
sedimentary
Chert (Flint / Chalcedony pebble)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5 - 7 on the Mohs scale. Color: Brownish-gray, translucent to opaque. Luster: Waxy to vitreous or dull. Cleavage: None (shows characteristic conchoidal fracture). Microcrystalline structure.
- Hardness
- 6
- Color
- Brownish-gray, translucent to opaque
- Luster
- Waxy to vitreous or dull
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Physical properties
Hardness: 6.5 - 7 on the Mohs scale. Color: Brownish-gray, translucent to opaque. Luster: Waxy to vitreous or dull. Cleavage: None (shows characteristic conchoidal fracture). Microcrystalline structure.
Formation & geological history
Formed through the accumulation and chemical precipitation of silica-rich biogenic sediment (like radiolarian or sponge spicules) or chemical replacement of carbonates in sedimentary marine environments, often tumbled into smooth pebbles by water action.
Uses & applications
Historically used for stone tools, arrowheads, and spark-striking fire starters due to its sharpness when fractured and high hardness. Currently used in jewelry, landscaping, and lapidary tumbling.
Geological facts
Chert and flint were among the very first materials used by early humans in the Stone Age to manufacture sharp tools. It produces a sharp edge that can be sharper than a modern surgical scalpel.
Field identification & locations
Identify in the field by its hardness (scratches glass easily), waxy luster, and distinctive curved (conchoidal) shell-like fractures along chipped edges. Very common along gravel beds, riverbanks, and beaches worldwide.
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