
sedimentary
Chert (Fossiliferous)
Microcrystalline quartz (SiO2)
Hardness: 7 on the Mohs scale, Color: White, cream, and yellowish-tan, Luster: Vitreous to dull, Crystal structure: Microcrystalline/cryptocrystalline quartz (chalcedony), Cleavage: None (exhibits conchoidal fracture), Specific Gravity: 2.60-2.65.
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Physical properties
Hardness: 7 on the Mohs scale, Color: White, cream, and yellowish-tan, Luster: Vitreous to dull, Crystal structure: Microcrystalline/cryptocrystalline quartz (chalcedony), Cleavage: None (exhibits conchoidal fracture), Specific Gravity: 2.60-2.65.
Formation & geological history
Formed through the diagenesis of silica-rich marine sediments, often involving the replacement of limestone or chalk by silica from sponge spicules or radiolaria over millions of years.
Uses & applications
Historically used for making stone tools and arrowheads due to its sharp conchoidal fracture. Today used locally for decorative landscaping or collected as a geological specimen.
Geological facts
Chert containing fossils often displays distinctive small circular pits or impressions where ancient marine organisms or fossil fragments have weathered out.
Field identification & locations
Can be identified in the field by its high hardness (scratches glass), waxy to dull luster, and smooth conchoidal fracture. Frequently found in limestone and chalk formations worldwide.
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