Rock Identifier
Quartz geode fragment (likely amethyst/citrine-bearing) (Microcrystalline and crystalline quartz, SiO₂, with possible iron staining or amethyst coloration) — mineral
mineral

Quartz geode fragment (likely amethyst/citrine-bearing)

Microcrystalline and crystalline quartz, SiO₂, with possible iron staining or amethyst coloration

AI-generated identification · may be incorrect

Hardness 7 Mohs; translucent brown-gold interior with white crystalline crust, vitreous luster, and uneven fracture. The white material may be chalcedony or druzy quartz; crystal habit is too small/irregular to confirm precisely from the image.

Identified More mineral
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Physical properties

Hardness 7 Mohs; translucent brown-gold interior with white crystalline crust, vitreous luster, and uneven fracture. The white material may be chalcedony or druzy quartz; crystal habit is too small/irregular to confirm precisely from the image.

Formation & geological history

Likely formed as silica-rich fluids filled a cavity in volcanic rock, depositing chalcedony and later quartz crystals. Such geodes commonly formed in Cenozoic basaltic volcanic environments, though exact age and locality cannot be determined visually.

Uses & applications

Used as a decorative specimen, lapidary material, and collectible; attractive pieces may be polished or cut into jewelry. It has little industrial value at this small size.

Geological facts

The brown coloration may reflect iron oxides, smoky quartz, or lighting rather than true citrine. Quartz is one of Earth’s most abundant minerals and is the defining component of many geodes.

Field identification & locations

Look for a hard, glassy surface, conchoidal fracture, and crystals lining a cavity; quartz will scratch ordinary glass but not be scratched by a steel knife. Common sources include Brazil, Uruguay, Mexico, and the western United States.