
mineral
Amethyst
Crystalline Silicon Dioxide with Iron impurities (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Purple to deep violet with white banding (common in tumbled stones); Luster: Vitreous/glassy; Crystal Structure: Hexagonal; Cleavage: None; Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Luster
- Vitreous/glassy
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Physical properties
Hardness: 7 on Mohs scale; Color: Purple to deep violet with white banding (common in tumbled stones); Luster: Vitreous/glassy; Crystal Structure: Hexagonal; Cleavage: None; Specific Gravity: 2.65
Formation & geological history
Forms in hydrothermal veins and cavities (geodes) within igneous rocks. The purple color is caused by irradiation of iron impurities within the quartz lattice.
Uses & applications
Widely used for jewelry, decorative carvings, spiritual/metaphysical collecting, and as a birthstone for February.
Geological facts
Amethyst was once considered as valuable as diamonds until large deposits were found in Brazil. Its name comes from the Ancient Greek 'amethystos', meaning 'not intoxicated', as it was believed to prevent drunkenness.
Field identification & locations
Identify by its characteristic purple color and ability to scratch glass. Tumbled pieces often show distinct 'V' shaped white patterns known as chevron banding. Commonly found in Brazil, Uruguay, and Zambia.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous