
sedimentary
Sandstone (Micaceous/Feldspathic variant)
Arenite (specifically subarkose or lithic arenite)
Hardness: 6-7 (Mohs scale); Color: Tan, beige, or buff; Luster: Dull to earthy; Structure: Granular/Clastic texture with visible sand-sized grains; Cleavage: None (fractures across grains); Specific Gravity: 2.2-2.8
- Hardness
- 6-7 (Mohs scale)
- Color
- Tan, beige, or buff
- Luster
- Dull to earthy
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Physical properties
Hardness: 6-7 (Mohs scale); Color: Tan, beige, or buff; Luster: Dull to earthy; Structure: Granular/Clastic texture with visible sand-sized grains; Cleavage: None (fractures across grains); Specific Gravity: 2.2-2.8
Formation & geological history
Formed via the accumulation and lithification of sand-sized mineral particles or rock fragments. This specimen likely formed in a high-energy environment such as a river bed, beach, or desert dune during various geological periods from the Precambrian to Holocene.
Uses & applications
Widely used as a construction material (dimension stone), in the manufacture of glass (if high silica), and as a reservoir rock for oil and natural gas. Fine-grained versions are used for grindstones.
Geological facts
Sandstone represents about 20-25% of all sedimentary rocks on Earth. The famous red rocks of the Grand Canyon and the Nabataean city of Petra are primarily composed of various layers of sandstone.
Field identification & locations
Identify by the 'sandpaper' feel of the surface. It will often show bedding planes or cross-bedding. Common in basins and coastal regions; collectors look for specimens with unique ripple marks or trace fossils.
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