
sedimentary
Sandstone Beach Pebble
Clastic Sandstone (SiO2 - Quartz-dominant)
AI-generated identification · may be incorrectHardness: 6-7 Mohs; Color: Tan, beige, or brownish-grey; Luster: Dull or earthy; Crystal structure: Granular/clastic; Cleavage: None; Specific gravity: 2.2-2.8. Smooth, rounded texture due to water erosion.
- Hardness
- 6-7 Mohs
- Color
- Tan, beige, or brownish-grey
- Luster
- Dull or earthy
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Physical properties
Hardness: 6-7 Mohs; Color: Tan, beige, or brownish-grey; Luster: Dull or earthy; Crystal structure: Granular/clastic; Cleavage: None; Specific gravity: 2.2-2.8. Smooth, rounded texture due to water erosion.
Formation & geological history
Formed from the compaction and cementation of sand-sized mineral grains or rock fragments over millions of years. This specific specimen has been further shaped by fluvial or coastal wave action (mechanical weathering), typical of the Cenozoic era or older formations depending on the local coastline.
Uses & applications
Common pebbles are used as aquarium substrate, decorative landscaping, and occasionally in the construction of terrazzo floors or as aggregate. Large-scale sandstone is used in masonry and architecture.
Geological facts
Sandstone contains a record of the past environment, such as ancient riverbeds or dunes. Some sandstone beach pebbles can contain micro-fossils or mineral inclusions like iron oxides which give them their reddish-brown tint.
Field identification & locations
Identified in the field by its gritty texture (if broken) and visible sand grains. It is often found on high-energy beaches or riverbanks. Collectors value them for 'pocket stones' or rock tumbling due to their durability.
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