
sedimentary
Sandstone
Clastic Sedimentary Rock
Hardness: 6 to 7 on the Mohs scale (depending on the cementing material); Color: Tan, brown, yellow, red, grey, pink, white; Luster: Dull to earthy; Crystal structure: Amorphous/clastic grain aggregation (quartz grains); Cleavage: None
- Color
- Tan, brown, yellow, red, grey, pink, white
- Luster
- Dull to earthy
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Physical properties
Hardness: 6 to 7 on the Mohs scale (depending on the cementing material); Color: Tan, brown, yellow, red, grey, pink, white; Luster: Dull to earthy; Crystal structure: Amorphous/clastic grain aggregation (quartz grains); Cleavage: None
Formation & geological history
Formed by the accumulation, compaction, and cementation of mineral particles or rock fragments, chiefly quartz and feldspar, in environments such as beaches, deserts, flood plains, and rivers. Geological age varies widely from Precambrian to Recent.
Uses & applications
Commonly used in construction as building stone, paving material, and in the manufacturing of glass, concrete, and abrasives.
Geological facts
Sandstone is porous and permeable, which makes it an excellent aquifer for storing groundwater and natural oil deposits. Many famous historical monuments, such as Petra in Jordan and parts of the Egyptian temples, are carved directly out of sandstone cliffs.
Field identification & locations
Easily identified by its gritty texture (feeling like fine sandpaper) and visible sand grains or distinct bedding planes. Found worldwide in sedimentary basins, deserts, and coastal regions. For collectors, look for banded varieties or fossil-bearing layers.
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Sandstone or Siltstone
Arenite (if sandstone)
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Quartz pebble
Silicon dioxide (SiO2)
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Fossiliferous Concretion
Septarian Concretion containing Brachiopods/Crinoids
fossil
Generic Pebble / Rock Fragment
Lithic fragment / Weathered rock
sedimentary
Sedimentary Sandstone
Arenite (Sedimentary Rock)
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Banded Siltstone / Mudstone Pebble
Siltstone / Argillite
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