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

Amethyst

Silicon Dioxide (SiO2) with iron impurities

Hardness: 7 on Mohs scale; Color: Purple, violet, to pale lavender, often with white quartz banding (Chevron pattern); Luster: Vitreous/glassy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65.

Hardness
7 on Mohs scale
Luster
Vitreous/glassy
Identified More mineral
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Physical properties

Hardness: 7 on Mohs scale; Color: Purple, violet, to pale lavender, often with white quartz banding (Chevron pattern); Luster: Vitreous/glassy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65.

Formation & geological history

Formed in hydrothermal veins or as linings within volcanic rock cavities (geodes). The purple color comes from irradiation of iron impurities within the quartz lattice. Most commercial deposits are millions of years old.

Uses & applications

Widely used for jewelry (faceted stones and cabochons), ornamental decoration, holistic practices, and as a popular starter specimen for mineral collectors.

Geological facts

Amethyst is the birthstone for February. Its name comes from the Ancient Greek word 'amethystos', meaning 'not intoxicated', as the ancients believed it could prevent drunkenness. Some amethyst can fade if left in direct sunlight for extended periods.

Field identification & locations

Identify by its distinct purple hue and hardness (it will scratch glass). Often found in Brazil, Uruguay, and Zambia. Look for white V-shaped 'chevron' patterns in tumbled stones like this one.