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

Green Chert

Microcrystalline Quartz (SiO2)

Hardness: 6.5-7 on Mohs scale; Color: dull green to olive; Luster: waxy to vitreous; Crystal structure: Trigonal/Microcrystalline; Cleavage: none, exhibits conchoidal fracture; Specific gravity: approx 2.65.

Hardness
6
Color
dull green to olive
Luster
waxy to vitreous
Identified More sedimentary

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Physical properties

Hardness: 6.5-7 on Mohs scale; Color: dull green to olive; Luster: waxy to vitreous; Crystal structure: Trigonal/Microcrystalline; Cleavage: none, exhibits conchoidal fracture; Specific gravity: approx 2.65.

Formation & geological history

Formed from the accumulation of silica-rich organic remains (like radiolaria or diatoms) or chemical precipitation in marine environments; typically Paleozoic to Mesozoic in age.

Uses & applications

Historically used for stone tools (arrowheads/scrapers), currently used as decorative gravel, in lapidary work, and as a geological study specimen.

Geological facts

Green chert is often associated with the Franciscan Complex in California; it is a tough, durable rock that was highly prized by indigenous peoples for its sharp edge when flaked.

Field identification & locations

Identify in the field by its hardness (will scratch glass), waxy appearance, and characteristic shell-like (conchoidal) curved breaks. Common in coastal mountain ranges.