Rock Identifier
Polished pink gemstone, likely dyed quartz or chalcedony (Uncertain from image; possibilities include dyed quartz (SiO₂) or chalcedony (microcrystalline SiO₂)) — gemstone
gemstone

Polished pink gemstone, likely dyed quartz or chalcedony

Uncertain from image; possibilities include dyed quartz (SiO₂) or chalcedony (microcrystalline SiO₂)

AI-generated identification · may be incorrect

Small polished/tumbled stone with vivid hot-pink color and glossy luster; quartz/chalcedony has Mohs hardness 6.5–7, no visible cleavage, and specific gravity about 2.6. The unusually saturated color may indicate dyeing or coating.

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Physical properties

Small polished/tumbled stone with vivid hot-pink color and glossy luster; quartz/chalcedony has Mohs hardness 6.5–7, no visible cleavage, and specific gravity about 2.6. The unusually saturated color may indicate dyeing or coating.

Formation & geological history

Quartz and chalcedony form in silica-rich hydrothermal veins, cavities, and volcanic rocks; geological ages vary widely. A tumbled specimen is mechanically shaped and polished after collection, and may be artificially colored.

Uses & applications

Used as an inexpensive decorative stone, craft material, cabochon, or novelty gemstone; not typically suitable for high-value jewelry unless naturally colored and well documented.

Geological facts

Image resolution prevents reliable identification; color alone cannot distinguish dyed quartz from dyed agate, rose quartz, or glass. A scratch, magnification, and translucency test would help.

Field identification & locations

Check for color concentration in cracks, pits, or edges, which suggests dye; glassy bubbles or uniform color may indicate glass. Common sources of dyed material include Brazil, China, India, and Madagascar.