
sedimentary
Sandstone
Clastic Sedimentary Rock
AI-generated identification · may be incorrectHardness: 6 to 7 on the Mohs scale (depending on cement type); Color: Tan, brown, yellow, red, grey, pink, white, or black; Luster: Dull to earthy; Crystal structure: Clastic (composed of mineral particles or rock fragments cemented together); Cleavage: None; Specific gravity: 2.2 to 2.8
- Hardness
- 6 to 7 on the Mohs scale (depending on cement type)
- Color
- Tan, brown, yellow, red, grey, pink, white, or black
- Luster
- Dull to earthy
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Physical properties
Hardness: 6 to 7 on the Mohs scale (depending on cement type); Color: Tan, brown, yellow, red, grey, pink, white, or black; Luster: Dull to earthy; Crystal structure: Clastic (composed of mineral particles or rock fragments cemented together); Cleavage: None; Specific gravity: 2.2 to 2.8
Formation & geological history
Formed by the accumulation, compaction, and cementation of mineral particles or rock fragments, chiefly quartz and feldspar, deposited by water, wind, or ice in environments such as deserts, rivers, and beaches over millions of years.
Uses & applications
Commonly used in construction as a building material, paving stone, decorative aggregate, and historically for grindstones and whetstones.
Geological facts
Sandstone formations often display distinct layering called cross-bedding, which records the direction of ancient winds or water currents. Famous monuments worldwide, including Petra in Jordan and parts of the Grand Canyon, are carved into or composed of sandstone.
Field identification & locations
Identified in the field by its granular, sandpaper-like texture and visible sand-sized grains. Found worldwide in sedimentary basins, deserts, and coastal regions.
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