Rock Identifier
Granite (Granite (composed primarily of Quartz, Alkali Feldspar, and Plagioclase)) — igneous
igneous

Granite

Granite (composed primarily of Quartz, Alkali Feldspar, and Plagioclase)

AI-generated identification · may be incorrect

Phaneritic (coarsegrained) texture; Mohs hardness of 6-7; colors range from pink/orange to grey/white with black flecks; vitreous to dull luster; non-cleavable overall as a rock but individual minerals show cleavage.

Identified More igneous
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Physical properties

Phaneritic (coarsegrained) texture; Mohs hardness of 6-7; colors range from pink/orange to grey/white with black flecks; vitreous to dull luster; non-cleavable overall as a rock but individual minerals show cleavage.

Formation & geological history

Formed from the slow crystalline cooling of silica-rich magma deep underground (plutonic) over millions of years. This specific specimen is a water-worn river pebble or glacial cobble.

Uses & applications

Commonly used in construction for countertops, floor tiles, and monuments; as gravel in road building; and as decorative river stone in landscaping.

Geological facts

Granite makes up a large portion of the Earth's continental crust. Mount Rushmore is carved into a granite batholith. The pink color in this specimen comes from potassium-rich orthoclase feldspar.

Field identification & locations

Identify in the field by its 'salt and pepper' appearance and visible interlocking crystals of varied colors. It is found globally in mountainous regions and glacial deposits.