
sedimentary
Sandstone (with Iron Staining)
Clastic Sedimentary Rock (primarily Quartz with Limonite/Goethite staining)
Hardness: 6-7 (individual grains); Color: Tan to yellowish-orange; Luster: Dull/Earthy; Crystal structure: Granular/Clastic; Cleavage: None; Specific Gravity: 2.2-2.8
- Hardness
- 6-7 (individual grains)
- Color
- Tan to yellowish-orange
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 (individual grains); Color: Tan to yellowish-orange; Luster: Dull/Earthy; Crystal structure: Granular/Clastic; Cleavage: None; Specific Gravity: 2.2-2.8
Formation & geological history
Formed from the accumulation and cementation of sand-sized mineral particles or rock fragments. The orange-brown color is due to iron oxide staining (rust) from groundwater infiltration, common in terrestrial and near-shore environments over millions of years.
Uses & applications
Used primarily as a construction material, for road base, or as an ornamental stone in landscaping and aquariums.
Geological facts
Sandstone accounts for approximately 10% to 25% of the earth's sedimentary rock. The distinct bands of color, often called 'Liesegang rings,' are caused by the precipitation of chemicals from saturated fluids moving through the rock.
Field identification & locations
Identify by its gritty, sandpaper-like texture and visible sand grains. It is extremely common in desert environments and riverbeds worldwide. Collectors look for unique banding patterns.
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