
sedimentary
Agatized Chert / Chalcedony
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale), Color: tan, yellow, and translucent white, Luster: waxy to vitreous, Crystal Structure: Cryptocrystalline (Microcrystalline Quartz), Cleavage: None (has conchoidal fracture), Specific Gravity: 2.58-2.64
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs scale), Color: tan, yellow, and translucent white, Luster: waxy to vitreous, Crystal Structure: Cryptocrystalline (Microcrystalline Quartz), Cleavage: None (has conchoidal fracture), Specific Gravity: 2.58-2.64
Formation & geological history
Formed through the precipitation of silica from groundwater into cavities or replacing organic matter in sedimentary rock layers. Often found in ancient riverbeds or limestone deposits where silica-rich fluids circulated millions of years ago.
Uses & applications
Commonly used for lapidary work (polishing and cabochons), primitive tool making (arrowheads/knapping), and as decorative landscaping stone.
Geological facts
This specimen shows clear 'banding' or swirls characteristic of agate, which is a translucent variety of chalcedony. The rough, pitted exterior is typical of river-worn stones where the harder silica mineral survives while the surrounding matrix wears away.
Field identification & locations
Identify in the field by its waxy texture, translucent edges when held to light, and characteristic 'conchoidal' (shell-like) chips on the corners. Found frequently in the American Midwest and Great Lakes region riverbeds.
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