
mineral
Likely rough rose quartz
Quartz, SiO₂ (trigonal crystal structure)
AI-generated identification · may be incorrectPink to reddish, opaque to translucent, with a vitreous luster and irregular fracture; hardness 7 Mohs, no cleavage, specific gravity about 2.65. The image alone cannot confirm the identification; iron staining or another pink mineral is possible.
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Physical properties
Pink to reddish, opaque to translucent, with a vitreous luster and irregular fracture; hardness 7 Mohs, no cleavage, specific gravity about 2.65. The image alone cannot confirm the identification; iron staining or another pink mineral is possible.
Formation & geological history
Quartz crystallizes from silica-rich fluids and pegmatitic melts; rose coloration is commonly linked to trace elements or microscopic inclusions. Specimens occur in Precambrian pegmatites and veins, though this piece’s age and source are unknown.
Uses & applications
Used as an ornamental and lapidary stone, in carvings and beads, and occasionally as a low-cost gemstone; ordinary rough pieces have little industrial value.
Geological facts
Rose quartz is generally massive rather than forming well-defined crystals; its color may fade with prolonged sunlight exposure.
Field identification & locations
Look for a pink color, glassy appearance, hardness sufficient to scratch glass, and no cleavage; common sources include Brazil, Madagascar, South Africa, and the United States. The specimen’s identity and locality cannot be established from the photo alone.
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