Pink Granite
Phaneritic plutonic rock (dominated by Alkali Feldspar)
Rock Type: igneous

Physical Properties
Hardness: 6-7 on Mohs scale; Color: Pink, salmon, or reddish with flecks of white, gray, and black; Luster: Dull to vitreous; Crystal Structure: Phaneritic (coarse-grained); Specific Gravity: 2.63-2.75
Formation & Geological History
Formed by the slow crystallization of magma below Earth's surface. The pink color is primarily due to an abundance of potassium feldspar (orthoclase). These rocks are often found in batholiths or mountain ranges and can be billions of years old.
Uses & Applications
Widely used for construction, countertops, monuments, curbing, and decorative landscaping stone.
Geological Facts
Granite makes up a large portion of the Earth's continental crust. Mount Rushmore is carved into a granite batholith. Its resistance to acid rain and high durability makes it ideal for outdoor memorials.
Field Identification & Locations
Identified in the field by its visible interlocking crystals of pink feldspar, translucent quartz, and dark minerals like mica or hornblende. Commonly found in shield areas and mountainous regions globally.
Identified on: 5/15/2026
Mode: Standard