Rock Identifier
Tumbled amethyst (Quartz, SiO₂; purple coloration from trace iron and irradiation) — mineral
mineral

Tumbled amethyst

Quartz, SiO₂; purple coloration from trace iron and irradiation

AI-generated identification · may be incorrect

Mohs hardness 7; translucent purple with vitreous luster and irregular internal fractures or inclusions. Trigonal crystal structure; no cleavage, with conchoidal fracture. The pictured piece is polished and rounded.

Identified More mineral →
Explore Tumbled amethyst in the encyclopedia →

Identify your own rocks.

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

Physical properties

Mohs hardness 7; translucent purple with vitreous luster and irregular internal fractures or inclusions. Trigonal crystal structure; no cleavage, with conchoidal fracture. The pictured piece is polished and rounded.

Formation & geological history

Amethyst forms as quartz crystals in gas cavities and fractures in volcanic rocks, often from silica-rich fluids. Deposits range from ancient to geologically recent; a specimen’s age cannot be determined from the image.

Uses & applications

Used in jewelry, ornaments, carvings, and mineral collections.

Geological facts

Amethyst is the purple variety of quartz; its color can fade with prolonged intense sunlight or heating.

Field identification & locations

Look for glassy luster, hardness sufficient to scratch glass, and purple color; common sources include Brazil, Uruguay, Zambia, and Madagascar. The photo shows a small polished specimen, but provenance and quality are unknown.