
mineral
Chalcedony (Agate/Carnelian variant)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Translucent tan to honey-yellow; Luster: Waxy to vitreous; Crystal Structure: Cryptocrystalline (Trigonal/Monoclinic); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58–2.64
- Hardness
- 6
- Color
- Translucent tan to honey-yellow
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Translucent tan to honey-yellow; Luster: Waxy to vitreous; Crystal Structure: Cryptocrystalline (Trigonal/Monoclinic); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58–2.64
Formation & geological history
Formed from the deposition of silica-rich water in cavities of volcanic or sedimentary rocks. This specific piece appears water-worn, suggesting it was found in a riverbed or alluvial deposit.
Uses & applications
Commonly used for lapidary work, decorative carvings, jewelry beads, and as a popular focus for rockhounding collectors.
Geological facts
Chalcedony is a broad term for all cryptocrystalline quartz. When it exhibits banding, it is called Agate; when it is reddish-brown, it is Carnelian. This translucent honey-colored variety is often found in river gravels globally.
Field identification & locations
Identify in the field by its waxy texture, inability to be scratched by a steel knife, and smooth, curved (conchoidal) fracture surfaces. Commonly found in riverbeds, beaches, and desert washes.
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