sedimentary

Chert (variously known as Flint or River Pebble)

Microcrystalline or Cryptocrystalline Quartz (SiO2)

AI-generated identification · may be incorrect

Hardness: 7 on Mohs scale. Color: Tan, grey, and cream banding. Luster: Waxy to dull. Structure: Cryptocrystalline. Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.

Hardness: 7 on Mohs scale
Color: Tan, grey, and cream banding
Luster: Waxy to dull

Identified April 13, 2026More sedimentary →

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Physical properties

Hardness: 7 on Mohs scale. Color: Tan, grey, and cream banding. Luster: Waxy to dull. Structure: Cryptocrystalline. Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.

Formation & geological history

Formed from the accumulation of siliceous remains of microscopic organisms (like diatoms or radiolarians) or chemical precipitation in marine environments. This specimen shows significant rounding from water erosion (fluvial transport).

Uses & applications

Historically used for stone tools and strike-a-lights; currently used in construction aggregate, road base, and as decorative river stones in landscaping.

Geological facts

Chert is so hard it can scratch steel. When broken, it creates exceptionally sharp edges, which is why it was the primary material for prehistoric arrowheads and scrapers.

Field identification & locations

Identify by its 'waxy' texture and conchoidal (shell-like) fractures. It will not react to acid and is harder than a pocket knife blade. Common in riverbeds and limestone outcrops.