Rock Identifier
Limonite-stained Chert (Silicon Dioxide (SiO2) with Hydrated Iron Oxide (FeO(OH)·nH2O)) — sedimentary
sedimentary

Limonite-stained Chert

Silicon Dioxide (SiO2) with Hydrated Iron Oxide (FeO(OH)·nH2O)

Hardness: 6.5–7 on Mohs scale (scratches glass); Color: Dark grey to charcoal with yellow-brown (ochre) iron staining; Luster: Waxy to dull; Structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture).

Hardness
6
Luster
Waxy to dull
Identified More sedimentary

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Physical properties

Hardness: 6.5–7 on Mohs scale (scratches glass); Color: Dark grey to charcoal with yellow-brown (ochre) iron staining; Luster: Waxy to dull; Structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture).

Formation & geological history

Formed through the accumulation of silica-rich organic remains or chemical precipitation within sedimentary rock layers, often limestone. The yellow staining (limonite) occurs later through the oxidation and hydration of iron-rich minerals during weathering.

Uses & applications

Historically used for stone tools and starting fires (flint); currently used for construction aggregate, road surfacing, and as decorative landscape stone or lapidary material for polishing.

Geological facts

Chert is a incredibly durable rock that resists chemical weathering. Because of its sharp conchoidal fracture, it was the primary material used by prehistoric humans for arrowheads, spear points, and scrapers.

Field identification & locations

Identify in the field by its smooth, shell-like (conchoidal) fracture surfaces and its ability to scratch glass. It is commonly found in gravel pits, riverbeds, and as nodules within limestone or chalk across North America and Europe.