
sedimentary
Agate
Silicon Dioxide (SiO2) - Chalcedony Variety
Hardness: 6.5-7 on the Mohs scale. Color: Brownish-yellow to translucent gray/tan with faint concentric banding. Luster: Waxy to vitreous. Crystal Structure: Microcrystalline/Cryptocrystalline (trigonal). Cleavage: None (conchoidal fracture).
- Hardness
- 6
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on the Mohs scale. Color: Brownish-yellow to translucent gray/tan with faint concentric banding. Luster: Waxy to vitreous. Crystal Structure: Microcrystalline/Cryptocrystalline (trigonal). Cleavage: None (conchoidal fracture).
Formation & geological history
Forms primarily within cavities (geodes) of volcanic or sedimentary rocks through the silica deposition from percolating groundwater over extensive geological periods.
Uses & applications
Used extensively in lapidary arts, jewelry, tumbled stones, ornamental carvings, and historically in scientific equipment like precision balances and mortars.
Geological facts
Agates are known for their distinctive color banding caused by trace impurities like iron and manganese during layer deposition. No two natural agates are completely identical.
Field identification & locations
Identified by its waxy luster, translucency when backlit, and subtle concentric or parallel banding patterns. Commonly found along riverbeds, gravel deposits, and volcanic fields worldwide (e.g., Lake Superior region, Brazil, Madagascar).
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