Rock Identifier
Tumbled amethyst quartz (Quartz, SiO₂; purple coloration from trace iron and irradiation, with likely milky quartz and iron-stained areas) — gemstone
gemstone

Tumbled amethyst quartz

Quartz, SiO₂; purple coloration from trace iron and irradiation, with likely milky quartz and iron-stained areas

AI-generated identification · may be incorrect

Hardness 7 Mohs; purple, white, and yellow-brown coloration; vitreous to waxy luster; trigonal crystal structure; no cleavage, with conchoidal fracture; specific gravity about 2.65. The rounded surface indicates human tumbling or polishing.

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Physical properties

Hardness 7 Mohs; purple, white, and yellow-brown coloration; vitreous to waxy luster; trigonal crystal structure; no cleavage, with conchoidal fracture; specific gravity about 2.65. The rounded surface indicates human tumbling or polishing.

Formation & geological history

Forms in silica-rich hydrothermal veins and volcanic cavities, commonly as crystal linings in basaltic geodes. Amethyst deposits range from Precambrian to recent, with major sources in Brazil, Uruguay, Zambia, and Bolivia.

Uses & applications

Used for inexpensive cabochons, beads, ornaments, and specimens; high-quality transparent material is used in jewelry. This small, heavily included tumbled piece generally has modest commercial value.

Geological facts

Purple amethyst is the most valued quartz variety, though heating can turn it yellow-orange, producing citrine. Yellow-brown patches may be iron staining or included goethite rather than a separate gemstone.

Field identification & locations

Identify by its purple quartz color, glassy fracture, hardness, and inability to scratch with a steel blade while scratching ordinary glass. Commonly found in geodes and amethyst-rich volcanic cavities.