
mineral
Amethyst
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: light to deep purple; Luster: Vitreous/glassy; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- light to deep purple
- Luster
- Vitreous/glassy
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Physical properties
Hardness: 7 on Mohs scale; Color: light to deep purple; Luster: Vitreous/glassy; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed in hydrothermal veins or cavities (geodes) of igneous and metamorphic rocks. The purple color comes from iron impurities and natural irradiation. Found in deposits ranging from Precambrian to Cenozoic eras.
Uses & applications
Primary use is in jewelry, gemstone cutting, and ornamental decoration. It is also a highly popular mineral for collectors and metaphysical use.
Geological facts
Until the 18th century, amethyst was included in the cardinal gemstones alongside diamond, ruby, emerald, and sapphire. Large deposits in Brazil discovered in the 1700s made it much more accessible.
Field identification & locations
Identify by its characteristic purple hue and inability to be scratched by a steel pocketknife. Commonly found in Brazil, Uruguay, Zambia, and Ontario. Collectors should look for saturated color and clarity.
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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