
sedimentary
Sandstone (Ferruginous)
Arenite with Iron-Oxide Cement
AI-generated identification · may be incorrectHardness: 6-7 (on Mohs scale); Color: Tan, orange, reddish-brown (indicated by iron oxidation); Luster: Dull/Earthy; Crystal structure: Clastic (composed of sand-sized mineral grains); Cleavage: None; Specific Gravity: 2.2-2.8
- Hardness
- 6-7 (on Mohs scale)
- Color
- Tan, orange, reddish-brown (indicated by iron oxidation)
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 (on Mohs scale); Color: Tan, orange, reddish-brown (indicated by iron oxidation); Luster: Dull/Earthy; Crystal structure: Clastic (composed of sand-sized mineral grains); Cleavage: None; Specific Gravity: 2.2-2.8
Formation & geological history
Formed through the accumulation and cementation of mineral particles or rock fragments (clasts). The orange-red hue suggests deposition in a terrestrial or oxidizing environment, likely from the Paleozoic or Mesozoic eras.
Uses & applications
Commonly used in construction for building stone, paving, and decorative landscaping. High-quality sandstones are used for glass manufacturing and water filtration systems.
Geological facts
Sandstone makes up about 20% of all sedimentary rocks on Earth. The famous red rock formations of the American Southwest, such as those in the Grand Canyon and Zion National Park, are primarily ferruginous sandstone.
Field identification & locations
Identify by its 'gritty' feel, similar to sandpaper, and visible grain layers. Often found in desert environments, riverbeds, and ancient marine basins. Collectors should look for unique cross-bedding or fossil inclusions.
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