
mineral
Chalcedony (River or Beach Pebbles)
Chalcedony (Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 6.5–7 (Mohs scale); Color: translucent tan, honey-yellow, brown, and green; Luster: waxy to vitreous; Crystal Structure: microcrystalline/cryptocrystalline; Cleavage: none; Fracture: conchoidal.
- Hardness
- 6
- Color
- translucent tan, honey-yellow, brown, and green
- Luster
- waxy to vitreous
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Physical properties
Hardness: 6.5–7 (Mohs scale); Color: translucent tan, honey-yellow, brown, and green; Luster: waxy to vitreous; Crystal Structure: microcrystalline/cryptocrystalline; Cleavage: none; Fracture: conchoidal.
Formation & geological history
These are water-worn cryptocrystalline quartz nodules (chalcedony and chert). They form via the precipitation of silica from groundwater in volcanic or sedimentary cavities. Their rounded shape indicates long-term transport in high-energy aqueous environments like rivers or coastal shorelines.
Uses & applications
Used primarily as decorative gravel, aquarium stones, and for lapidary arts like tumbling or cabochon making. Fine chalcedony is used in jewelry.
Geological facts
The smooth, rounded 'potato' look is caused by constant abrasion against other rocks in water. The green specimens visible in the photo may be green chalcedony (chrysoprase or jasper) or piece of sea glass.
Field identification & locations
Look for a waxy texture and translucency when held to a light source. These are common in riverbeds, glacial till, and coastal beaches globally. They are excellent candidates for rock tumblers.
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