
sedimentary
Chert / Chalcedony Nodule
Silicon Dioxide (SiO2)
Hardness: 6.5-7 on Mohs scale. Color: White, cream, tan, light grey, to pale yellow. Luster: Waxy to vitreous (glassy). Crystal Structure: Microcrystalline/Cryptocrystalline trigonal quartz. Fracture: Conchoidal with sharp edges.
- Hardness
- 6
- Color
- White, cream, tan, light grey, to pale yellow
- Luster
- Waxy to vitreous (glassy)
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Physical properties
Hardness: 6.5-7 on Mohs scale. Color: White, cream, tan, light grey, to pale yellow. Luster: Waxy to vitreous (glassy). Crystal Structure: Microcrystalline/Cryptocrystalline trigonal quartz. Fracture: Conchoidal with sharp edges.
Formation & geological history
Formed through the accumulation of silica-rich fluids or biological oozes (such as radiolarians or diatoms) in sedimentary environments, often replacing carbonate rocks like limestone or chalk. Commonly found in Marine Cretaceous or Tertiary sedimentary deposits worldwide.
Uses & applications
Historically used for stone tools, arrowheads, and spark-striking flints. Modern uses include lapidary arts, tumbling, specimen collecting, and decorative rock carving.
Geological facts
Chert and chalcedony were among the most critical resources for prehistoric humans due to their ability to fracture with predictable, razor-sharp conchoidal edges.
Field identification & locations
Look for a chalky outer weathered rind (cortex) covering a dense, fine-grained, translucent to opaque quartz interior that easily scratches glass and steel.
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