
sedimentary
Red Sandstone
Arenite (Ferruginous Sandstone)
AI-generated identification · may be incorrectHardness: 6-7 Mohs; Color: reddish-brown; Luster: dull/earthy; Texture: granular with visible pores; Composition: primarily quartz grains coated with iron oxides (hematite).
- Hardness
- 6-7 Mohs
- Color
- reddish-brown
- Luster
- dull/earthy
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Physical properties
Hardness: 6-7 Mohs; Color: reddish-brown; Luster: dull/earthy; Texture: granular with visible pores; Composition: primarily quartz grains coated with iron oxides (hematite).
Formation & geological history
Formed through the accumulation and cementation of sand-sized mineral grains or rock fragments. The red color suggests deposition in an oxygen-rich terrestrial environment, such as a desert or river floodplain, where iron minerals oxidize.
Uses & applications
Commonly used as a building material, decorative stone in landscaping, and in the manufacturing of glass or for industrial abrasives if high in silica.
Geological facts
The red color is caused by the presence of hematite (iron oxide). Many of the world's most famous natural landscapes, like the Grand Canyon or Sedona, Arizona, are composed of massive layers of red sandstone.
Field identification & locations
Identify by the sandpaper-like feel and the reddish rub-off. Found globally in basins and desert regions. Look for bedding planes or cross-bedding indicating ancient dunes or water currents.
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