Rock Identifier
Red Sandstone (Ferruginous Sandstone (SiO2 with Fe2O3)) — sedimentary
sedimentary

Red Sandstone

Ferruginous Sandstone (SiO2 with Fe2O3)

Hardness: 6-7 (Mohs scale), Color: Reddish-brown/Terracotta, Luster: Dull/Earthy, Crystal Structure: Granular/Clastic, Cleavage: None, Specific Gravity: 2.2-2.8

Identified More sedimentary

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Physical properties

Hardness: 6-7 (Mohs scale), Color: Reddish-brown/Terracotta, Luster: Dull/Earthy, Crystal Structure: Granular/Clastic, Cleavage: None, Specific Gravity: 2.2-2.8

Formation & geological history

Formed through the accumulation and cementation of sand-sized grains, typically quartz and feldspar, in desert or river delta environments. The red color suggests deposition in an oxygen-rich environment where iron minerals oxidized into hematite.

Uses & applications

Commonly used as a building material, paving stone, decorative garden rock, and in the production of glass or concrete.

Geological facts

Red sandstone is famous for creating iconic landscapes like the Grand Canyon and the 'Red Rocks' of Sedona. It was one of the most popular building materials for prehistoric structures and 19th-century brownstone buildings.

Field identification & locations

Identify by its gritty sandpaper feel and visible sand grains. Found globally in basins and ancient desert regions. For collectors, look for ripple marks or cross-bedding indicating ancient water or wind flow.