
mineral
Banded Agate (specifically Gobi Eyes or Eye Agate)
Silicon Dioxide (SiO2) - Variety of Chalcedony
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale), Color: Concentric bands of white, brown, grey, and black, Luster: Waxy to vitreous, Crystal structure: Trigonal (microcrystalline), Cleavage: None/Conchoidal fracture, Specific gravity: 2.60-2.65
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs scale), Color: Concentric bands of white, brown, grey, and black, Luster: Waxy to vitreous, Crystal structure: Trigonal (microcrystalline), Cleavage: None/Conchoidal fracture, Specific gravity: 2.60-2.65
Formation & geological history
Formed as secondary deposits in volcanic cavities or vesicles where silica-rich groundwater rhythmically precipitates layers of chalcedony over millions of years. Many eye agates date back to the Cretaceous or Neogene periods.
Uses & applications
Used primarily in lapidary arts for jewelry, decorative carvings, metaphysical 'eye stones' for protection, and as valued specimens for geological collectors.
Geological facts
The 'eye' pattern is created when silica layers deposit in a circular or spherical fashion. The Gobi Desert is famous for these desert-varnished 'Alashan' agates which have been naturally weathered by sand and wind.
Field identification & locations
Identify by its distinct concentric circular 'eye' banding and its ability to scratch glass. This specific specimen has been carved into a faceted geometric shape to showcase the internal patterns.
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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