
sedimentary
River Pebble (Greywacke or Chert mix)
Silicon Dioxide (SiO2) with varying mineral impurities
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale), Color: Dark grey, charcoal, and mottled brown-white, Luster: Dull to slightly waxy when polished, Crystal Structure: Microcrystalline or Cryptocrystalline, Cleavage: None (conchoidal fracture)
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs scale), Color: Dark grey, charcoal, and mottled brown-white, Luster: Dull to slightly waxy when polished, Crystal Structure: Microcrystalline or Cryptocrystalline, Cleavage: None (conchoidal fracture)
Formation & geological history
Formed from the lithification of sand, silt, and clay in deep-water marine environments or as chemical precipitates. This specific specimen has been significantly rounded and smoothed by fluvial or alluvial processes (water erosion in a stream or river).
Uses & applications
Mainly used in construction as aggregate, landscaping, decorative garden stones, and occasionally in lapidary for tumbling to create polished stones.
Geological facts
River pebbles act as geological time capsules, often containing fragments of much older rocks from further upstream. Their smooth, rounded shape is a direct result of 'abrasion,' where stones collide and wear down while being transported by water over miles.
Field identification & locations
Identify by its water-worn, rounded shape and smooth texture. Common in river beds, beaches, and glacial deposits. For identification, check for lack of visible large crystals and high hardness (will scratch glass).
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