Rock Identifier
Chert (specifically Gray/Tan Chert Node) (Microcrystalline Quartz (SiO2)) — sedimentary
sedimentary

Chert (specifically Gray/Tan Chert Node)

Microcrystalline Quartz (SiO2)

Hardness: 7 on Mohs scale; Color: Gray, tan, brownish-green; Luster: Waxy to dull; Crystal structure: Cryptocrystalline/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65

Hardness
7 on Mohs scale
Color
Gray, tan, brownish-green
Luster
Waxy to dull
Identified More sedimentary

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Physical properties

Hardness: 7 on Mohs scale; Color: Gray, tan, brownish-green; Luster: Waxy to dull; Crystal structure: Cryptocrystalline/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65

Formation & geological history

Formed from the accumulation of silica-rich organic remains (like diatoms or radiolaria) or through chemical precipitation within limestone or chalk beds. This specimen appears water-worn, suggesting it was found in a river or alluvial deposit.

Uses & applications

Historically used for stone tools and arrowheads; currently used as construction aggregate, road base, and as decorative landscape stone. It is also collected as a lapidary material for tumbling.

Geological facts

Chert has been used by humans for millions of years to create sharp-edged tools due to its conchoidal fracture. Some types of chert, like flint, were vital for starting fires in early history.

Field identification & locations

Identify in the field by its smooth, waxy feel, hardness (it will scratch glass), and the way it breaks into curved, shell-like flakes. Found globally in sedimentary basins and riverbeds.