Rock Identifier
Amethyst (Quartz variety; chemical formula: SiO₂ (silicon dioxide) with Fe³⁺ impurities) — Mineral
Mineral

Amethyst

Quartz variety; chemical formula: SiO₂ (silicon dioxide) with Fe³⁺ impurities

Hardness: 7 on the Mohs scale. Color: Pale lilac to deep purple. Luster: Vitreous (glassy). Crystal Structure: Hexagonal (trigonal), often found as prismatic crystals with pyramidal terminations. No distinct cleavage, but exhibits conchoidal fracture. Specific Gravity: 2.65.

Hardness
7 on the Mohs scale
Color
Pale lilac to deep purple
Luster
Vitreous (glassy)
Identified More mineral

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Physical properties

Hardness: 7 on the Mohs scale. Color: Pale lilac to deep purple. Luster: Vitreous (glassy). Crystal Structure: Hexagonal (trigonal), often found as prismatic crystals with pyramidal terminations. No distinct cleavage, but exhibits conchoidal fracture. Specific Gravity: 2.65.

Formation & geological history

Amethyst forms in silica-rich igneous and metamorphic rocks, particularly in hydrothermal veins and vugs (cavities) within basalts and other volcanic rocks. It crystallizes from aqueous solutions at relatively low temperatures and pressures. Its purple color is due to irradiation of iron impurities within the quartz lattice. Geologically, it can be found in formations ranging from ancient Precambrian to relatively recent Cenozoic eras, depending on the host rock formation.

Uses & applications

Amethyst is primarily used as a gemstone in jewelry, including rings, necklaces, earrings, and bracelets, like the one pictured. Larger specimens are popular for decorative objects, mineral collections, and as geode displays. Historically, it has also been used for carved ornaments and talismans.

Geological facts

Amethyst's name comes from the Greek 'amethystos,' meaning 'not drunk,' as it was believed to protect its wearer from intoxication. It was highly prized by ancient civilizations and royalty, often featured in crowns and religious jewelry. The color variability can be due to iron impurities within the quartz structure and natural irradiation. Heat treatment can change the color of amethyst, often turning it yellow (citrine) or greenish (prasiolite).

Field identification & locations

Amethyst is commonly found in large deposits in Brazil (especially in basaltic flows forming large geodes), Uruguay, Siberia (Russia), Zambia, Bolivia, and parts of the United States (e.g., Arizona, North Carolina). In the field, it can be identified by its distinctive purple color, vitreous luster, hexagonal crystal habit (though often found as massive or botryoidal aggregates within geodes), and its hardness (scratching glass). The presence of other minerals like calcite or chalcedony can indicate a geode environment. Its distinctive purple hue makes it relatively easy to distinguish from other quartz varieties like citrine (yellow) or clear quartz.