
sedimentary
Sandstone
Quartz Arenite / Sedimentary Rock
AI-generated identification · may be incorrectHardness: 6-7 on Mohs scale (due to quartz grains); Color: Reddish-brown, tan, gray, or white; Luster: Dull to vitreous on individual quartz crystals; Structure: Clastic, granular texture composed mainly of sand-sized mineral particles or rock fragments; Cleavage: None (fractures around grains)
- Hardness
- 6-7 on Mohs scale (due to quartz grains)
- Color
- Reddish-brown, tan, gray, or white
- Luster
- Dull to vitreous on individual quartz crystals
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Physical properties
Hardness: 6-7 on Mohs scale (due to quartz grains); Color: Reddish-brown, tan, gray, or white; Luster: Dull to vitreous on individual quartz crystals; Structure: Clastic, granular texture composed mainly of sand-sized mineral particles or rock fragments; Cleavage: None (fractures around grains)
Formation & geological history
Formed by the accumulation, compaction, and cementation of mineral particles or rock fragments (predominantly quartz) in environments such as deserts, rivers, and beaches, often over millions of years during the Paleozoic or Mesozoic eras.
Uses & applications
Commonly used in construction as building stone, paving material, flagstone, and historically for grinding stones and sharpening whetstones.
Geological facts
Famous structures built from sandstone include Petra in Jordan and Uluru (Ayers Rock) in Australia. Its porous nature often makes it an excellent aquifer for groundwater storage.
Field identification & locations
Easily identified by its gritty, sandpaper-like texture and visible sand grains. Found worldwide in sedimentary basins, river valleys, and desert regions. Collectors look for unique banding or fossil inclusions.
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