
sedimentary
Chert (Smooth River Stone)
Microcrystalline or cryptocrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Gray with yellowish-brown iron staining; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microscopic); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Gray with yellowish-brown iron staining
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: Gray with yellowish-brown iron staining; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microscopic); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like radiolarians or diatoms) or by chemical precipitation from silica-rich fluids within sedimentary rock layers. This specimen has been smoothed by fluvial (river) erosion over many years.
Uses & applications
Historically used for stone tools/arrowheads due to its sharp edges when broken. Today used in decorative landscaping, aquarium gravel, and as a material for lapidary tumbling.
Geological facts
Chert is extremely durable and chemically stable, which is why it often survives as a smooth pebble in riverbeds long after other rocks have eroded away. Varieties include flint, jasper, and agate.
Field identification & locations
Identify in the field by its waxy appearance, extreme hardness (it will scratch glass), and conchoidal (shell-like) fracture patterns. It is found globally in sedimentary basins and riverbeds.
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