
sedimentary
Sandstone (Water-worn)
Arenite
AI-generated identification · may be incorrectHardness: 6-7 Mohs; Color: Tan, beige, or grey with visible bedding planes; Luster: Dull/Earthy; Crystal structure: Clastic (sand-sized grains); Cleavage: None (distinct bedding instead); Specific gravity: 2.2-2.8
- Hardness
- 6-7 Mohs
- Color
- Tan, beige, or grey with visible bedding planes
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 Mohs; Color: Tan, beige, or grey with visible bedding planes; Luster: Dull/Earthy; Crystal structure: Clastic (sand-sized grains); Cleavage: None (distinct bedding instead); Specific gravity: 2.2-2.8
Formation & geological history
Formed through the accumulation and cementation of mineral particles or rock fragments (detritus). This specific specimen shows river or beach wear, rounding the edges through aqueous erosion. Usually formed in fluvial or marine environments.
Uses & applications
Primary uses include building stone and paving materials. Fine-grained samples are sometimes used for whetstones or grindstones.
Geological facts
Sandstone is one of the most common sedimentary rocks on Earth. This specific sample displays 'bedding'—distinct layers that were originally horizontal deposits of sediment.
Field identification & locations
Identify by its gritty texture (feels like sandpaper) and visible layering (stratification). Found globally in riverbanks, deserts, and coastal cliffs. Collectors should look for unique weathering patterns.
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