
sedimentary
Sandstone (Ferruginous)
Arenite (Fe2O3 enriched)
Hardness: 6-7 (Mohs); Color: Brown, tan, or reddish-brown due to iron oxide; Luster: Dull/Earthy; Crystal structure: Clastic (sand-sized grains); Cleavage: None; SG: 2.2-2.8
- Hardness
- 6-7 (Mohs)
- Color
- Brown, tan, or reddish-brown due to iron oxide
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 (Mohs); Color: Brown, tan, or reddish-brown due to iron oxide; Luster: Dull/Earthy; Crystal structure: Clastic (sand-sized grains); Cleavage: None; SG: 2.2-2.8
Formation & geological history
Formed through the accumulation and cementation of mineral particles or rock fragments (sand) in various environments like deserts, river beds, or beaches. Geological ages vary from Precambrian to Cenozoic.
Uses & applications
Used primarily in construction for building stone, paving, and road aggregate. Finely ground sandstone is sometimes used in glassmaking if silica content is high.
Geological facts
Sandstone makes up about 20-25% of all sedimentary rocks on Earth. The famous red rock formations in Sedona, Arizona and the Grand Canyon are primarily composed of ferruginous sandstone layers.
Field identification & locations
Identify by its gritty, sandpaper-like feel and visible grains. It can be found globally in outcrop formations and sedimentary basins. Collectors value specimens with unique weathering patterns or fossil inclusions.
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