
mineral
Botryoidal Chalcedony (Agate)
Cryptocrystalline Quartz (SiO2)
Hardness: 6.5-7.0 (Mohs scale); Color: White, translucent, with orange/carnelian banding; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microscopic); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58–2.64
- Hardness
- 6
- Color
- White, translucent, with orange/carnelian banding
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7.0 (Mohs scale); Color: White, translucent, with orange/carnelian banding; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microscopic); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58–2.64
Formation & geological history
Secondary formation in volcanic or sedimentary rock cavities. It forms when silica-rich hydrothermal fluids precipitate in voids or vugs, often creating 'grape-like' or botryoidal structures over thousands of years. This piece specifically shows features of agate with carnelian-colored iron oxide staining.
Uses & applications
Commonly used as gemstones for jewelry (cabochons), lapidary work, ornamental carvings, and as a popular specimen for mineral collectors due to its unique patterns.
Geological facts
While it appears opaque or solid white, chalcedony is actually composed of micro-fibrous quartz. The orange hue seen in the corner is caused by trace amounts of iron oxide, typically classifying that specific section as carnelian.
Field identification & locations
Identify in the field by its waxy luster, hardness (it will scratch glass), and typical botryoidal (rounded) surface texture. Often found in riverbeds or eroding out of volcanic basalt flows in locations like Oregon, Washington, or Brazil.
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mineral