
sedimentary
Sandstone
Arenite (SiO2 primarily)
Hardness: 6-7 on Mohs scale (grains) but can crumble easily; Color: Brown, tan, reddish; Luster: Dull, earthy; Crystal structure: Clastic (grainy texture); Cleavage: None; Specific gravity: 2.2-2.8
- Hardness
- 6-7 on Mohs scale (grains) but can crumble easily
- Color
- Brown, tan, reddish
- Luster
- Dull, earthy
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Physical properties
Hardness: 6-7 on Mohs scale (grains) but can crumble easily; Color: Brown, tan, reddish; Luster: Dull, earthy; Crystal structure: Clastic (grainy texture); Cleavage: None; Specific gravity: 2.2-2.8
Formation & geological history
Formed from the accumulation and cementation of sand-sized mineral grains or rock fragments, typically through wind or water action in environments like deserts, river beds, or beaches.
Uses & applications
Extensively used in construction, paving, as a decorative stone, and historically as a material for grindstones and sculpture.
Geological facts
Sandstone can act as an important reservoir for groundwater and oil because it is often porous and permeable. Some of the world's most famous rock formations, like those in the Grand Canyon, are primarily sandstone layers.
Field identification & locations
Identify in the field by its sandpaper-like feel and visible grains. It is extremely common worldwide in sedimentary basins. Collectors often look for colorful banding or fossil inclusions.
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Other sedimentary specimens
Sandstone or Siltstone
Arenite (if sandstone)
Sedimentary
Fossiliferous Concretion
Septarian Concretion containing Brachiopods/Crinoids
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Shale
Shale (clastic sedimentary rock)
sedimentary
Brown Sandstone (River Rock)
Arenite
sedimentary
Cone-in-cone structure (Limestone)
Cone-in-cone structure (Secondary Sedimentary Structure)
sedimentary
Shale
Argillaceous sedimentary rock
sedimentary