
sedimentary
Sandstone (Quartzose)
Arenite (primarily SiO2)
Hardness: 6-7 (on Mohs scale if quartz-rich); Color: Tan, beige, or yellowish brown; Luster: Dull/Earthy; Crystal structure: Clastic (grainy texture); Cleavage: None; Specific gravity: 2.2-2.8
- Hardness
- 6-7 (on Mohs scale if quartz-rich)
- Color
- Tan, beige, or yellowish brown
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 (on Mohs scale if quartz-rich); Color: Tan, beige, or yellowish brown; Luster: Dull/Earthy; Crystal structure: Clastic (grainy texture); Cleavage: None; Specific gravity: 2.2-2.8
Formation & geological history
Formed through the accumulation, compaction, and cementation of sand-sized mineral grains or rock fragments. Typically deposited in river beds, beaches, or deserts over millions of years.
Uses & applications
Widely used as an architectural stone, in paving, as a source of silica for glass making, and for grinding tools. It is also a significant reservoir rock for oil, water, and gas.
Geological facts
Sandstone makes up about 20-25% of all sedimentary rocks on Earth. The famous red rock formations in Sedona, Arizona and Petra, Jordan are composed primarily of sandstone containing iron oxide.
Field identification & locations
Identify in the field by its distinctive 'sandpaper' feel. It is commonly found in sedimentary basins and cliff faces. Collectors look for unique banding or fossil inclusions.
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