Rock Identifier
Amethyst cluster (Quartz, SiO₂; purple coloration is caused mainly by trace iron and natural irradiation) — mineral
mineral

Amethyst cluster

Quartz, SiO₂; purple coloration is caused mainly by trace iron and natural irradiation

AI-generated identification · may be incorrect

Purple, translucent to transparent quartz crystals with a vitreous luster and hexagonal crystal structure; Mohs hardness 7, with no cleavage and conchoidal fracture. The small specimen appears as a rough crystal cluster.

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Physical properties

Purple, translucent to transparent quartz crystals with a vitreous luster and hexagonal crystal structure; Mohs hardness 7, with no cleavage and conchoidal fracture. The small specimen appears as a rough crystal cluster.

Formation & geological history

Amethyst forms as quartz crystals lining cavities in volcanic rocks, often in basalt geodes; deposits range from ancient to geologically recent. The image does not reveal its specific locality or age.

Uses & applications

Commonly collected and used for jewelry, ornaments, and decorative specimens.

Geological facts

Amethyst is the purple variety of quartz; heating can turn some material yellow or orange, resembling citrine.

Field identification & locations

Identify by its purple color, glassy luster, and hard, pointed quartz crystals. Major sources include Brazil, Uruguay, Zambia, and Russia; avoid assuming color alone proves natural origin.