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

Amethyst (Geode/Cluster)

Silicon Dioxide (SiO2) with iron impurities

Hardness: 7 (Mohs scale); Color: Pale lavender to deep violet; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None; Specific Gravity: 2.65

Hardness
7 (Mohs scale)
Color
Pale lavender to deep violet
Luster
Vitreous (glassy)
Identified More mineral
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Physical properties

Hardness: 7 (Mohs scale); Color: Pale lavender to deep violet; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None; Specific Gravity: 2.65

Formation & geological history

Formed in hydrothermal veins or as geodes in volcanic rock. Magma/gas bubbles create cavities where silica-rich fluids crystallize over millions of years, primarily in the Cretaceous period specimens from South America.

Uses & applications

Widely used in jewelry (as a gemstone), home decor, metaphysical collecting, and as a birthstone (February).

Geological facts

The purple color comes from irradiation, iron impurities, and the presence of trace elements. It was once considered one of the 'Cardinal Gems' alongside diamond and ruby until large deposits were found in Brazil.

Field identification & locations

Identify by the macrocrystalline quartz structure and distinctive purple hue. Common in Brazil and Uruguay geodes. Look for hexagonal points and a white or grey outer rind (host rock).