
sedimentary
Eye Agate
Chalcedony (Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale. Color: Gray, lavender, and brown concentric banding. Luster: Waxy to vitreous. Crystal structure: Cryptocrystalline (hexagonal). Cleavage: None. Specific Gravity: 2.58-2.64.
- Hardness
- 6
- Color
- Gray, lavender, and brown concentric banding
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale. Color: Gray, lavender, and brown concentric banding. Luster: Waxy to vitreous. Crystal structure: Cryptocrystalline (hexagonal). Cleavage: None. Specific Gravity: 2.58-2.64.
Formation & geological history
Formed by the deposition of silica from groundwater into cavities (gas bubbles) in volcanic or sedimentary rocks. The 'eye' pattern is a result of concentric layering as silica-rich fluids cooled and solidified within the cavity.
Uses & applications
Largely used for lapidary arts, jewelry (cabochons), and collecting. In ancient times, eye agates were valued as talismans believed to protect the wearer from the 'evil eye'.
Geological facts
Agates are one of the oldest gemstones used in jewelry. The unique 'eye' patterns are highly sought after by collectors of patterned chalcedony. This specific specimen appears to be a small nodule that has been polished.
Field identification & locations
Identify by concentric circular banding and translucency when held to light. Common in Brazil, Botswana, and the Lake Superior region of the US. Field identification often requires breaking through a rough, weathered exterior.
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