
sedimentary
Sandstone (Pebble)
Arenite (primarily SiO2)
Hardness: 6-7 Mohs; Color: Greyish-tan with white mineral clasts; Luster: Dull/Earthy; Structure: Fine-grained clastic texture; Cleavage: None (conchoidal fracture on fresh surfaces).
- Hardness
- 6-7 Mohs
- Color
- Greyish-tan with white mineral clasts
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 Mohs; Color: Greyish-tan with white mineral clasts; Luster: Dull/Earthy; Structure: Fine-grained clastic texture; Cleavage: None (conchoidal fracture on fresh surfaces).
Formation & geological history
Formed through the accumulation and cementation of sand-sized mineral grains or rock fragments, typically in riverbeds, beaches, or deserts. High degree of rounding indicates significant transport by water.
Uses & applications
Used in construction, as a landscaping material, and as an abrasive in industrial processes. Polished river stones are used for decorative flooring and massage therapy.
Geological facts
Sandstone makes up about 20% of all sedimentary rocks on Earth. This specific specimen is a 'river rock' or 'cobble' that has been naturally tumbled and smoothed by hydraulic action over thousands of years.
Field identification & locations
Identify in the field by its gritty texture (feels like sandpaper) and visible grains. Commonly found in alluvial deposits, stream beds, and near coastal areas.
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