Rock Identifier
River Cobble (likely Basalt or Chert) (Siliceous River Rock / Microcrystalline Quartz / Mafic Igneous) — igneous/sedimentary
igneous/sedimentary

River Cobble (likely Basalt or Chert)

Siliceous River Rock / Microcrystalline Quartz / Mafic Igneous

Hardness 6-7 (Mohs scale), colors ranging from charcoal grey to earthy brown with weathering rinds, dull to waxy luster, microcrystalline structure, smooth but pitted surface texture due to river erosion.

Identified More igneous/sedimentary

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Physical properties

Hardness 6-7 (Mohs scale), colors ranging from charcoal grey to earthy brown with weathering rinds, dull to waxy luster, microcrystalline structure, smooth but pitted surface texture due to river erosion.

Formation & geological history

Formed through volcanic activity (if basalt) or silica precipitation (if chert), subsequently weathered and polished by fluvial (river) action over thousands of years.

Uses & applications

Commonly used as decorative landscaping stone, in construction aggregates, or as bedding for drainage. Well-worn specimens are often used as 'worry stones' or for aquarium decor.

Geological facts

River rocks are 'geological travelers'; they often originate in high mountain ranges and move hundreds of miles, becoming smaller and smoother as they tumble against other rocks in the currents.

Field identification & locations

Identify by its rounded, water-worn edges and extreme hardness (cannot be scratched by a steel knife). Commonly found in dry creek beds, riverbanks, and glacial moraines.