Rock Identifier
Chert Nodule (Microcrystalline quartz (SiO2)) — sedimentary
sedimentary

Chert Nodule

Microcrystalline quartz (SiO2)

AI-generated identification · may be incorrect

Mohs hardness of 7; conchoidal fracture; waxy to vitreous luster; translucent to opaque brownish-red color.

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Physical properties

Mohs hardness of 7; conchoidal fracture; waxy to vitreous luster; translucent to opaque brownish-red color.

Formation & geological history

Formed through the chemical precipitation of silica in marine limestone or chalk environments during the Cenozoic or older eras.

Uses & applications

Used historically for primitive stone tools and fire-starting; currently collected as a geological specimen.

Geological facts

Texas regional geology around San Antonio frequently yields chert and flint nodules weathered out from Cretaceous limestone formations.

Field identification & locations

Identify by its extreme hardness, sharp conchoidal edges, and smooth weathered exterior cortex. Common in gravel beds and limestone creeks.