Rock Identifier
Chert (Microcrystalline Quartz (SiO2)) — sedimentary
sedimentary

Chert

Microcrystalline Quartz (SiO2)

Hardness: 7 on Mohs scale; Color: Gray, tan, brown with waxy luster; Crystal Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Hardness
7 on Mohs scale
Color
Gray, tan, brown with waxy luster
Identified More sedimentary
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Physical properties

Hardness: 7 on Mohs scale; Color: Gray, tan, brown with waxy luster; Crystal Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Formation & geological history

Formed in marine environments through the precipitation of silica or from the accumulation of siliceous remains such as diatoms or radiolarians, often found as nodules in limestone.

Uses & applications

Historically used for stone tools (arrowheads); currently used in road construction, as an abrasive, and occasionally as a decorative landscape stone.

Geological facts

Chert has been used by humans for millions of years because of its ability to fracture into extremely sharp edges. Flint is a high-quality variety of chert.

Field identification & locations

Identify by its waxy appearance, extreme hardness (it will scratch glass), and its characteristic smooth, curved conchoidal fractures.