
sedimentary
Sandstone
Clastic Sedimentary Rock
AI-generated identification · may be incorrectHardness: 6-7 on Mohs scale (depending on cement); Color: Tan, brown, yellow, red, grey, pink, white; Luster: Dull to earthy; Crystal structure: Clastic/granular, composed mostly of quartz and feldspar grains; Cleavage: None
- Hardness
- 6-7 on Mohs scale (depending on cement)
- Color
- Tan, brown, yellow, red, grey, pink, white
- Luster
- Dull to earthy
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Physical properties
Hardness: 6-7 on Mohs scale (depending on cement); Color: Tan, brown, yellow, red, grey, pink, white; Luster: Dull to earthy; Crystal structure: Clastic/granular, composed mostly of quartz and feldspar grains; Cleavage: None
Formation & geological history
Formed by the accumulation, compaction, and cementation of mineral particles or rock fragments, usually sand-sized (0.0625 to 2 mm), predominantly quartz. Forms in environments like deserts, beaches, rivers, and floodplains over millions of years.
Uses & applications
Used extensively in construction as building stone, paving material, and for making glass, concrete, and abrasives.
Geological facts
Sandstone is porous and permeable, making it an excellent natural aquifer that stores and filters groundwater. Famous structures built from sandstone include Petra in Jordan and the White House in Washington, D.C.
Field identification & locations
Easily identified by its gritty, sandpaper-like texture and visible sand grains. Found worldwide in regions with ancient sedimentary basins, deserts, and coastal areas.
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