
mineral
Oceanside Agate (Orbicular Agate)
Silicon Dioxide (SiO2) - Variety of Chalcedony
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale), Color: Greenish-white with circular ring patterns, Luster: Waxy to vitreous, Crystal structure: Trigonal/Microcrystalline, Cleavage: None (conchoidal fracture), Specific Gravity: 2.6-2.7
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs scale), Color: Greenish-white with circular ring patterns, Luster: Waxy to vitreous, Crystal structure: Trigonal/Microcrystalline, Cleavage: None (conchoidal fracture), Specific Gravity: 2.6-2.7
Formation & geological history
Formed through the deposition of silica-rich groundwater into cavities in volcanic rocks (often basalt). The orbicular 'eye' patterns result from rhythmic precipitation of silica. These specimens are often millions of years old (CenozoicEra).
Uses & applications
Used primarily by lapidaries as gemstones for cabochons, jewelry, and by mineral collectors for its unique orbicular aesthetic.
Geological facts
Orbicular agates are sometimes referred to as 'Eye Agates' because the circular bands resemble eyes, which were historically believed to ward off the 'evil eye'.
Field identification & locations
Identify by looking for translucent to opaque silica with distinct circular or 'bubbly' banding. Commonly found in coastal areas or volcanic deposits; similar to patterns seen in Ocean Jasper from Madagascar.
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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