
mineral
Amethyst
Silicon dioxide (SiO2)
AI-generated identification · may be incorrectHardness of 7 on the Mohs scale, purple to violet color, vitreous luster, trigonal crystal system, conchoidal fracture with no true cleavage, specific gravity of 2.65.
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Physical properties
Hardness of 7 on the Mohs scale, purple to violet color, vitreous luster, trigonal crystal system, conchoidal fracture with no true cleavage, specific gravity of 2.65.
Formation & geological history
Forms in hydrothermal veins, volcanic gas cavities, or as linings of geodes, typically through the irradiation of trace iron impurities within a quartz crystal lattice.
Uses & applications
Widely used in jewelry, ornamental carvings, metaphysical practices, and mineral collections.
Geological facts
The purple color is caused by irradiation, iron impurities, and the presence of other trace elements. Historically, amethyst was considered a precious gemstone equivalent in value to diamonds, rubies, and emeralds until large deposits were discovered in Brazil.
Field identification & locations
Identified by its distinctive purple color, hexagonal crystal structure with pyramidal terminations (often doubly terminated in specimens like this), and lack of cleavage. Commonly found in Brazil, Uruguay, Zambia, and the United States.
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Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
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Granite
Granite (Phaneritic intrusive igneous rock)
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Septarian Pebble
Septarian nodule / Concretion
sedimentary