
sedimentary
Sandstone (Ferruginous)
Arenite (Fe-rich SiO2)
AI-generated identification · may be incorrectHardness: 6-7 (Mohs); Color: Tan, yellow-orange, or brown with red oxidation; Luster: Dull/Earthy; Crystal structure: Clastic (grainy); Cleavage: None; Specific gravity: 2.2-2.8
- Hardness
- 6-7 (Mohs)
- Color
- Tan, yellow-orange, or brown with red oxidation
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 (Mohs); Color: Tan, yellow-orange, or brown with red oxidation; Luster: Dull/Earthy; Crystal structure: Clastic (grainy); Cleavage: None; Specific gravity: 2.2-2.8
Formation & geological history
Formed through the accumulation and cementation of sand-sized mineral grains or rock fragments. The orange/red coloring indicates the presence of iron oxide (hematite or limonite) that precipitated between the grains as a natural cement.
Uses & applications
Used primarily in building construction as a paving or tile material. Highly weather-resistant specimens are used for monuments and landscaping.
Geological facts
Sandstone is one of the most common sedimentary rocks on Earth. This specific specimen appears to be a stream-rounded cobble, meaning its smooth surface was shaped by water transport over a long period.
Field identification & locations
Identify by its gritty, abrasive feel (like sandpaper). It is commonly found in riverbeds, canyons, and coastal areas. Look for visible sand grains and layering (bedding planes).
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Sandstone or Siltstone
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