
mineral
Amethyst
SiO2 (Silicon Dioxide with iron impurities)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Purple/Violet; Luster: Vitreous/Glassy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Purple/Violet
- Luster
- Vitreous/Glassy
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Physical properties
Hardness: 7 on Mohs scale; Color: Purple/Violet; Luster: Vitreous/Glassy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed in hydrothermal veins or as linings within volcanic rock cavities (geodes). The purple color results from irradiation of trivalent iron impurities within the quartz crystal lattice.
Uses & applications
Primary use is in jewelry and lapidary arts as a semi-precious gemstone. Also highly valued as a collector specimen and popular in the metaphysical community for decorative purposes.
Geological facts
Amethyst was considered a 'Cardinal Gem' until the 18th century, ranked alongside diamonds and rubies in value until major deposits were discovered in Brazil. Its name comes from the Greek word 'amethystos', meaning 'not intoxicated'.
Field identification & locations
Identify in the field by its distinctive purple hue, hexagonal prism crystal habits, and ability to scratch glass. Commonly found in Brazil, Uruguay, Madagascar, and the Lake Superior region of North America.
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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