
igneous and sedimentary
River Pebbles (Basalt and Graywacke/Limestone)
Mafic Volcanic Rock / Impure Sandstone
AI-generated identification · may be incorrectHardness: 5-7 (Mohs scale); Color: Dark grey to charcoal black (top) and medium grey with calcite veining (bottom); Luster: Dull/Matte; Structure: Fine-grained/Aphanitic; Shape: Well-rounded/discoidal due to water erosion.
- Hardness
- 5-7 (Mohs scale)
- Luster
- Dull/Matte
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Physical properties
Hardness: 5-7 (Mohs scale); Color: Dark grey to charcoal black (top) and medium grey with calcite veining (bottom); Luster: Dull/Matte; Structure: Fine-grained/Aphanitic; Shape: Well-rounded/discoidal due to water erosion.
Formation & geological history
Formed through volcanic cooling (top) or sedimentary deposition (bottom) followed by long-term mechanical weathering in a high-energy aquatic environment such as a riverbed or coastal beach.
Uses & applications
Landscaping, decorative garden mulch, aquarium substrate, massage stones (basalt), and architectural pebble mosaic.
Geological facts
The smooth, rounded shape is a result of a process called 'abrasion,' where rocks collide with each other in water, wearing down sharp edges over thousands of years.
Field identification & locations
Identify by their smooth, 'soft' texture and lack of sharp edges; common in river basins and glacial deposits. The white lines on the bottom pebble are likely secondary calcite or quartz veins filling ancient fractures.
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igneous