
sedimentary
Chert (River Pebble)
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs; Color: Brown, tan, earthy tones; Luster: Dull to waxy; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 6
- Color
- Brown, tan, earthy tones
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 Mohs; Color: Brown, tan, earthy tones; Luster: Dull to waxy; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like radiolaria or diatoms) or chemical precipitation in sedimentary environments. These pebbles are typically worn smooth by water transport in rivers.
Uses & applications
Historically used for stone tools/fire-starting; currently used for landscaping, aggregate in construction, and as aquarium or decorative stones.
Geological facts
Chert is extremely durable and chemically stable, which is why it often survives as rounded pebbles in riverbeds long after other rocks have eroded away. It was a primary material for prehistoric arrowheads.
Field identification & locations
Identify by its extreme hardness (cannot be scratched by a steel knife) and its smooth, rounded 'water-worn' texture. Found globally in riverbanks, beaches, and gravel pits.
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