sedimentary

Chert (River Pebble)

Microcrystalline silicon dioxide (SiO2)

AI-generated identification · may be incorrect

Hardness: 6.5–7 (Mohs scale); Color: Grayish-green with brownish iron staining; Luster: Dull to waxy; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.6

Hardness: 6
Color: Grayish-green with brownish iron staining
Luster: Dull to waxy

Identified April 15, 2026More sedimentary →

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Physical properties

Formation & geological history

Formed through the accumulation of silica-rich microfossils or chemical precipitation from groundwater. This specimen appears water-worn, indicating it was transported by a river or stream, likely dating from the Paleozoic to Mesozoic eras.

Uses & applications

Historically used for stone tools and sparks (flint). Today used as aggregate in construction, decorative landscaping, and occasionally for lapidary tumbling.

Geological facts

Chert is so durable that it often survives long after the surrounding rock has weathered away. It is chemically identical to quartz but has a much finer grain structure.

Field identification & locations

Identify in the field by its hardness (it will scratch glass) and its smooth, curved conchoidal fractures. Commonly found in riverbeds and within limestone or chalk formations.