sedimentary

Chert (variations include Flint or Jasper)

Microcrystalline or Cryptocrystalline Quartz (SiO2)

AI-generated identification · may be incorrect

Hardness: 6.5-7 on Mohs scale; Color: typically gray, brown, tan, or green; Luster: waxy to dull; Crystal structure: trigonal (microscopic); Cleavage: none, exhibits conchoidal fracture.

Hardness: 6
Color: typically gray, brown, tan, or green
Luster: waxy to dull

Identified May 3, 2026More sedimentary →

Explore Chert (variations include Flint or Jasper) in the encyclopedia →

Identify your own rocks.

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

App Store Google Play

Physical properties

Hardness: 6.5-7 on Mohs scale; Color: typically gray, brown, tan, or green; Luster: waxy to dull; Crystal structure: trigonal (microscopic); Cleavage: none, exhibits conchoidal fracture.

Formation & geological history

Formed through the precipitation of silica-rich fluids in marine environments or the accumulation of silica-based skeletal remains of organisms like diatoms and radiolarians. Common in ancient limestone and chalk beds.

Uses & applications

Historically used for stone tools (arrowheads, knives) due to its sharp edges; used today as road gravel, in concrete, and some colorful varieties (Jasper) are used in jewelry.

Geological facts

Chert was one of the most important minerals for early humans because its conchoidal fracture pattern allows it to be worked into extremely sharp blades.

Field identification & locations

Identify in the field by its very hard surface (scratches glass), waxy luster when freshly broken, and smooth, shell-like (conchoidal) fracture surfaces. Commonly found as nodules in limestone outcrops.