
sedimentary
Sandstone
Arenite (primarily SiO2)
Hardness: 6-7 (Mohs scale); Color: Tan, yellow, or buff (due to iron oxides); Luster: Dull/Earthy; Crystal structure: Clastic (grainy texture); Cleavage: None; Specific gravity: 2.2-2.8
- Hardness
- 6-7 (Mohs scale)
- Color
- Tan, yellow, or buff (due to iron oxides)
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 (Mohs scale); Color: Tan, yellow, or buff (due to iron oxides); Luster: Dull/Earthy; Crystal structure: Clastic (grainy texture); Cleavage: None; Specific gravity: 2.2-2.8
Formation & geological history
Formed through the accumulation and cementation of sand-sized mineral grains or rock fragments. Typically deposited in riverbeds, deserts, or beaches over millions of years (geological age varies from Precambrian to Holocene).
Uses & applications
Commonly used as a building material, paving stone, and in the production of glass. It is also an important reservoir rock for groundwater and petroleum.
Geological facts
Sandstone makes up about 20-25% of all sedimentary rocks on Earth. Famous formations include the Antelope Canyon in Arizona and the red sandstone of Petra, Jordan.
Field identification & locations
Identify in the field by its 'gritty' feel (like sandpaper) and visible sand grains. It is ubiquitous in sedimentary basins worldwide. Collectors look for unique banding patterns (Liesegang rings).
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