mineral
Pink Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness of 7 on the Mohs scale, pink to rose coloration, vitreous luster, hexagonal crystal system, and conchoidal fracture.
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Physical properties
Hardness of 7 on the Mohs scale, pink to rose coloration, vitreous luster, hexagonal crystal system, and conchoidal fracture.
Formation & geological history
Formed in pegmatites and hydrothermal veins through the crystallization of silica-rich solutions under high pressure and temperature.
Uses & applications
Widely used in ornamental carvings, gemstone jewelry, and metaphysical practices.
Geological facts
The pink coloration is typically caused by microscopic trace amounts of titanium, iron, or manganese embedded within the quartz structure.
Field identification & locations
Identified by its distinctive pink hue, lack of cleavage, and ability to scratch glass easily; commonly found in worldwide pegmatite deposits.
