
sedimentary
Banded Chert (Flint)
Microcrystalline Quartz (SiO2)
Hardness: 7 on Mohs scale; Color: Cream, grey, and charcoal banding; Luster: Waxy to vitreous; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Cream, grey, and charcoal banding
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: Cream, grey, and charcoal banding; Luster: Waxy to vitreous; Crystal 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 marine environments. This specimen shows typical water-worn rounding, likely from a riverbed or coastal area.
Uses & applications
Historically used for stone tools and weapons due to sharp edges; currently used for decorative stones, landscaping, and as a material for fire-starting (flint and steel).
Geological facts
Chert behaves like glass when broken, creating 'flakes' with edges sharper than a steel scalpel. It is one of the most common materials found at archaeological sites worldwide because of its durability.
Field identification & locations
Identify by its 'waxy' texture and curved, glass-like (conchoidal) fractures. It will easily scratch glass but cannot be scratched by a steel knife. Common in limestone regions and river gravels.
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