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

Chert

Microcrystalline Quartz (SiO2)

Hardness: 7 (Mohs scale), Color: tan, brown, or gray, Luster: waxy to dull, Crystal Structure: Cryptocrystalline, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65

Identified More sedimentary

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Physical properties

Hardness: 7 (Mohs scale), Color: tan, brown, or gray, Luster: waxy to dull, Crystal Structure: Cryptocrystalline, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65

Formation & geological history

Forms through the precipitation of silica from seawater or the accumulation of silica-rich organic remains like sponges and radiolarians. Often found as nodules in limestone or as bedded deposits.

Uses & applications

Historically used for making stone tools (arrowheads). Modern uses include road surfacing materials, decorative landscaping, and as a raw material for silicon production.

Geological facts

Because it breaks with a conchoidal fracture like glass, it produces very sharp edges, which is why it was the primary material for prehistoric weapons and cutting tools.

Field identification & locations

Identify in the field by its extreme hardness (cannot be scratched by a steel knife) and its waxy luster on fresh broken surfaces. Found globally in sedimentary basins.