
sedimentary
Sandstone
Sandstone (Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 6-7 Mohs; Color: Tan, beige, or grey with grainy texture; Luster: Dull/Earthy; Crystal structure: Clastic/Granular; Cleavage: None; Specific Gravity: 2.2-2.8
- Hardness
- 6-7 Mohs
- Color
- Tan, beige, or grey with grainy texture
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 Mohs; Color: Tan, beige, or grey with grainy texture; Luster: Dull/Earthy; Crystal structure: Clastic/Granular; 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. Most sandstone is composed of quartz or feldspar. It can range in age from Precambrian to recent.
Uses & applications
Extensively used in construction for paving, building stone, and tiles; also used as a reservoir rock for oil and water, and in glass manufacturing if high in quartz content.
Geological facts
Sandstone represents about 20-25% of all sedimentary rocks on Earth. Familiar landmarks like the Grand Canyon and the Nabataean city of Petra are carved from sandstone.
Field identification & locations
Identified by its sandpaper-like feel and visible grains. Often found in riverbeds, beaches, and desert environments. Collectors look for unique banding patterns known as Liesegang rings.
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