Rock Identifier
Chert / Flint (Chert (Cryptocrystalline Quartz, SiO2)) — sedimentary
sedimentary

Chert / Flint

Chert (Cryptocrystalline Quartz, SiO2)

Hardness: 7 (Mohs scale); Color: Brown, tan, cream; Luster: Waxy to dull; Structure: Cryptocrystalline (microscopic crystals); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.

Hardness
7 (Mohs scale)
Color
Brown, tan, cream
Luster
Waxy to dull
Identified More sedimentary

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Physical properties

Hardness: 7 (Mohs scale); Color: Brown, tan, cream; Luster: Waxy to dull; Structure: Cryptocrystalline (microscopic crystals); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.

Formation & geological history

Formed through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or chemical precipitation from groundwater within limestone or chalk beds. It can date from the Precambrian to the Cenozoic era.

Uses & applications

Historically used for stone tools (arrowheads, scrapers) due to its sharp edges; used in construction as road metal and aggregate; also used in fire-starting kits (flint).

Geological facts

Chert was one of the first materials used by early humans for tools because of its conchoidal fracture, which creates razor-sharp edges. It is incredibly durable and chemically resistant.

Field identification & locations

Identify by its extreme hardness (cannot be scratched by steel), waxy texture, and conchoidal (shell-like) fracture patterns. Frequently found in stream beds or within limestone outcrops.