sedimentary

Chert Nodule / Ironstone Concretion

Microcrystalline Quartz (SiO2) with Iron Oxides

AI-generated identification · may be incorrect

Hardness: 6.5 to 7 on Mohs scale. Color: Brownish-red, tan, rust, and yellowish-grey hues due to iron oxide staining. Luster: Dull, earthy, to waxy. Structure: Cryptocrystalline to microcrystalline. Cleavage: None (conchoidal fracture).

Hardness: 6
Luster: Dull, earthy, to waxy

Identified July 24, 2026More sedimentary →

Explore Chert Nodule / Ironstone Concretion in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

App Store Google Play

Physical properties

Formation & geological history

Formed in sedimentary rock layers, primarily limestone or chalk, where silica-rich fluids precipitated around organic or mineral cores, often enriched with iron compounds during diagenesis.

Uses & applications

Historically used for stone tools and fire-starting (flint). Commonly collected as decorative river rocks, natural sculptures, or geological curiosities.

Geological facts

Ironstone concretions and chert nodules often develop strange, organic-looking shapes due to differential weathering, leading people to frequently mistake them for fossils, meteorites, or petrified wood.

Field identification & locations

Identified by its high hardness (scratches glass), smooth waxy-to-dull texture, heavy weight if iron-rich, and irregular smoothed nodular form. Frequently found in riverbeds, limestone quarries, and coastal bluffs worldwide.