
sedimentary
River Pebble
Weathered Rock Fragment
Hardness varies based on mineral composition (typically 6-7 on Mohs scale if quartz-based); gray to brown color; dull luster; amorphous or cryptocrystalline structure; no distinct cleavage; specific gravity around 2.65.
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Physical properties
Hardness varies based on mineral composition (typically 6-7 on Mohs scale if quartz-based); gray to brown color; dull luster; amorphous or cryptocrystalline structure; no distinct cleavage; specific gravity around 2.65.
Formation & geological history
Formed through the weathering and erosion of parent rocks, followed by transport via rivers and streams where water action rounds the edges over long periods.
Uses & applications
Used in landscaping, decorative garden paths, concrete aggregate, and sometimes in hobbyist rock tumbling.
Geological facts
Water-worn pebbles can travel miles downstream from their original source, becoming progressively smoother and more rounded due to abrasion against other rocks in the riverbed.
Field identification & locations
Commonly found along riverbeds, beaches, and ancient alluvial deposits. Identified by its smooth, rounded shape and lack of sharp edges.
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