
sedimentary
Sandstone
Clastic Sedimentary Rock
Hardness: 6 to 7 on the Mohs scale (depending on the cement); Color: Tan, brown, yellow, red, grey, pink, white, or black; Luster: Dull or earthy; Crystal Structure: Amorphous/granular (composed of mineral grains); Cleavage: None
- Hardness
- 6 to 7 on the Mohs scale (depending on the cement)
- Color
- Tan, brown, yellow, red, grey, pink, white, or black
- Luster
- Dull or earthy
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Physical properties
Hardness: 6 to 7 on the Mohs scale (depending on the cement); Color: Tan, brown, yellow, red, grey, pink, white, or black; Luster: Dull or earthy; Crystal Structure: Amorphous/granular (composed of mineral grains); Cleavage: None
Formation & geological history
Formed by the accumulation, compaction, and cementation of mineral particles or rock fragments, usually composed mostly of quartz and feldspar, deposited in environments such as deserts, rivers, and beaches over millions of years.
Uses & applications
Commonly used in construction, building facades, paving, flooring, and historically for grinding stones and whetstones.
Geological facts
Sandstone can absorb water and acts as a natural aquifer, storing significant amounts of groundwater. Many famous historical monuments, such as Petra in Jordan and the temples of Angkor Wat, are carved directly out of sandstone formations.
Field identification & locations
Identified in the field by its distinct gritty texture, similar to coarse sandpaper, and visible sand-sized grains. Found worldwide in sedimentary basins, deserts, and ancient riverbeds.
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