
sedimentary
Chert / Flint
Cryptocrystalline quartz (SiO2)
Hardness of 7 on the Mohs scale, typically brown, grey, white, or black in color, waxy to vitreous luster, conchoidal fracture with no true cleavage, and a specific gravity around 2.60 to 2.65.
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Physical properties
Hardness of 7 on the Mohs scale, typically brown, grey, white, or black in color, waxy to vitreous luster, conchoidal fracture with no true cleavage, and a specific gravity around 2.60 to 2.65.
Formation & geological history
Formed through the chemical precipitation of silica from aqueous solutions or the accumulation of siliceous skeletal remains of microscopic marine organisms (like radiolarians and diatoms) within carbonate sedimentary environments, primarily limestone or chalk, over millions of years.
Uses & applications
Historically used for making stone tools, arrowheads, and fire-starting (flint and steel); currently used in abrasive products, road aggregate, and occasionally in decorative landscaping.
Geological facts
Chert is extremely durable and weather-resistant, which is why prehistoric stone tools made from it survive intact for hundreds of thousands of years. Varieties heavily pigmented with dark organic matter or iron oxides are often specifically called flint.
Field identification & locations
Identified easily by its distinctive conchoidal fracture (curved, sharp glass-like breaking patterns) and high hardness that readily scratches glass and steel. Commonly found weathering out of chalk or limestone formations worldwide.
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