mineral
Rose quartz
Quartz (SiO₂), pink variety
AI-generated identification · may be incorrectTypically translucent to opaque pink, with a vitreous luster and massive, non-crystalline habit; Mohs hardness 7, no cleavage, conchoidal fracture, and specific gravity about 2.65. The image appears to show a rough, polished-like pink quartz specimen.
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Physical properties
Typically translucent to opaque pink, with a vitreous luster and massive, non-crystalline habit; Mohs hardness 7, no cleavage, conchoidal fracture, and specific gravity about 2.65. The image appears to show a rough, polished-like pink quartz specimen.
Formation & geological history
Color generally comes from trace iron, titanium, manganese, or microscopic inclusions. It forms mainly in granitic pegmatites and hydrothermal veins, commonly during Precambrian to younger continental-crust events.
Uses & applications
Used for ornamental carvings, beads, cabochons, decorative stone, and inexpensive metaphysical specimens; transparent faceted material is uncommon. It has little industrial value compared with ordinary quartz.
Geological facts
Rose quartz usually lacks well-formed crystal faces; rare transparent pink crystals are called crystalline rose quartz. The note “Po” is too ambiguous to add reliable geological context.
Field identification & locations
Identify it by its uniform pink color, hardness sufficient to scratch glass, lack of cleavage, and quartz-like conchoidal fracture. Common sources include Brazil, Madagascar, India, South Africa, and the United States.
