
sedimentary
Chert (and Chalcedony)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Gray, white, brown with mottled patterns; Luster: Waxy to vitreous; Structure: Microcrystalline/cryptocrystalline; Cleavage: None (conchoidal fracture); SG: 2.6
- Hardness
- 6
- Color
- Gray, white, brown with mottled patterns
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Gray, white, brown with mottled patterns; Luster: Waxy to vitreous; Structure: Microcrystalline/cryptocrystalline; Cleavage: None (conchoidal fracture); SG: 2.6
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or chemical precipitation from hydrothermal fluids in limestone or volcanic host rocks.
Uses & applications
Historically used for stone tools (arrowheads); currently used for decorative landscaping, lapidary arts, and as a concrete aggregate.
Geological facts
This specimen appears to be a common variety of chert with chalcedony inclusions. Chert was one of the most vital materials for early humans due to its ability to hold a razor-sharp edge when fractured.
Field identification & locations
Identify by its waxy texture, hardness (it will scratch glass), and shell-like (conchoidal) fracture pattern. Found globally in sedimentary basins and volcanic regions.
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