
sedimentary
Sandstone (likely Arkosic or Lithic)
Clastic Sedimentary Rock (composed mostly of SiO2)
AI-generated identification · may be incorrectHardness: 6-7 on Mohs scale (grains) but can crumble; Color: Tan, beige, or grey with dark mineral inclusions; Luster: Dull/Earthy; Crystal structure: Clastic/Granular texture; Cleavage: None; Specific Gravity: 2.2 - 2.8
- Hardness
- 6-7 on Mohs scale (grains) but can crumble
- Color
- Tan, beige, or grey with dark mineral inclusions
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 on Mohs scale (grains) but can crumble; Color: Tan, beige, or grey with dark mineral inclusions; Luster: Dull/Earthy; Crystal structure: Clastic/Granular texture; 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. These typically form in river beds, beaches, or deserts where sediment is buried and pressurized over millions of years.
Uses & applications
Commonly used as a construction material (building stone), in road pavement, as a reservoir rock for oil and gas, and as a source of silica for glass making.
Geological facts
Sandstone is one of the most common sedimentary rocks on Earth. The famous red rocks of the Grand Canyon and the ancient city of Petra are primarily composed of sandstone.
Field identification & locations
Identify by its gritty, sandpaper-like feel and visible grains. Found globally in basins and coastal areas. Collectors look for unique banding (Liesegang rings) or fossils within the layers.
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