
sedimentary
Sandstone (Ferruginous)
Arenite with Iron Oxide cement (SiO2 + Fe2O3)
Hardness: 6-7 (individual grains), 4-5 (matrix); Color: Tanish-brown to reddish-brown; Luster: Dull/Earthy; Crystal structure: Granular/Clastic; Cleavage: None; Specific Gravity: 2.2-2.8
- Hardness
- 6-7 (individual grains), 4-5 (matrix)
- Color
- Tanish-brown to reddish-brown
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 (individual grains), 4-5 (matrix); Color: Tanish-brown to reddish-brown; Luster: Dull/Earthy; Crystal structure: Granular/Clastic; Cleavage: None; Specific Gravity: 2.2-2.8
Formation & geological history
Formed through the accumulation and litification of sand-sized mineral grains or rock fragments, typically in desert, river, or coastal environments. Reddish hues indicate oxidation of iron minerals during burial.
Uses & applications
Commonly used as a building material, for paving stones, grindstones, and as a reservoir rock for oil, gas, and groundwater. Ferruginous varieties are rarely used for jewelry but are popular in landscaping.
Geological facts
Sandstone accounts for approximately 20-25% of all sedimentary rock on Earth. Famous landmarks like the Grand Canyon and Petra are primarily composed of various sandstone formations.
Field identification & locations
Identify by a gritty 'sandpaper' feel when rubbed. It often shows layering (bedding). This specific specimen appears to be a weathered, iron-rich terrestrial fragment.
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