Rock Identifier
Chert (Jasper/Flint variant) (Microcrystalline quartz (SiO2)) — sedimentary
sedimentary

Chert (Jasper/Flint variant)

Microcrystalline quartz (SiO2)

Hardness: 6.5-7 on Mohs scale; Color: Grayish-brown to olive; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline/cryptocrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.

Hardness
6
Color
Grayish-brown to olive
Luster
Waxy to vitreous
Identified More sedimentary
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Physical properties

Hardness: 6.5-7 on Mohs scale; Color: Grayish-brown to olive; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline/cryptocrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.

Formation & geological history

Formed through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or chemical precipitation in marine environments. These specimens are often hundreds of millions of years old, typically found in nodules within limestone or chalk beds.

Uses & applications

Historically used for stone tools (arrowheads/scrapers) due to its sharp edges when fractured. Modernly used in construction aggregate, road surfacing, and as a semi-precious gemstone when colorful (Jasper).

Geological facts

Chert was one of the most vital materials for early humans; its ability to produce a predictable conchoidal fracture allowed for the creation of sophisticated tools and weaponry.

Field identification & locations

Identify in the field by its hardness (will scratch glass), waxy texture, and shell-like (conchoidal) fracture patterns. Look for it in riverbeds or eroding out of sedimentary rock layers.