
sedimentary
Flint (Chert Flake / Drill Tool)
SiO2 (Microcrystalline Quartz)
Hardness: 7 on Mohs scale; Color: Dark grey to blackish-brown; Luster: Waxy to vitreous; Crystal Structure: Cryptocrystalline; Cleavage: None (exhibits prominent conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Dark grey to blackish-brown
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: Dark grey to blackish-brown; Luster: Waxy to vitreous; Crystal Structure: Cryptocrystalline; Cleavage: None (exhibits prominent conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed as nodular masses or layers in sedimentary rocks, predominantly chalk and limestone formations, through chemical precipitation of silica or replacement of carbonate minerals.
Uses & applications
Historically used for knapping into prehistoric tools such as arrowheads, scrapers, drills, and spear points, as well as for spark generation in flintlock firearms and fire-starting. Today used in mineral collections, lapidary arts, and decorative landscaping.
Geological facts
This specimen shows clear signs of deliberate flaking (conchoidal retouching), resembling an worked stone drill, awl, or retouch flake created by flintknapping.
Field identification & locations
Identified by its fine grain, smooth waxy surface, shell-like (conchoidal) curved fractures, and sharp edges. Commonly found in limestone and chalk deposits globally, especially in Europe and North America.
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