Rock Identifier
Chert with Quartz Veining (Microcrystalline Quartz (SiO2)) — sedimentary
sedimentary

Chert with Quartz Veining

Microcrystalline Quartz (SiO2)

Hardness: 7 (Mohs scale), Color: Dark grey to black with white quartz veins and some iron oxidation (orange/brown), Luster: Dull to waxy, Crystal structure: Cryptocrystalline, Fracture: Conchoidal to irregular

Identified More sedimentary

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Physical properties

Hardness: 7 (Mohs scale), Color: Dark grey to black with white quartz veins and some iron oxidation (orange/brown), Luster: Dull to waxy, Crystal structure: Cryptocrystalline, Fracture: Conchoidal to irregular

Formation & geological history

Formed by the accumulation of siliceous remains of marine organisms or via chemical precipitation from silica-rich fluids in sedimentary basins. The white veins are later-stage quartz filled fractures.

Uses & applications

Historically used for making stone tools due to its conchoidal fracture. Modern uses include abrasives and road surfacing material.

Geological facts

Chert is essentially a dense form of quartz. It was highly prized by indigenous cultures globally for crafting arrowheads, knives, and scrapers because it produces a very sharp edge.

Field identification & locations

Identify in the field by its high hardness (it will scratch glass) and smooth, shell-like fracture surfaces. Often found as nodules or lenses within limestone formations.