Rock Identifier
Amethyst (Silicon dioxide with iron impurities (SiO2 + Fe3+)) — mineral
mineral

Amethyst

Silicon dioxide with iron impurities (SiO2 + Fe3+)

Hardness: 7 on the Mohs scale; Color: Purple, violet, or lavender; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Hardness
7 on the Mohs scale
Color
Purple, violet, or lavender
Luster
Vitreous (glassy)
Identified More mineral
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Physical properties

Hardness: 7 on the Mohs scale; Color: Purple, violet, or lavender; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Formation & geological history

Formed in hydrothermal veins and geodes when silica-rich water cools in cavities of igneous rocks, such as basalt. The purple color is caused by natural irradiation of trace iron impurities within the quartz crystal lattice.

Uses & applications

Highly valued as a gemstone for jewelry (necklaces, rings, earrings), decorative carvings, and as a popular specimen for mineral collectors and metaphysical practitioners.

Geological facts

The word 'amethyst' comes from the Greek 'amethystos', meaning 'not drunken', as ancient Greeks believed it could prevent intoxication. It is the birthstone for February and was once considered as valuable as diamonds until large deposits were found in Brazil.

Field identification & locations

Identified by its purple color and typical hexagonal prism crystal habit. Common locations include Brazil, Uruguay, Zambia, and South Korea. This specific specimen has been shaped/polished into an obelisk point and wire-wrapped for use as a pendant.