
sedimentary
Sandstone
Arenite (primarily SiO2)
Hardness: 6-7 (on Mohs scale); Color: Tan, brown, or buff; Luster: Dull to earthy; Crystal structure: Clastic (usually quartz grains); Cleavage: None; Specific gravity: 2.2 - 2.8
- Hardness
- 6-7 (on Mohs scale)
- Color
- Tan, brown, or buff
- Luster
- Dull to earthy
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Physical properties
Hardness: 6-7 (on Mohs scale); Color: Tan, brown, or buff; Luster: Dull to earthy; Crystal structure: Clastic (usually quartz grains); Cleavage: None; Specific gravity: 2.2 - 2.8
Formation & geological history
Formed through the accumulation of sand-sized mineral particles or rock fragments held together by a mineral cement (like silica or calcium carbonate) over millions of years. This specimen likely originates from a terrestrial or shallow marine environment.
Uses & applications
Extensively used as a building material, masonry, and road construction aggregate; also used for making grindstones and in glass manufacturing.
Geological facts
Sandstone accounts for roughly 20 to 25 percent of all sedimentary rocks. It is a major reservoir for groundwater and petroleum because of its porosity and permeability.
Field identification & locations
Identify in the field by its gritty 'sandpaper' feel when rubbed and the presence of visible grains. Common in arid desert regions and coastal formations worldwide.
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