
sedimentary
Sandstone
Clastic Sedimentary Rock
Hardness: 6-7 on Mohs scale (due to quartz grains); Color: Varies widely including tan, brown, yellow, red, grey, pink, and white; Luster: Dull to earthy; Crystal structure: Composed of cemented mineral particles rather than a single crystal structure; Cleavage: None, but tends to fracture along bedding planes;…
- Hardness
- 6-7 on Mohs scale (due to quartz grains)
- Luster
- Dull to earthy
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Physical properties
Hardness: 6-7 on Mohs scale (due to quartz grains); Color: Varies widely including tan, brown, yellow, red, grey, pink, and white; Luster: Dull to earthy; Crystal structure: Composed of cemented mineral particles rather than a single crystal structure; Cleavage: None, but tends to fracture along bedding planes; Specific Gravity: 2.2-2.8
Formation & geological history
Formed from the accumulation, compaction, and cementation of mineral particles or rock fragments, chiefly quartz and feldspar, in environments such as deserts, rivers, lakes, and shallow marine areas over millions of years.
Uses & applications
Widely used in construction, building facades, paving stones, architecture, and historically for grindstones and whetstones.
Geological facts
Sandstone is porous and permeable, making it an excellent natural reservoir for groundwater, oil, and natural gas. Famous monuments like Petra in Jordan and the White House in Washington, D.C., are built from sandstone.
Field identification & locations
Identified in the field by its distinct gritty texture (like sandpaper) and visible sand grains cemented together. Found globally in regions with ancient sedimentary basins, deserts, or coastal formations.
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