sedimentary

Chert (Flint)

Microcrystalline or cryptocrystalline Quartz (SiO2)

AI-generated identification · may be incorrect

Hardness: 7 on Mohs scale; Color: Gray, black, or tan; Luster: Dull to waxy; Structure: Cryptocrystalline (no visible grains); Cleavage: None (exhibits conchoidal fracture); Specific Gravity: 2.65.

Hardness: 7 on Mohs scale
Color: Gray, black, or tan
Luster: Dull to waxy

Identified April 14, 2026More sedimentary →

Explore Chert (Flint) in the encyclopedia →

Identify your own rocks.

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

App Store Google Play

Physical properties

Hardness: 7 on Mohs scale; Color: Gray, black, or tan; Luster: Dull to waxy; Structure: Cryptocrystalline (no visible grains); Cleavage: None (exhibits conchoidal fracture); Specific Gravity: 2.65.

Formation & geological history

Formed through the precipitation of silica from groundwater or the accumulation of siliceous skeletal remains (like diatoms or radiolarians) in marine environments. It is often found as nodules in limestone or chalk beds.

Uses & applications

Historically used for stone tools and starting fires; currently used in construction aggregate, road surfacing, and as a semi-precious gemstone for decorative carvings or jewelry.

Geological facts

Because it breaks with a conchoidal 'shell-like' fracture, it produces extremely sharp edges, making it the primary material for prehistoric arrowheads, scrapers, and knives.

Field identification & locations

Identify by its extreme hardness (cannot be scratched by a steel knife) and its smooth, curved fracture surfaces. It is ubiquitous in sedimentary basins worldwide, particularly where limestone is present.