
sedimentary
Sandstone (Quartz-rich)
Arenite (SiO2)
Hardness: 6-7 on Mohs scale; Color: Tan, brown, or reddish-brown; Luster: Dull/Earthy; Crystal Structure: Clastic (sand grains); Cleavage: None (conchoidal fracture within grains); Specific Gravity: 2.2–2.8
- Hardness
- 6-7 on Mohs scale
- Color
- Tan, brown, or reddish-brown
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 on Mohs scale; Color: Tan, brown, or reddish-brown; Luster: Dull/Earthy; Crystal Structure: Clastic (sand grains); Cleavage: None (conchoidal fracture within grains); 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 riverbeds, deserts, or coastal environments over millions of years (clastic sedimentation).
Uses & applications
Used extensively in construction as a building material, paving, and decorative stone. Also used for grindstones and in the manufacturing of glass when high in quartz purity.
Geological facts
Sandstone acts as a natural aquifer, holding vast amounts of groundwater or petroleum in its pore spaces. The famous city of Petra is carved entirely out of sandstone.
Field identification & locations
Identify by its gritty, sandpaper-like texture and visible sedimentary layers (bedding). It is extremely common worldwide in sedimentary basins and exposed cliff faces.
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