
mineral
Polished agate slice
Agate, a banded variety of chalcedony (microcrystalline SiO₂)
AI-generated identification · may be incorrectHardness 6.5–7 Mohs; translucent gray, cream, and brown concentric banding; waxy to vitreous luster; cryptocrystalline quartz with no visible cleavage. The irregular outer rind appears natural and may retain druzy quartz or host-rock material.
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Physical properties
Hardness 6.5–7 Mohs; translucent gray, cream, and brown concentric banding; waxy to vitreous luster; cryptocrystalline quartz with no visible cleavage. The irregular outer rind appears natural and may retain druzy quartz or host-rock material.
Formation & geological history
Forms when silica-rich groundwater fills cavities in volcanic rocks, depositing successive layers of chalcedony over millions of years, commonly during the Cenozoic or older volcanic episodes. This specimen has been cut and polished.
Uses & applications
Used for cabochons, jewelry, bookends, decorative slabs, and lapidary ornaments; attractive slices typically sell for about $15–$75, with larger or unusually patterned pieces reaching $100–$300.
Geological facts
The pale concentric bands record changing chemistry and fluid conditions during cavity filling. Agate is a variety of quartz rather than a separate mineral species.
Field identification & locations
Identify by curved or concentric banding, translucency, quartz-like hardness, and inability to scratch with a steel knife; it should scratch glass. Common sources include Brazil, Uruguay, Mexico, India, Madagascar, and the western United States.
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