Rock Identifier
Flint (Chert Flake / Drill Tool) (SiO2 (Microcrystalline Quartz)) — sedimentary
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
Identified More sedimentary
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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.