
mineral
Eye Agate
Silicon Dioxide (SiO2) - Banded Chalcedony
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale), Color: Concentric bands of white, tan, and brown, Luster: Waxy to vitreous, Crystal Structure: Trigonal (microcrystalline), Cleavage: None (conchoidal fracture), Specific Gravity: 2.58-2.64
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs scale), Color: Concentric bands of white, tan, and brown, Luster: Waxy to vitreous, Crystal Structure: Trigonal (microcrystalline), Cleavage: None (conchoidal fracture), Specific Gravity: 2.58-2.64
Formation & geological history
Formed as a secondary mineral in volcanic rock cavities (vesicles) through the deposition of silica from groundwater. The 'eye' effect is produced by concentric layering around a central seed or gas bubble over thousands of years.
Uses & applications
Primarily used in jewelry (rings, pendants), as talismans in cultural practices, and as collector specimens for lapidary artists.
Geological facts
Also known as 'Third Eye Agate' or 'Shiva Eye' in some spiritual traditions, it has been used for millennia as an amulet against the 'evil eye'. The concentric rings are natural, though sometimes enhanced by heat treatment.
Field identification & locations
Identify by looking for perfect concentric circles that do not break through the surface like paint. Found commonly in Brazil, India, and the Lake Superior region (USA). Collectors look for high symmetry and sharp contrast in the rings.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous