Rock Identifier
Amethyst Cluster (Silicon Dioxide (SiO2) with iron impurities) — mineral
mineral

Amethyst Cluster

Silicon Dioxide (SiO2) with iron impurities

Hardness 7 on Mohs scale, vitreous luster, hexagonal (trigonal) crystal system, conchoidal fracture, purple to pale violet tips with clear/white quartz base.

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Physical properties

Hardness 7 on Mohs scale, vitreous luster, hexagonal (trigonal) crystal system, conchoidal fracture, purple to pale violet tips with clear/white quartz base.

Formation & geological history

Formed in hydrothermal veins and basalt geode cavities where silica-rich fluids crystallized under heat and pressure with iron radiation color centers.

Uses & applications

Used primarily in mineral collections, ornamental displays, jewelry, and metaphysical practices.

Geological facts

The distinctive purple color of amethyst comes from trace amounts of iron (Fe3+) incorporated into the crystal lattice, subjected to natural irradiation. It was historically considered as precious as diamond.

Field identification & locations

Identified by its hexagonal crystal points, purple color zoning, and hardness (scratches glass). Commonly found in Brazil, Uruguay, Madagascar, and Thunder Bay, Canada.