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

Chert/Flint Nodule

Microcrystalline Quartz (SiO2)

AI-generated identification · may be incorrect

Hardness of 6.5-7 on the Mohs scale, typically brown, tan, gray, or black, waxy or dull luster, microcrystalline structure, conchoidal fracture.

Identified More sedimentary
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Physical properties

Hardness of 6.5-7 on the Mohs scale, typically brown, tan, gray, or black, waxy or dull luster, microcrystalline structure, conchoidal fracture.

Formation & geological history

Formed as a chemical sedimentary rock, often from the accumulation of silica-rich marine micro-organisms or through chemical precipitation in limestone or chalk beds.

Uses & applications

Historically used for making stone tools (arrowheads, scrapers) and starting fires. Currently used in road construction or as gravel.

Geological facts

Because it breaks with a conchoidal fracture, it can produce very sharp edges, making it one of the most important materials for early human tools.

Field identification & locations

Identify by its hardness (scratches glass), smooth waxy appearance, and conchoidal fracture. Commonly found in riverbeds, glacial deposits, and sedimentary rock formations.