
sedimentary
Chert (and Flint)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Dark grey, black, brown, or tan; Luster: Waxy to dull; Crystal Structure: Microcrystalline (Cryptocrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Dark grey, black, brown, or tan
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 (Mohs scale); Color: Dark grey, black, brown, or tan; Luster: Waxy to dull; Crystal Structure: Microcrystalline (Cryptocrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like radiolarians or diatoms) or by chemical precipitation from groundwater within sedimentary beds like limestone. Found in strata dating back to the Precambrian era.
Uses & applications
Historically used for stone tools and starting fires (flint); currently used in road construction, as an abrasive, and sometimes in jewelry (as jasper or agate variants).
Geological facts
Chert was one of the most important materials for early humans because its conchoidal fracture produces extremely sharp edges suitable for arrowheads and knives. It is chemically very stable and resistant to weathering.
Field identification & locations
Identify in the field by its waxy texture, extreme hardness (can scratch glass), and distinctive shell-like (conchoidal) curved fracture lines when broken. Commonly found in riverbeds or as nodules within limestone outcrops.
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