
sedimentary
Sandstone (Ferruginous)
Arenite (SiO2 with Fe2O3 inclusions)
AI-generated identification · may be incorrectHardness: 6-7 on Mohs scale; Color: Reddish-brown, tan, or orange due to iron oxide; Luster: Dull to earthy (sparkly surface indicates quartz grains); Crystal Structure: Granular/clastic; Cleavage: None; Specific Gravity: 2.2-2.8
- Hardness
- 6-7 on Mohs scale
- Color
- Reddish-brown, tan, or orange due to iron oxide
- Luster
- Dull to earthy (sparkly surface indicates quartz grains)
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Physical properties
Hardness: 6-7 on Mohs scale; Color: Reddish-brown, tan, or orange due to iron oxide; Luster: Dull to earthy (sparkly surface indicates quartz grains); Crystal Structure: Granular/clastic; Cleavage: None; Specific Gravity: 2.2-2.8
Formation & geological history
Formed through the accumulation and cementation of sand-sized mineral or rock grains. The reddish tint suggests formation in an oxygen-rich terrestrial environment where iron minerals oxidized (rusted) during lithification. Most common in desert or river delta deposits.
Uses & applications
Used widely in construction as a building stone (brownstone), paving material, and as an aquifer for groundwater or a reservoir for oil and gas. Fine specimens are used in landscaping and garden decor.
Geological facts
Sandstone makes up about 20% of all sedimentary rocks on Earth. The famous red rock formations in Sedona, Arizona and the 'wave' in Utah are composed of this type of ferruginous sandstone.
Field identification & locations
Identify by its gritty, sandpaper-like feel and visible grains. It can be found globally in sedimentary basins. Collectors should look for unique layering (cross-bedding) or fossil inclusions.
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Sedimentary Sandstone
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