
sedimentary
Sandstone
Arenite (composed primarily of SiO2)
Hardness: 6-7 on Mohs scale; Color: Tan, brown, or earthy yellow (due to iron oxides); Luster: Dull or earthy; Crystal structure: Clastic (grainy texture); Cleavage: None (grains are cemented together); Specific gravity: 2.2-2.8
- Hardness
- 6-7 on Mohs scale
- Color
- Tan, brown, or earthy yellow (due to iron oxides)
- Luster
- Dull or earthy
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Physical properties
Hardness: 6-7 on Mohs scale; Color: Tan, brown, or earthy yellow (due to iron oxides); Luster: Dull or earthy; Crystal structure: Clastic (grainy texture); Cleavage: None (grains are cemented together); Specific gravity: 2.2-2.8
Formation & geological history
Formed through the accumulation and cementation of sand-sized grains (mostly quartz and feldspar) in environments such as river beds, deserts, or marine basins. This sample appears to be from a terrestrial weathering environment.
Uses & applications
Commonly used as a building material, paving stone, and in the production of glass (if high purity quartz). It is also a significant reservoir rock for groundwater and petroleum.
Geological facts
Sandstone makes up about 20-25% of all sedimentary rocks on Earth. The famous red rocks of the Grand Canyon and Petra in Jordan are primarily made of sandstone.
Field identification & locations
Identify in the field by its gritty texture (feels like sandpaper) and visible layering (bedding). It can often be scratched with a steel blade if the cement is weak, but the grains themselves are hard quartz. Found globally in basins and mountainous regions.
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