
sedimentary
Red Sandstone
Quartz Arenite (iron-stained) / Quartzite precursor
Hardness: 6-7 on Mohs scale. Color: reddish-brown to brick red due to iron oxide (hematite) cementation. Luster: dull, earthy, or granular. Texture: clastic, medium to fine-grained sandy texture with visible quartz grains.
- Hardness
- 6-7 on Mohs scale
- Luster
- dull, earthy, or granular
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Physical properties
Hardness: 6-7 on Mohs scale. Color: reddish-brown to brick red due to iron oxide (hematite) cementation. Luster: dull, earthy, or granular. Texture: clastic, medium to fine-grained sandy texture with visible quartz grains.
Formation & geological history
Formed through the deposition, compaction, and cementation of sand-sized quartz grains in terrestrial, aeolian (desert sand dunes), or fluvial (river bed) environments. The red coloration is due to small amounts of hematite or iron oxide coating the quartz grains during diagenesis.
Uses & applications
Widely used as a construction stone, paving material, architectural face-stone, land-scaping accent, and aggregate.
Geological facts
Red sandstone formations comprise some of the most dramatic landscapes on Earth, including the American Southwest (e.g., Zion National Park, Sedona) and Old Red Sandstone deposits in Europe.
Field identification & locations
Identified in the field by its distinct gritty sandpaper-like feel, fine-to-medium quartz grain structure, and dark red to brownish-red color. Highly abundant globally, especially in desert or ancient riverbed deposits.
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