Rock Identifier
Chert (Jasper/Flint variety) (Silicon Dioxide (SiO2)) — sedimentary
sedimentary

Chert (Jasper/Flint variety)

Silicon Dioxide (SiO2)

Hardness: 7 on Mohs scale; Color: Tan, brown, and grey with possible iron oxide staining; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7

Hardness
7 on Mohs scale
Color
Tan, brown, and grey with possible iron oxide staining
Luster
Waxy to dull
Identified More sedimentary
Explore Chert (Jasper/Flint variety) in the encyclopedia →

Identify your own rocks.

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

Physical properties

Hardness: 7 on Mohs scale; Color: Tan, brown, and grey with possible iron oxide staining; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7

Formation & geological history

Formed through the accumulation of silica-rich microfossils (like radiolaria or diatoms) or by chemical precipitation in marine or groundwater environments. Often found as nodules in limestone or chalk beds.

Uses & applications

Historically used for making stone tools (arrowheads/scrapers) due to conchoidal fracturing. Modern uses include road surfacing, decorative gravel, and lapidary work (polishing into cabochons).

Geological facts

Because it breaks with a very sharp edge, chert was one of the most important minerals for early human technological development. It is also sparks when struck against steel, making it vital for early fire-starting and flintlock firearms.

Field identification & locations

Identify by its waxy texture, extreme hardness (it will scratch glass), and the way it breaks into curved, shell-like (conchoidal) shards. Commonly found in creek beds or limestone outcrops.