Rock Identifier
Pink quartz geode (Quartz geode; silicon dioxide (SiO₂), commonly chalcedony with drusy quartz) — mineral
mineral

Pink quartz geode

Quartz geode; silicon dioxide (SiO₂), commonly chalcedony with drusy quartz

AI-generated identification · may be incorrect

White to pale pink, sugary drusy crystals lining a hollow cavity; vitreous to pearly luster, trigonal quartz structure, conchoidal fracture, no cleavage, Mohs hardness 7, and specific gravity about 2.65. Pink coloration may reflect iron, inclusions, or surface treatment.

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Physical properties

White to pale pink, sugary drusy crystals lining a hollow cavity; vitreous to pearly luster, trigonal quartz structure, conchoidal fracture, no cleavage, Mohs hardness 7, and specific gravity about 2.65. Pink coloration may reflect iron, inclusions, or surface treatment.

Formation & geological history

Forms when silica-rich groundwater deposits chalcedony and quartz crystals inside gas vesicles or cavities in volcanic rock, usually basalt. The cavity may develop over months to millions of years; the specimen’s precise age cannot be determined from the image.

Uses & applications

Used as a decorative and lapidary specimen, crystal display, and occasional jewelry material; geodes are popular educational and collector objects.

Geological facts

The hollow interior is called a vug, and the tiny crystals are termed drusy or druzy quartz. Brown-orange patches may be iron-oxide staining or inclusions.

Field identification & locations

Identify by the hollow rounded cavity, sparkly quartz lining, hardness, and lack of cleavage; common sources include Brazil, Uruguay, Mexico, and the western United States. Avoid assuming the pink color is natural without testing or provenance.