
sedimentary
Chert (Flint)
Silicon dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs); Color: Tan, brown, or dirty white; Luster: Waxy to dull pebble-like; Crystal Structure: Microcrystalline (Cryptocrystalline); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.6-2.65
- Hardness
- 6
- Color
- Tan, brown, or dirty white
- Luster
- Waxy to dull pebble-like
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Tan, brown, or dirty white; Luster: Waxy to dull pebble-like; Crystal Structure: Microcrystalline (Cryptocrystalline); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.6-2.65
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like diatoms or radiolaria) or by chemical precipitation in marine environments, often replacing original limestone or chalk layers. This specimen appears water-worn or tumbled.
Uses & applications
Historically used for stone tools and weapons due to its sharp edges; currently used as construction aggregate, road metal, and occasionally for lapidary work.
Geological facts
Chert is a tough, durable rock that resists weathering better than the surrounding limestone it often forms in. It has been used by humans for millions of years to create fire (by sparking against steel) and sharp tools.
Field identification & locations
Identify in the field by its hardness (it will scratch glass) and its characteristic conchoidal fracture which leaves smooth, curved surfaces when broken. It is extremely common in sedimentary riverbeds and gravel deposits worldwide.
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