
sedimentary
Sandstone
Arenite (primarily Quartz, SiO2)
Hardness: 6-7 (individual grains); Color: Tan, brown, or buff; Luster: Dull or earthy; Crystal structure: Clastic/granular; Cleavage: None; Specific Gravity: 2.2-2.8
- Hardness
- 6-7 (individual grains)
- Color
- Tan, brown, or buff
- Luster
- Dull or earthy
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Physical properties
Hardness: 6-7 (individual grains); Color: Tan, brown, or buff; Luster: Dull or 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. Typically deposited in river, lake, or marine environments over millions of years.
Uses & applications
Used widely as a building material, masonry decoration, road gravel, and as a source of high-purity silica for glass manufacturing.
Geological facts
Sandstone reservoirs are one of the most important sources of ground water and petroleum because of their high porosity and permeability.
Field identification & locations
Identify by a 'gritty' sandpaper feel when rubbed. Found worldwide in sedimentary basins. Collectors often look for specimens with interesting 'Liesegang rings' or fossil inclusions.
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