mineral
Pink Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectMohs hardness of 7, pale pink to rose color, vitreous luster, hexagonal crystal system, and conchoidal fracture.
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Physical properties
Mohs hardness of 7, pale pink to rose color, vitreous luster, hexagonal crystal system, and conchoidal fracture.
Formation & geological history
Formed in pegmatites and hydrothermal veins through the crystallization of silica-rich solutions.
Uses & applications
Used primarily in ornamental carvings, gemstone jewelry, and metaphysical collections.
Geological facts
The pink coloration is typically caused by trace amounts of titanium, iron, or manganese within the silica matrix.
Field identification & locations
Identified by its distinct pink hue, lack of cleavage, and hard glassy crystals; commonly sourced from Brazil, Madagascar, and the USA.
