
sedimentary
Beach Agate / Chalcedony Pebble
Silicon Dioxide (SiO2) - Microcrystalline Quartz
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs. Color: translucent grey, beige, and brown with fine white banding and quartz veining. Luster: vitreous to waxy when wet/polished. Structure: microcrystalline/cryptocrystalline. Specific gravity: ~2.6.
- Hardness
- 6
- Luster
- vitreous to waxy when wet/polished
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Physical properties
Hardness: 6.5-7 Mohs. Color: translucent grey, beige, and brown with fine white banding and quartz veining. Luster: vitreous to waxy when wet/polished. Structure: microcrystalline/cryptocrystalline. Specific gravity: ~2.6.
Formation & geological history
Formed by secondary deposition of silica-rich fluids filling cavities (vesicles) within volcanic rocks or fractures in sedimentary beds. Subsequently eroded and naturally rounded by coastal wave action over thousands of years.
Uses & applications
Popular for rock tumbling, lapidary arts, jewelry components, cabochon cutting, and amateur rockhounding collections.
Geological facts
Agates are microcrystalline varieties of quartz known for their translucency and concentric or horizontal banding patterns. Ocean waves naturally polish these stones, giving them a smooth, rounded pebble shape.
Field identification & locations
Look for translucency when backlit by a flashlight, along with fine linear banding or quartz cross-veins on smooth coastal pebbles. Commonly found along gravel beaches and riverbanks in active geological zones.
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