
sedimentary
Red Sandstone
Sandstone (lithic arenite or arkose with iron oxide)
AI-generated identification · may be incorrectHardness: 6-7 on Mohs scale; Color: Red, reddish-brown, or orange due to hematite; Luster: Dull/Earthy; Crystal structure: Clastic (grainy); Cleavage: None; Specific gravity: 2.2-2.8
- Hardness
- 6-7 on Mohs scale
- Color
- Red, reddish-brown, or orange due to hematite
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 on Mohs scale; Color: Red, reddish-brown, or orange due to hematite; Luster: Dull/Earthy; Crystal structure: Clastic (grainy); Cleavage: None; Specific gravity: 2.2-2.8
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 environment such as a desert or river floodplain where iron minerals oxidized. Ages range from Precambrian to Recent.
Uses & applications
Used widely as a building material, decorative stone, for paving, and as an abrasive in some industrial processes.
Geological facts
Red sandstone is what gives famous landscapes like the Grand Canyon, Sedona (Arizona), and the Red Rocks of Colorado their distinctive appearance. It is a major reservoir rock for groundwater and petroleum.
Field identification & locations
Identify by its gritty, sandpaper-like texture and visible sand grains. It is commonly found in sedimentary basins and arid regions. Collectors look for interesting ripple marks or cross-bedding patterns.
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