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

Chert

Microcrystalline Quartz (SiO2)

Hardness: 6.5-7 Mohs; Color: Tan, brown, or grayish; Luster: Dull to waxy; Crystal Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7.

Hardness
6
Color
Tan, brown, or grayish
Luster
Dull to waxy
Identified More sedimentary
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Physical properties

Hardness: 6.5-7 Mohs; Color: Tan, brown, or grayish; Luster: Dull to waxy; Crystal Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7.

Formation & geological history

Formed via the accumulation of siliceous remains of organisms or precipitation from silica-rich fluids within sedimentary basins; often found as nodules in limestone or chalk beds.

Uses & applications

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

Geological facts

Chert is essentially the same mineral as flint, but the name flint is usually reserved for dark varieties found in chalk. It is highly resistant to chemical weathering.

Field identification & locations

Identified by its extreme hardness (scratches glass) and its smooth, shell-like (conchoidal) fracture pattern. Commonly found in riverbeds and gravel pits.