
sedimentary
Flint / Chert
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 7 on the Mohs scale; Color: Varies from white, grey, brown to black; Luster: Waxy to vitreous; Crystal structure: Microcrystalline/cryptocrystalline (quartz); Cleavage: None, exhibits conchoidal fracture; Specific gravity: 2.60 - 2.65
- Hardness
- 7 on the Mohs scale
- Color
- Varies from white, grey, brown to black
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 7 on the Mohs scale; Color: Varies from white, grey, brown to black; Luster: Waxy to vitreous; Crystal structure: Microcrystalline/cryptocrystalline (quartz); Cleavage: None, exhibits conchoidal fracture; Specific gravity: 2.60 - 2.65
Formation & geological history
Formed as nodules in sedimentary rocks such as chalk and limestone through the replacement of calcium carbonate by silica-rich solutions in marine environments over millions of years.
Uses & applications
Historically used for making stone tools, arrowheads, and fire-starting (striking against steel). Occasionally used in decorative items and landscaping.
Geological facts
Flint was one of the most important materials for early humans due to its ability to break with very sharp edges (conchoidal fracture) and its durability.
Field identification & locations
Found worldwide, often weathering out of chalk or limestone cliffs and riverbeds. Identified by its waxy luster, conchoidal fracture, and ability to scratch glass.
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