
sedimentary
Sandstone (Quartzose)
Arenite (primarily SiO2)
AI-generated identification · may be incorrectHardness: 6-7 on Mohs scale; Color: Tan, beige, light gray; Luster: Dull/Earthy; Crystal Structure: Clastic (granular texture); Cleavage: None; Specific Gravity: 2.2-2.8
- Hardness
- 6-7 on Mohs scale
- Color
- Tan, beige, light gray
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 on Mohs scale; Color: Tan, beige, light gray; Luster: Dull/Earthy; Crystal Structure: Clastic (granular texture); Cleavage: None; Specific Gravity: 2.2-2.8
Formation & geological history
Formed through the accumulation and cementation of mineral particles or rock fragments (detritus), usually quartz or feldspar, over millions of years in environments like riverbeds, deserts, or shorelines.
Uses & applications
Commonly used as a building material, in the manufacture of glass, as a reservoir for oil and water, and as a decorative stone in landscaping.
Geological facts
Sandstone makes up about 20% of all sedimentary rocks on Earth. It is many-layered and frequently contains fossils of prehistoric life trapped within its strata.
Field identification & locations
Identify by its gritty, sandpaper-like feel and visible grains of sand. In the field, look for distinct bedding layers. It is found globally in sedimentary basins.
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Sandstone or Siltstone
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