
gemstone
Rose quartz bangle
Quartz, silicon dioxide (SiO₂), commonly colored by trace elements and inclusions
AI-generated identification · may be incorrectHardness 7 Mohs; translucent pale pink to peach, with a vitreous-to-waxy luster and conchoidal fracture. Quartz is trigonal and lacks cleavage; the smooth circular form is polished and carved.
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Physical properties
Hardness 7 Mohs; translucent pale pink to peach, with a vitreous-to-waxy luster and conchoidal fracture. Quartz is trigonal and lacks cleavage; the smooth circular form is polished and carved.
Formation & geological history
Rose quartz crystallizes mainly in granitic pegmatites and hydrothermal veins as silica-rich magma or fluids cool, generally during Precambrian to younger geological events. The bangle is a human-shaped, polished specimen.
Uses & applications
Used for ornamental carvings, beads, bangles, cabochons, and inexpensive jewelry; it has little industrial value in this form.
Geological facts
Its pink color is commonly linked to microscopic inclusions of dumortierite-like material or other trace components, rather than simply manganese. Rose quartz is typically translucent and rarely forms well-developed crystals.
Field identification & locations
Identify it by its even pink color, glassy translucence, hardness, and lack of cleavage; it should resist scratching by a steel knife but can be scratched by topaz or corundum. Major sources include Brazil, Madagascar, India, and South Africa.
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