
sedimentary
Chert (Beach Pebble)
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Gray, tan, white, and black swirls; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 6
- Color
- Gray, tan, white, and black swirls
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Gray, tan, white, and black swirls; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like radiolaria or diatoms) or chemical precipitation in marine environments. This specimen has been rounded and polished by wave action on a beach.
Uses & applications
Historically used for stone tools and starting fires (flint); currently used for decorative landscaping, jewelry (as river stones), and as a study specimen for sedimentary processes.
Geological facts
Chert is extremely durable and chemically stable, which is why it often survives as smooth pebbles on beaches while softer rocks erode into sand. It is essentially the same material as flint, jasper, and agate.
Field identification & locations
Identify in the field by its hardness (it will scratch glass), its smooth waxy feel, and its curved conchoidal fractures. Commonly found in riverbeds and coastal shorelines where sedimentary layers have eroded.
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