Rock Identifier
Agated Chert (Microcrystalline Quartz (SiO2)) — sedimentary
sedimentary

Agated Chert

Microcrystalline Quartz (SiO2)

Hardness of 7 on the Mohs scale, colors ranging from white and cream to brown and red due to iron oxide impurities, waxy to vitreous luster, cryptocrystalline structure with conchoidal fracture.

Identified More sedimentary
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Physical properties

Hardness of 7 on the Mohs scale, colors ranging from white and cream to brown and red due to iron oxide impurities, waxy to vitreous luster, cryptocrystalline structure with conchoidal fracture.

Formation & geological history

Formed in sedimentary environments by the replacement of calcium carbonate in limestone by silica-rich groundwaters, often developing micro-quartz and chalcedony banding over millions of years.

Uses & applications

Used for ornamental carvings, lapidary arts, and as a durable mineral specimen for rock collectors.

Geological facts

Chert and flint have been utilized by humans since prehistoric times for creating sharp tools and weapon points due to its predictable conchoidal fracture.

Field identification & locations

Can be identified by its high hardness (scratches glass), waxy luster, and lack of cleavage. Often found in limestone and chalk deposits globally.