
sedimentary
Chert Nodule
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 7 Mohs scale. Color: Grayish-brown with waxy to dull luster. Structure: Cryptocrystalline. Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
- Hardness
- 7 Mohs scale
- Color
- Grayish-brown with waxy to dull luster
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Physical properties
Hardness: 7 Mohs scale. Color: Grayish-brown with waxy to dull luster. Structure: Cryptocrystalline. Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
Formation & geological history
Formed in marine sedimentary environments through the precipitation of silica from seawater or the accumulation of siliceous skeletal remains (like radiolaria) within limestone or chalk beds.
Uses & applications
Historically used for stone tools (flint knapping). Today used as laboratory mortar and pestles, road material, or as decorative river rock.
Geological facts
Chert is so durable that it often remains as pebbles in stream beds long after the surrounding limestone has eroded away. Varieties include flint, jasper, and agate.
Field identification & locations
Identify by its extreme hardness (scratches glass), waxy luster when freshly broken, and smooth, rounded water-worn exterior often found in riverbeds.
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