Rock Identifier
Chert (specifically Flint or Jasper variant) (Microcrystalline or Cryptocrystalline Silicon Dioxide (SiO2)) — sedimentary
sedimentary

Chert (specifically Flint or Jasper variant)

Microcrystalline or Cryptocrystalline Silicon Dioxide (SiO2)

Hardness: 7 (Mohs scale); Color: Variegated brown, tan, and creamy white cortex; Luster: Waxy to dull; Crystal structure: Trigonal (microscopic); Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.7

Hardness
7 (Mohs scale)
Color
Variegated brown, tan, and creamy white cortex
Luster
Waxy to dull
Identified More sedimentary

Identify your own rocks.

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

Physical properties

Hardness: 7 (Mohs scale); Color: Variegated brown, tan, and creamy white cortex; Luster: Waxy to dull; Crystal structure: Trigonal (microscopic); Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.7

Formation & geological history

Formed through the accumulation of silica-rich organic remains (like radiolarians or diatoms) or chemical precipitation from hydrothermal fluids in sedimentary basins. Often found as nodules within limestone or chalk beds.

Uses & applications

Historically used for stone tools/weapons (knapping) and fire-starting. Industrially used in construction aggregates; aesthetically used for lapidary work, cabochons, and decorative landscaping.

Geological facts

Chert was one of the most vital materials for early humans due to its ability to fracture into razor-sharp edges. It is extremely resistant to chemical weathering, which is why it often remains as 'river rocks' long after the surrounding limestone has eroded.

Field identification & locations

Identify in the field by its smooth, shell-like (conchoidal) fracture surfaces and its ability to scratch glass. Commonly found in riverbeds, glacial tills, and chalk cliffs. Collectors look for unique color patterns and translucency.