Rock Identifier
Amethyst Quartz (Silicon Dioxide (SiO2) with iron impurities) — mineral
mineral

Amethyst Quartz

Silicon Dioxide (SiO2) with iron impurities

Hardness: 7 on the Mohs scale. Color: Pale lilac to deep purple. Luster: Vitreous (glassy). Crystal Structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.

Hardness
7 on the Mohs scale
Color
Pale lilac to deep purple
Luster
Vitreous (glassy)
Identified More mineral
Explore Amethyst Quartz in the encyclopedia →

Identify your own rocks.

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

Physical properties

Hardness: 7 on the Mohs scale. Color: Pale lilac to deep purple. Luster: Vitreous (glassy). Crystal Structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.

Formation & geological history

Formed in hydrothermal veins or cavities within hollow igneous rocks (geodes). The purple color is caused by irradiation of trivalent iron impurities within the quartz crystal lattice.

Uses & applications

Primarily used as a semi-precious gemstone in jewelry, for decorative carvings, and as a popular specimen for mineral collectors.

Geological facts

Amethyst was considered a cardinal gem until the 18th century. The name comes from the Ancient Greek 'amethystos', meaning 'not intoxicated', expressing the belief that the stone protected its owner from drunkenness.

Field identification & locations

Identify by its characteristic purple zoning, hexagonal crystal habit, and ability to scratch glass. Common locations include Brazil, Uruguay, Zambia, and South Korea.