Rock Identifier
Amethyst (Amethyst (SiO2 - Silicon Dioxide with iron impurities)) — Mineral
Mineral

Amethyst

Amethyst (SiO2 - Silicon Dioxide with iron impurities)

Hardness: 7 on the Mohs scale; Color: Ranges from very dark purple to reddish-purple; Luster: Vitreous; Crystal Structure: Hexagonal (trigonal); Cleavage: None; Specific Gravity: Approximately 2.65

Hardness
7 on the Mohs scale
Color
Ranges from very dark purple to reddish-purple
Luster
Vitreous
Identified More mineral

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Physical properties

Hardness: 7 on the Mohs scale; Color: Ranges from very dark purple to reddish-purple; Luster: Vitreous; Crystal Structure: Hexagonal (trigonal); Cleavage: None; Specific Gravity: Approximately 2.65

Formation & geological history

Amethyst is a variety of quartz that forms in hydrothermal veins and vugs (cavities) within volcanic rocks. It crystallizes from silica-rich fluids at relatively low temperatures. Much of the world's amethyst formed during the Mesozoic and Cenozoic eras.

Uses & applications

Predominantly used as a gemstone in jewelry (rings, necklaces, earrings). Larger specimens are also popular for decorative purposes and as mineral collecting pieces.

Geological facts

Amethyst's purple color is due to irradiation of iron impurities within the quartz crystal. Heat treatment can change the color of amethyst to yellow, orange, or green, often sold as citrine or 'prasiolite' (green amethyst). It has long been associated with royalty and was believed to prevent intoxication.

Field identification & locations

In the field, amethyst can be identified by its distinctive purple color, vitreous luster, and hexagonal crystal habit (though often found as massive or geode fillings). It is commonly found in Brazil (especially Rio Grande do Sul), Uruguay, Bolivia, Siberia (Russia), Zambia, and Canada. For collectors, look for deep, uniform color and good clarity. Be cautious of heat-treated or synthetic amethyst.