Rock Identifier
Chert (Flint variety) (Microcrystalline or Cryptocrystalline Quartz (SiO2)) — sedimentary
sedimentary

Chert (Flint variety)

Microcrystalline or Cryptocrystalline Quartz (SiO2)

Hardness: 7 on Mohs scale; Color: Gray, tan, brown, or white; Luster: Waxy to dull; Crystal structure: Trigonal (microscopic); Cleavage: None (conchoidal fracture); Specific gravity: 2.65

Hardness
7 on Mohs scale
Color
Gray, tan, brown, or white
Luster
Waxy to dull
Identified More sedimentary

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Physical properties

Hardness: 7 on Mohs scale; Color: Gray, tan, brown, or white; Luster: Waxy to dull; Crystal structure: Trigonal (microscopic); 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 the chemical replacement of limestone/dolomite by silica-rich groundwater. Often found as nodules or lenses within carbonate rock layers.

Uses & applications

Historically used for stone tools (arrowheads, knives) and strike-a-lights. Modernly used as a decorative stone, road aggregate, and for making high-quality ceramics or as a grinding medium.

Geological facts

Because it fractures conchoidally to produce razor-sharp edges, it was the most important material for early human technology. Flint (a dark variety of chert) was essential for spark-ignition systems in early firearms.

Field identification & locations

Identify in the field by its smooth, waxy surface and its ability to scratch glass. Look for the distinct 'shell-like' curved fracture patterns. It is extremely common in areas with limestone bedrock globally.