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

Chert (Grey Chert)

Microcrystalline or Cryptocrystalline Quartz (SiO2)

Hardness: 7 on Mohs scale; Color: Dull grey, tan, or brown; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microscopic); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Hardness
7 on Mohs scale
Color
Dull grey, tan, or brown
Luster
Waxy to vitreous
Identified More sedimentary

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Physical properties

Hardness: 7 on Mohs scale; Color: Dull grey, tan, or brown; Luster: Waxy to vitreous; 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 chemical precipitation from groundwater within limestone or chalk beds. Often occurring as nodules or bedded deposits throughout the Paleozoic to Mesozoic eras.

Uses & applications

Historically used for stone tools (arrowheads, scrapers) due to its sharp edges. Modernly used as road aggregate, in abrasive manufacturing, and occasionally as a decorative landscape stone.

Geological facts

Because it breaks with a conchoidal fracture like glass, it was one of the most important minerals for prehistoric tool making. It is very resistant to chemical weathering and often remains in soil long after the surrounding limestone has dissolved.

Field identification & locations

Identify in the field by its hardness (it can scratch glass and steel), its smooth waxy surface, and shell-like (conchoidal) fracture patterns. Frequently found in riverbeds or eroding out of limestone outcrops in the Midwest and Southern United States.