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

Chert

Microcrystalline Quartz (SiO2)

Hardness: 6.5-7 Mohs; Color: dark grey to black (Flint variety); Luster: waxy to dull; Structure: microcrystalline; Cleavage: none, exhibits strong conchoidal fracture; SG: 2.65.

Hardness
6
Color
dark grey to black (Flint variety)
Luster
waxy to dull
Identified More sedimentary

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Physical properties

Hardness: 6.5-7 Mohs; Color: dark grey to black (Flint variety); Luster: waxy to dull; Structure: microcrystalline; Cleavage: none, exhibits strong conchoidal fracture; SG: 2.65.

Formation & geological history

Formed in marine environments through the accumulation of silica-rich organic remains (diatoms/radiolarians) or chemical precipitation within limestone/chalk beds.

Uses & applications

Used historically for stone tools and fire-starting; currently used as construction aggregate, road surfacing, and sometimes for jewelry as jasper or agate.

Geological facts

Black chert is often called Flint and was the most important material for prehistoric humans to create sharp hunting tools like arrowheads and knives.

Field identification & locations

Identify by its extreme hardness (scratches glass) and smooth, curved (conchoidal) breakage surfaces. Commonly found in riverbeds and limestone outcrops.