Rock Identifier
Colorless faceted gemstones, likely quartz (rock crystal) (Quartz, silicon dioxide (SiO₂), trigonal crystal system) — gemstone
gemstone

Colorless faceted gemstones, likely quartz (rock crystal)

Quartz, silicon dioxide (SiO₂), trigonal crystal system

AI-generated identification · may be incorrect

Transparent to translucent, colorless, glassy luster, and conchoidal fracture; Mohs hardness 7, specific gravity about 2.65. The stones are cut and faceted, so natural crystal faces and cleavage are not visible; inclusions and cutting quality vary.

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Physical properties

Transparent to translucent, colorless, glassy luster, and conchoidal fracture; Mohs hardness 7, specific gravity about 2.65. The stones are cut and faceted, so natural crystal faces and cleavage are not visible; inclusions and cutting quality vary.

Formation & geological history

Quartz crystallizes from silica-rich hydrothermal fluids and igneous pegmatites, commonly in veins and cavities from many geological ages. These specimens have been shaped and polished by human processing.

Uses & applications

Used as inexpensive decorative gemstones, jewelry accents, teaching specimens, and crystal collections. Faceted quartz generally has modest value unless exceptionally clear, large, or well cut.

Geological facts

The photograph alone cannot reliably distinguish quartz from colorless topaz, zircon, beryl, or synthetic glass. Quartz is piezoelectric and is widely used in oscillators and electronics.

Field identification & locations

Field identification requires a hardness test: quartz scratches ordinary glass but not readily with a steel nail; it lacks cleavage and has a typical SG near 2.65. Common sources include Brazil, Madagascar, the United States, and India.