portion of the Earth's continental crust. Its name comes from the Latin 'granum', meaning a grain, in reference to its coarse-grained structure. It is the signature rock of the continental plates.
Field Identification & Locations
Identify in the field by its hard, scratch-resistant surface and visible, randomly oriented crystals of quartz (clear/gray) and feldspar (pink/white). Common in mountain ranges and glacial deposits.
Identified on: 4/25/2026
Mode: Standard