
sedimentary
River Pebble (Granite / Sandstone Cobble)
Stream-rounded Rock Pebble
AI-generated identification · may be incorrectHardness: 6-7 on Mohs scale (quartz/feldspar dominant); Color: Tan, beige, grey, and speckled buff; Luster: Dull to sub-vitreous; Texture: Fine to medium-grained, smooth rounded surface from aqueous erosion; Specific Gravity: Approximately 2.5 - 2.7.
- Hardness
- 6-7 on Mohs scale (quartz/feldspar dominant)
- Color
- Tan, beige, grey, and speckled buff
- Luster
- Dull to sub-vitreous
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Physical properties
Hardness: 6-7 on Mohs scale (quartz/feldspar dominant); Color: Tan, beige, grey, and speckled buff; Luster: Dull to sub-vitreous; Texture: Fine to medium-grained, smooth rounded surface from aqueous erosion; Specific Gravity: Approximately 2.5 - 2.7.
Formation & geological history
Formed through mechanical weathering and stream transport. Pre-existing granite, quartzite, or coarse sandstone fragments are eroded and continuously tumbled along riverbeds or shorelines, smoothing sharp edges into a rounded cobble.
Uses & applications
Landscaping, decorative garden accents, aquarium gravel, construction aggregate, and tactile rock painting or polished crafts.
Geological facts
Smooth river stones are natural indicators of ancient or active water flow. The process of naturally rounding a pebble can take hundreds to thousands of years of constant water action.
Field identification & locations
Identified by its well-rounded spherical or ovoid shape, fine gritty texture, and lack of sharp edges. Commonly found in riverbeds, glacial till, stream deposits, and ocean beaches worldwide.
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