
Mineral
Amethyst
Quartz (SiO2) with trace iron impurities
Hardness: 7 on Mohs scale. Color: Violet to dark purple, often with banding or color zoning. Luster: Vitreous. Crystal Structure: Hexagonal. Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Violet to dark purple, often with banding or color zoning
- Luster
- Vitreous
Identified More mineral →
Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness: 7 on Mohs scale. Color: Violet to dark purple, often with banding or color zoning. Luster: Vitreous. Crystal Structure: Hexagonal. Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
Formation & geological history
Amethyst forms in hydrothermal veins and vugs (cavities) within igneous rocks, particularly basaltic lavas. The violet color is due to irradiation and iron impurities within the crystal lattice. Formation occurs from silica-rich fluids at relatively low temperatures (around 50-250°C). Geological age varies depending on the host rock, but many significant deposits formed during volcanic activity over millions of years.
Uses & applications
Predominantly used as a gemstone in jewelry (rings, necklaces, earrings, bracelets) due to its attractive color and durability. It is also used in ornamental carvings, as decorative pieces for homes, and in spiritual practices for its purported calming and protective properties. Lower-quality or industrial-grade amethyst may be crushed for abrasive uses, though this is less common.
Geological facts
The name 'amethyst' comes from the Ancient Greek word 'amethystos', meaning 'not drunken,' as it was believed to protect its owner from intoxication. Brazil and Uruguay are famous for their large geode formations lined with amethyst crystals. The color of amethyst can be heat-treated to produce citrine (yellow-orange) or green ametrine. It is the birthstone for February.
Field identification & locations
Identify by its distinctive violet to purple color, often found as terminated crystals or clusters within geode cavities or veins. Its hardness allows it to scratch glass. Look for its characteristic hexagonal crystal habit. Commonly found in Brazil, Uruguay, Russia, South Korea, Zambia, Canada, and various locations in the United States. In the field, look for volcanic rocks with vugs or hydrothermal veins. For collectors, well-formed crystals with vibrant, consistent color are highly prized.
More like this
Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
Metamorphic Rock
Green Apatite on Albite
Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]
mineral
Epidote
Epidote - Ca2(Al2,Fe3+)3(SiO4)3(OH)
mineral