
sedimentary
Chert Pebble
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Gray, tan, and dark charcoal; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7.
- Hardness
- 7 on Mohs scale
- Color
- Gray, tan, and dark charcoal
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: Gray, tan, and dark charcoal; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7.
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like radiolaria or diatoms) or chemical precipitation from groundwater within limestone or chalk beds. This specimen is water-worn into a river cobble shape.
Uses & applications
Historically used for making stone tools (arrowheads). Modernly used as decorative landscaping stone, in construction aggregate, or for flint-striking to start fires.
Geological facts
Chert is so hard it can scratch glass and steel. Darker varieties are often called flint. It is one of the most durable rocks, often surviving long-term river transport as rounded pebbles.
Field identification & locations
Identify in the field by its extreme hardness, smooth waxy texture when wet, and distinctive shell-like (conchoidal) fractures. Found globally in riverbeds and coastal areas.
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