
sedimentary
Red Sandstone
Sandstone with Hematite cement
AI-generated identification · may be incorrectHardness: 6-7 (quartz sand grains); Color: Red/rust due to iron oxide; Luster: Earthy to dull; Texture: Clastic, gritty feel.
- Hardness
- 6-7 (quartz sand grains)
- Color
- Red/rust due to iron oxide
- Luster
- Earthy to dull
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Physical properties
Hardness: 6-7 (quartz sand grains); Color: Red/rust due to iron oxide; Luster: Earthy to dull; Texture: Clastic, gritty feel.
Formation & geological history
Formed by the accumulation and lithification of sand-sized grains, typically in ancient desert, river, or coastal environments. The red color comes from iron oxide (hematite) cementing the grains together over millions of years.
Uses & applications
Commonly used in construction as a building material, dimension stone, and for decorative landscaping.
Geological facts
Red sandstone was widely used in ancient architecture, including iconic structures like Petra in Jordan and many castles and cathedrals in Europe and India.
Field identification & locations
Identified by its gritty feel (like sandpaper) and distinct red color. Commonly found worldwide in sedimentary basins. A simple streak test on unglazed porcelain will often leave a reddish-brown streak due to the hematite.
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