
sedimentary
Sandstone (Quartzose)
Arenite (primarily SiO2)
Hardness: 6-7 (individual grains); Color: Tan, beige, grey; Luster: Dull/Earthy; Crystal structure: Granular/Clastic; Cleavage: None; Specific Gravity: 2.2-2.8
- Hardness
- 6-7 (individual grains)
- Color
- Tan, beige, grey
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 (individual grains); Color: Tan, beige, grey; Luster: Dull/Earthy; Crystal structure: Granular/Clastic; 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 (0.06 to 2 mm diameter) in environments such as deserts, river beds, or beaches. It is lithified by minerals like silica or calcium carbonate over millions of years.
Uses & applications
Widely used as a construction material (dimension stone), in the manufacture of glass, for road base, and as decorative landscaping stone. It is also an important reservoir rock for oil, gas, and groundwater.
Geological facts
Sandstone accounts for approximately 20% of all sedimentary rocks on Earth. Familiar landmarks like the Grand Canyon exhibit massive layers of sandstone that represent ancient environments spanning hundreds of millions of years.
Field identification & locations
Identify it by its gritty, sandpaper-like feel. It can be found globally in outcrop areas, old riverbeds, and coastal regions. Collectors should look for unique cross-bedding patterns or fossil inclusions.
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