Amethyst
Silicon Dioxide with iron impurities (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 7 on Mohs scale; Color: Pale lilac to deep purple; Luster: Vitreous (glass-like); Crystal structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & Geological History
Formed in hydrothermal veins or cavities (geodes) of igneous rocks when silica-rich water cools. The purple color is caused by irradiation of trivalent iron (Fe3+). Found in volcanic rocks ranging from prehistoric to modern eras.
Uses & Applications
Predominantly used for jewelry, lapidary arts, spiritual/metaphysical collecting, and as decorative interior specimens.
Geological Facts
Amethyst was considered a 'Precious Stone' until the 18th century when large deposits were found in Brazil. Its name comes from the Greek 'amethystos', meaning 'not intoxicated', as it was believed to prevent drunkenness.
Field Identification & Locations
Identify by its purple color and hexagonal prism crystal habits. Commonly found in Brazil, Uruguay, and Zambia. Collectors look for deep saturation of purple and lack of visible inclusions.
Identified on: 4/22/2026
Mode: Standard