
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
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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.
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