Rock Identifier
Tumbled purple chalcedony or low-grade amethyst bead bracelet (Chalcedony (microcrystalline SiO₂), possibly quartz/amethyst; composition is SiO₂) — mineral
mineral

Tumbled purple chalcedony or low-grade amethyst bead bracelet

Chalcedony (microcrystalline SiO₂), possibly quartz/amethyst; composition is SiO₂

AI-generated identification · may be incorrect

Hardness 6.5–7 Mohs; pale lavender, gray-purple, and bluish-gray colors with waxy to vitreous luster. Quartz has a trigonal crystal structure, but chalcedony is cryptocrystalline and shows no visible cleavage; specific gravity is about 2.58–2.65.

Identified More mineral
Explore Tumbled purple chalcedony or low-grade amethyst bead bracelet in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness 6.5–7 Mohs; pale lavender, gray-purple, and bluish-gray colors with waxy to vitreous luster. Quartz has a trigonal crystal structure, but chalcedony is cryptocrystalline and shows no visible cleavage; specific gravity is about 2.58–2.65.

Formation & geological history

Forms when silica-rich groundwater fills cavities and fractures in volcanic rocks, commonly through repeated deposition. The beads are polished and shaped, so their geological age cannot be determined from the image.

Uses & applications

Used for inexpensive jewelry, beads, carvings, and ornamental objects; attractive saturated purple material may be sold as amethyst.

Geological facts

The soft, cloudy appearance and mixed gray-lavender tones are more typical of chalcedony or pale amethyst than gem-grade amethyst. Color may be natural or enhanced by dye or heat treatment.

Field identification & locations

Identify by its glassy/waxy luster, translucency, lack of cleavage, and hardness sufficient to scratch ordinary glass; a gemological test is needed to distinguish chalcedony, amethyst, dyed quartz, and glass. Common sources include Brazil, Uruguay, Madagascar, India, and Mexico.