
sedimentary
Yellow Chert Pebble
Microcrystalline Quartz (SiO2)
Hardness: 7 Mohs scale; Color: Dull yellow to mustard; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7. Often smooth and water-worn in pebble form.
- Hardness
- 7 Mohs scale
- Color
- Dull yellow to mustard
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 Mohs scale; Color: Dull yellow to mustard; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7. Often smooth and water-worn in pebble form.
Formation & geological history
Formed via the accumulation of siliceous remains of microscopic organisms (like radiolaria) or chemical precipitation from silica-rich fluids in sedimentary basins. This specimen is a river-rounded or beach-worn pebble.
Uses & applications
Historically used for stone tools (flintknapping); current uses involve landscaping, decorative gravel, and occasionally as a lapidary material for tumbling.
Geological facts
Yellow chert gets its color from iron oxide inclusions like goethite or limonite. It is extremely durable and can survive long-distance transport in rivers and glacial till.
Field identification & locations
Identify in the field by its hardness (cannot be scratched by a steel knife) and waxy, smooth texture. Look for conchoidal (shell-like) fractures on broken edges. Common in riverbeds and gravel deposits worldwide.
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