
sedimentary
Sandstone (Pebble)
Arenite (primarily SiO2)
Hardness: 6-7 (Mohs); Color: Tan, beige, grey; Luster: Dull/Earthy; Crystal structure: Clastic (composed of mineral grains); Cleavage: None; Grains are medium-sized and sandy to the touch.
- Hardness
- 6-7 (Mohs)
- Color
- Tan, beige, grey
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 (Mohs); Color: Tan, beige, grey; Luster: Dull/Earthy; Crystal structure: Clastic (composed of mineral grains); Cleavage: None; Grains are medium-sized and sandy to the touch.
Formation & geological history
Formed through the accumulation and cementation of sand-sized mineral grains, typically quartz. This rounded shape indicates high-energy transport in water, such as a riverbed or coastal environment.
Uses & applications
Commonly used as construction aggregate, decorative landscaping stone, and occasionally for sharpening tools in its rough form.
Geological facts
Sandstone acts as a natural aquifer, holding large amounts of water or oil in the pore spaces between sand grains. The rounded 'egg' shape is a result of millions of collisions during transport.
Field identification & locations
Common in the Pyrenees region (near 43.3°N, 1.2°E), where diverse sedimentary deposits from the Cenozoic and Mesozoic are found. Identify by its sandpaper-like texture and visible sand grains.
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