
sedimentary
Chert (River Cobble)
Microcrystalline or cryptocrystalline Quartz (SiO2)
Hardness: 7 (Mohs scale); Color: Brown, tan, and reddish-grey; Luster: Dull to waxy; Structure: Non-crystalline/Massive; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Brown, tan, and reddish-grey
- Luster
- Dull to waxy
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Physical properties
Hardness: 7 (Mohs scale); Color: Brown, tan, and reddish-grey; Luster: Dull to waxy; Structure: Non-crystalline/Massive; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed from the accumulation of silica-rich organic remains (like radiolarians or diatoms) or by chemical precipitation. This specific specimen has been chemically weathered and physically rounded into a 'cobble' by water action in a river or creek bed.
Uses & applications
Historically used for stone tools (arrowheads/scrapers) due to its sharp edges when broken. Today used in landscape construction, road base, and as decorative river rock.
Geological facts
Chert is so hard it can scratch steel; when struck against steel, it can create sparks, which led to its historical use in flintlock firearms and fire-starting.
Field identification & locations
Identify by its extreme hardness, smooth water-worn surface, and waxy luster on fresh breaks. Found globally in stream beds, gravel pits, and sedimentary outcrops.
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