Rock Identifier
Amethyst geode fragment (Quartz, SiO₂, colored by trace iron; purple quartz crystals lining a geode cavity) — mineral
mineral

Amethyst geode fragment

Quartz, SiO₂, colored by trace iron; purple quartz crystals lining a geode cavity

AI-generated identification · may be incorrect

Visible purple crystalline interior with a dark gray-brown outer rind. Quartz has Mohs hardness 7, vitreous luster, and a trigonal crystal structure; the specimen appears to be a small cut or broken geode section.

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Physical properties

Visible purple crystalline interior with a dark gray-brown outer rind. Quartz has Mohs hardness 7, vitreous luster, and a trigonal crystal structure; the specimen appears to be a small cut or broken geode section.

Formation & geological history

Amethyst crystals formed as silica-rich fluids deposited quartz inside a cavity in volcanic rock; iron impurities and natural radiation produced the purple color. The exact age and locality cannot be determined from the image.

Uses & applications

Amethyst is used in jewelry, ornaments, and mineral collections; geode fragments are commonly displayed as curiosities.

Geological facts

Amethyst is the purple variety of quartz, and its color can fade with prolonged exposure to strong sunlight.

Field identification & locations

Identify it by the purple quartz crystals and contrasting outer rind; notable sources include Brazil, Uruguay, and Zambia. The image does not establish provenance or gem quality.