
sedimentary
Chert (Flint)
Microcrystalline quartz (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: Dark blue, grey, or black with conchoidal fracture. Luster: Waxy to vitreous. Crystal structure: Microcrystalline/cryptocrystalline quartz (chalcedony). Cleavage: None, breaks with a sharp conchoidal fracture. Specific gravity: 2.60 to 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Dark blue, grey, or black with conchoidal fracture
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 7 on Mohs scale. Color: Dark blue, grey, or black with conchoidal fracture. Luster: Waxy to vitreous. Crystal structure: Microcrystalline/cryptocrystalline quartz (chalcedony). Cleavage: None, breaks with a sharp conchoidal fracture. Specific gravity: 2.60 to 2.65.
Formation & geological history
Formed through the diagenesis of siliceous oozes from the remains of marine organisms like diatoms or radiolarians, or through the replacement of limestone or chalk by silica-rich groundwater in marine environments over millions of years.
Uses & applications
Historically used for making stone tools, arrowheads, and fire-starting (striking against steel). Today used for decorative landscaping, gravel, and occasionally lapidary arts.
Geological facts
Chert and flint are essentially the same material; the term 'flint' is often used specifically for darker varieties found in chalk, while 'chert' is used for occurrences in limestone.
Field identification & locations
Identified by its waxy luster, hardness that scratches glass, and sharp conchoidal fracture edges. Commonly found embedded as nodules within sedimentary rock formations such as limestone and chalk worldwide.
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