
sedimentary
Red Sandstone
Sedimentary Quartz Arenite / Arkose
Hardness: 6-7 on Mohs scale (due to quartz grains); Color: Red, reddish-brown, pinkish (derived from iron oxide cements); Luster: Dull to earthy; Crystal structure: Clastic texture composed of sand-sized mineral particles or rock fragments; Cleavage: None (fractures around grains); Specific Gravity: 2.2-2.8
- Hardness
- 6-7 on Mohs scale (due to quartz grains)
- Luster
- Dull to earthy
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Physical properties
Hardness: 6-7 on Mohs scale (due to quartz grains); Color: Red, reddish-brown, pinkish (derived from iron oxide cements); Luster: Dull to earthy; Crystal structure: Clastic texture composed of sand-sized mineral particles or rock fragments; Cleavage: None (fractures around grains); Specific Gravity: 2.2-2.8
Formation & geological history
Formed from the accumulation, compaction, and cementation of mineral particles or rock fragments, typically in desert, river, or beach environments over millions of years.
Uses & applications
Used extensively in construction as a building and paving stone, decorative landscaping, and historically for monuments and sculptures.
Geological facts
The characteristic red color of many sandstones comes from iron oxide (hematite) acting as a cement between the sand grains. Famous geological formations like the American Southwest's desert monuments are carved from massive sandstone layers.
Field identification & locations
Easily identified by its gritty, sandpaper-like texture and visible sand grains. Commonly found worldwide in sedimentary basins, riverbeds, and arid regions.
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