Rock Identifier
Amethyst and mixed gemstone bracelet (Amethyst: purple quartz, silicon dioxide (SiO₂); likely accompanied by other quartz or decorative mineral beads) — gemstone
gemstone

Amethyst and mixed gemstone bracelet

Amethyst: purple quartz, silicon dioxide (SiO₂); likely accompanied by other quartz or decorative mineral beads

AI-generated identification · may be incorrect

Visible beads are polished, translucent purple-to-blue stones with vitreous luster; amethyst is Mohs hardness 7, trigonal crystal structure, no cleavage, and specific gravity about 2.65. Exact identification of the darker and blue beads requires close examination.

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Physical properties

Visible beads are polished, translucent purple-to-blue stones with vitreous luster; amethyst is Mohs hardness 7, trigonal crystal structure, no cleavage, and specific gravity about 2.65. Exact identification of the darker and blue beads requires close examination.

Formation & geological history

Amethyst forms when iron-bearing quartz crystallizes in cavities of volcanic rocks, commonly basalt, through hydrothermal fluids; most deposits are Cenozoic to Precambrian in age. The bracelet is human-processed by cutting, drilling, and polishing.

Uses & applications

Used primarily in jewelry and ornamental objects; quartz is also important industrially in glass, electronics, and abrasives. Bracelet value is mainly determined by bead quality, color, treatments, and craftsmanship.

Geological facts

Amethyst’s purple color results from irradiation and iron-related defects in quartz and can fade with prolonged strong heat or sunlight. Common sources include Brazil, Uruguay, Zambia, and Namibia.

Field identification & locations

Identify amethyst by its purple color, glassy luster, hardness, and lack of cleavage; it should scratch glass but not be scratched by a steel knife. This is not classifiable as igneous, sedimentary, or metamorphic because it is a mineral assemblage in jewelry.