
sedimentary
Sandstone
Arenite (primarily SiO2)
AI-generated identification · may be incorrectHardness: 6-7 (Mohs); Color: Tan, brown, or grayish-yellow; Luster: Dull or earthy; Crystal structure: Granular/Clastic; Cleavage: None; Specific Gravity: 2.2-2.8
- Hardness
- 6-7 (Mohs)
- Color
- Tan, brown, or grayish-yellow
- Luster
- Dull or earthy
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Physical properties
Hardness: 6-7 (Mohs); Color: Tan, brown, or grayish-yellow; 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 mineral particles or rock fragments (sand-sized). Most sandstones are composed of quartz or feldspar. They form in environments like beaches, deserts, and floodplains.
Uses & applications
Commonly used in construction as a building material and decorative stone, for making grindstones, and as a source for glass silicon.
Geological facts
Sandstone makes up about 20% to 25% of all sedimentary rocks on Earth. The famous red rocks of the Grand Canyon and Petra in Jordan are both made of sandstone layers.
Field identification & locations
Identified by its 'sandpaper' feel and visible grains. Often displays bedding layers. Commonly found in river basins, coastal cliffs, and arid regions. Collectors look for unique banding patterns (wonderstone).
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Other sedimentary specimens
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)
sedimentary