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

Amethyst

Silicon dioxide (SiO2) with iron impurities

Hardness: 7 on Mohs scale; Color: Pale lavender to deep violet; Luster: Vitreous (glassy); Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

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

Identify your own rocks.

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

Physical properties

Hardness: 7 on Mohs scale; Color: Pale lavender to deep violet; Luster: Vitreous (glassy); Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Formation & geological history

Forms in hydrothermal veins or as linings in geodes. The purple color is caused by irradiation of iron impurities within the quartz crystal lattice. Found in volcanic rocks.

Uses & applications

Primarily used as a gemstone in jewelry, as decorative specimens for collectors, and in alternative healing practices (crystal therapy).

Geological facts

Until the 18th century, amethyst was included in the cardinal gemstones alongside diamond, ruby, sapphire, and emerald. Large deposits found in Brazil lowered its market value.

Field identification & locations

Identify by its characteristic purple color and quartz-like fracture. Commonly found in Brazil, Uruguay, Zambia, and South Korea. Look for hexagonal crystal points or purple mass within rock cavities.