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; Luster: Vitreous; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Hardness
7 on Mohs scale
Color
Purple, violet
Luster
Vitreous
Identified More mineral
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Physical properties

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

Formation & geological history

Formed in hydrothermal veins or geodes where silica-rich fluids cool and crystallize in volcanic cavities. Commonly found in basalt or other igneous rocks, dating primarily from the Mesozoic era to present.

Uses & applications

Extensively used in jewelry (faceting, cabochons, beads), decorative objects, and as a popular collector specimen. Historically believed to prevent intoxication.

Geological facts

The purple color comes from irradiation and iron impurities within the quartz lattice. When heated, natural amethyst can turn yellow-orange, often sold as 'burnt' citrine.

Field identification & locations

Identify by its hexagonal crystal habit and distinctive purple hue that is often zoned. Found worldwide with major deposits in Brazil and Uruguay. Collectors look for deep saturation and clarity.