
sedimentary
Chert
Microcrystalline quartz (SiO2)
Hardness: 7 on the Mohs scale. Color: various shades of white, grey, brown, yellowish-brown, or black. Luster: waxy to vitreous. Crystal structure: microcrystalline/cryptocrystalline quartz (chalcedony). Cleavage: none (conchoidal fracture). Specific gravity: 2.60 to 2.65.
- Hardness
- 7 on the Mohs scale
- Luster
- waxy to vitreous
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Physical properties
Hardness: 7 on the Mohs scale. Color: various shades of white, grey, brown, yellowish-brown, or black. Luster: waxy to vitreous. Crystal structure: microcrystalline/cryptocrystalline quartz (chalcedony). Cleavage: none (conchoidal fracture). Specific gravity: 2.60 to 2.65.
Formation & geological history
Formed through chemical and biochemical precipitation in marine environments, often replacing limestone or chalk during diagenesis through the accumulation of siliceous skeletal remains of microscopic organisms like radiolarians or diatoms.
Uses & applications
Historically used for making stone tools, arrowheads, and blades due to its sharp conchoidal fracture. Today used in abrasives, road construction, and decorative landscaping.
Geological facts
Chert has been utilized by humans for hundreds of thousands of years for tool-making. Varieties include flint, jasper, and chalcedony. When struck with steel, chert produces sparks, making it vital for fire-starting throughout history.
Field identification & locations
Easily identified by its extreme hardness (scratches glass), waxy luster, and distinctive conchoidal (shell-like) fracture. Commonly found embedded in limestone and chalk formations worldwide.
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