
sedimentary
Sandstone (Quartzose)
Arenite (primarily SiO2)
AI-generated identification · may be incorrectHardness: 6-7 (mohs); Color: Tan, beige, or light brown; Luster: Dull or earthy; Crystal structure: Granular/Clastic; Cleavage: None; Specific gravity: 2.2-2.8
- Hardness
- 6-7 (mohs)
- Color
- Tan, beige, or light brown
- Luster
- Dull or earthy
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Physical properties
Hardness: 6-7 (mohs); Color: Tan, beige, or light brown; Luster: Dull or earthy; Crystal structure: Granular/Clastic; Cleavage: None; Specific gravity: 2.2-2.8
Formation & geological history
Formed through the accumulation and cementation of sand-sized mineral grains or rock fragments (clasts). Typically forms in desert, river, or coastal environments over millions of years through lithification.
Uses & applications
Commonly used in construction as a building material and decorative stone, in the glass-making industry, and as a reservoir rock for oil and natural gas.
Geological facts
Sandstone accounts for roughly 20-25 percent of all sedimentary rocks on Earth. The famous red rocks of the Grand Canyon are primarily composed of various sandstone layers.
Field identification & locations
Identify by its gritty texture (feels like sandpaper) and visible grains. It is extremely common worldwide in sedimentary basins and outcropping cliffs.
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Fossil-bearing concretion, possibly containing a fossil shell or other organic inclusion
Calcareous concretion; exact fossil and host-rock composition are not identifiable from the image
fossil
Fossiliferous Sedimentary Rock
Sedimentary limestone with invertebrate fossil imprint
fossil
Sandstone or Siltstone
Arenite (if sandstone)
Sedimentary
Sandstone
Arenite
sedimentary
Shale
Shale (clastic sedimentary rock)
sedimentary
Shale (or Mudstone/Siltstone)
Sedimentary Mudrock (SiO2, Al2O3 base with clay minerals)
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