Rock Identifier
Chert (or Dark Flint) (Microcrystalline Quartz (SiO2)) — sedimentary
sedimentary

Chert (or Dark Flint)

Microcrystalline Quartz (SiO2)

Hardness: 7 (Mohs), Color: Dark brown to black, Luster: Waxy to dull, Structure: Cryptocrystalline, Fracture: Conchoidal, Specific Gravity: 2.65

Identified More sedimentary
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Physical properties

Hardness: 7 (Mohs), Color: Dark brown to black, Luster: Waxy to dull, Structure: Cryptocrystalline, Fracture: Conchoidal, Specific Gravity: 2.65

Formation & geological history

Formed by the precipitation of silica in sedimentary environments, often replacing calcium carbonate or accumulating from the silica-rich remains of microscopic organisms (radiolarians/diatoms) on the ocean floor.

Uses & applications

Historically used for making stone tools due to its sharp edges; modernly used as a decorative stone, in construction aggregate, and occasionally in jewelry as cabochons.

Geological facts

Chert is so hard it can scratch steel and was used by ancient humans to create sparks for fire and sharp edges for weaponry. Dark, high-quality chert is often referred specifically as flint.

Field identification & locations

Identify by its extreme hardness, waxy texture, and conchoidal (shell-like) fracture patterns. Frequently found in limestone beds as nodules or layers.