Rock Identifier
Chert (possibly a worked stone flake) (Microcrystalline quartz, SiO₂) — sedimentary
sedimentary

Chert (possibly a worked stone flake)

Microcrystalline quartz, SiO₂

AI-generated identification · may be incorrect

Brown, dull to slightly waxy surface; chert has Mohs hardness about 7, no cleavage, and a very fine-grained crystalline structure. The triangular shape and sharp edges may indicate it was intentionally chipped into a tool or projectile point.

Identified More sedimentary →
Explore Chert (possibly a worked stone flake) in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Brown, dull to slightly waxy surface; chert has Mohs hardness about 7, no cleavage, and a very fine-grained crystalline structure. The triangular shape and sharp edges may indicate it was intentionally chipped into a tool or projectile point.

Formation & geological history

Chert forms when silica-rich material accumulates and recrystallizes, often in sedimentary rocks; it occurs across many geological ages. If shaped, this piece was made by flintknapping, but its age cannot be determined from the image.

Uses & applications

Chert is used for cutting tools and historically for fire-starting; worked pieces are collected as archaeological or lithic artifacts.

Geological facts

Chert fractures conchoidally, producing sharp edges that made it valuable to prehistoric toolmakers.

Field identification & locations

Look for a smooth, fine-grained texture and curved fracture surfaces; the apparent flake shape alone does not establish its age or whether it is an artifact. Chert is widespread in sedimentary formations worldwide.