Rock Identifier
Amethyst on Basalt (Silicon dioxide (SiO2) with trace Iron) — mineral
mineral

Amethyst on Basalt

Silicon dioxide (SiO2) with trace Iron

Hardness: 7 on Mohs scale; Color: light to deep purple; Luster: vitreous (glass-like); Crystal Structure: hexagonal (trigonal); Cleavage: none (conchoidal fracture); Specific Gravity: 2.65

Hardness
7 on Mohs scale
Color
light to deep purple
Luster
vitreous (glass-like)
Identified More mineral
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Physical properties

Hardness: 7 on Mohs scale; Color: light to deep purple; Luster: vitreous (glass-like); Crystal Structure: hexagonal (trigonal); Cleavage: none (conchoidal fracture); Specific Gravity: 2.65

Formation & geological history

Formed in hydrothermal environments, specifically within gas cavities (vesicles) of volcanic basalt rock. As silica-rich water cools, crystals grow on the inner walls. Most commercial specimens are from the Cretaceous period (approx. 130 million years ago).

Uses & applications

Primarily used for interior decoration, jewelry, alternative healing practices, and as a popular collector mineral.

Geological facts

The purple color of amethyst comes from irradiation, iron impurities, and the presence of trace elements. It was once considered as valuable as diamonds until large deposits were found in Brazil in the 1700s.

Field identification & locations

Identify by its characteristic purple quartz crystals sitting on a dark, volcanic matrix (basalt). It is most commonly found in Brazil, Uruguay, and Namibia. Collectors should look for deep saturation of color and undamaged crystal points.