Rock Identifier
Chert / Flint (Microcrystalline Quartz (SiO2)) — sedimentary
sedimentary

Chert / Flint

Microcrystalline Quartz (SiO2)

AI-generated identification · may be incorrect

Hardness 6.5-7 on the Mohs scale, typically gray, white, brown, or black with a waxy to dull luster. Exhibits conchoidal fracture when broken.

Identified More sedimentary
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Physical properties

Hardness 6.5-7 on the Mohs scale, typically gray, white, brown, or black with a waxy to dull luster. Exhibits conchoidal fracture when broken.

Formation & geological history

Formed through the accumulation of silica-rich marine microfossils or precipitation of silica in sedimentary environments like limestone or chalk deposits.

Uses & applications

Historically used for making stone tools and sparking fires due to its hardness and conchoidal fracture. Sometimes used as a low-grade aggregate or in lapidary arts.

Geological facts

Flint, a variety of chert, was essential to early human survival for tool making and fire starting.

Field identification & locations

Identified by its dense, fine-grained texture, conchoidal fracture, and ability to scratch glass. Commonly found as nodules in sedimentary rock formations globally.