Rock Identifier
Chert (Flint/Gray Chalcedony) (Silicon Dioxide (SiO2)) — sedimentary
sedimentary

Chert (Flint/Gray Chalcedony)

Silicon Dioxide (SiO2)

Hardness: 7 (Mohs scale); Color: Gray to brownish-gray; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline; Cleavage: None (Conchoidal fracture); Specific gravity: 2.6-2.7

Hardness
7 (Mohs scale)
Color
Gray to brownish-gray
Luster
Waxy to dull
Identified More sedimentary

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Physical properties

Hardness: 7 (Mohs scale); Color: Gray to brownish-gray; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline; Cleavage: None (Conchoidal fracture); Specific gravity: 2.6-2.7

Formation & geological history

Formed through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or by chemical precipitation in marine environments and limestone cavities. Age varies widely from Precambrian to Cenozoic.

Uses & applications

Historically used for making stone tools and starting fires; currently used as filler in construction, decorative landscaping, and occasionally for cabochon jewelry or flintknapping art.

Geological facts

Chert and flint were among the first materials used by early humans to create sophisticated tools due to their predictable fracturing patterns. Gray chert is often part of the 'Lake Superior Agate' family when found in the American Midwest.

Field identification & locations

Identify in the field by looking for smooth, shell-like (conchoidal) fractures and its ability to scratch glass. Commonly found in riverbeds, glacial till, and embedded in limestone/dolomite outcrops.