
sedimentary
Banded Chert
Microcrystalline Quartz (SiO2)
Hardness: 7 Mohs scale; Color: Dark grey to black with brown and tan bands; Luster: Waxy to dull; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 Mohs scale
- Color
- Dark grey to black with brown and tan bands
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 Mohs scale; Color: Dark grey to black with brown and tan bands; Luster: Waxy to dull; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed in marine environments through the accumulation of silica-rich organic remains or chemical precipitation. These bands represent variations in mineral content during deposition over millions of years.
Uses & applications
Historically used for making sharp tools (arrowheads). Currently used for landscaping, as river stones, and for tumbling/polishing by collectors.
Geological facts
Chert is so hard it can strike sparks against steel. This specific specimen’s rounded shape indicates it was water-worn by a river or beach action.
Field identification & locations
Identified by its extreme hardness (cannot be scratched by a steel knife) and smooth, rounded water-worn texture. Commonly found in riverbeds and glacial deposits.
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