
sedimentary
Sandstone
Arenite (primarily SiO2)
Hardness: 6-7 (on Mohs scale); Color: Tan, brown, or reddish-brown due to iron oxide; Luster: Dull or earthy; Crystal Structure: Clastic texture with granular grains; Cleavage: None (breaks across grains); Specific Gravity: 2.2-2.8
- Hardness
- 6-7 (on Mohs scale)
- Color
- Tan, brown, or reddish-brown due to iron oxide
- Luster
- Dull or earthy
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Physical properties
Hardness: 6-7 (on Mohs scale); Color: Tan, brown, or reddish-brown due to iron oxide; Luster: Dull or earthy; Crystal Structure: Clastic texture with granular grains; Cleavage: None (breaks across grains); Specific Gravity: 2.2-2.8
Formation & geological history
Formed from the accumulation and cementation of mineral particles or rock fragments (sand). Usually occurs in desert dunes, riverbeds, or beaches. It can range in age from Precambrian to recent times.
Uses & applications
Extensively used in construction as a building stone, for paving, and in the manufacture of glass. Smaller decorative pieces are used in landscaping and aquariums.
Geological facts
Sandstone makes up about 20% of all sedimentary rocks on Earth. Famous landmarks like the Treasury at Petra and the Grand Canyon are primarily composed of various sandstone layers.
Field identification & locations
Identify in the field by its gritty, sand-paper-like feel and visible grains. Often found in layered outcroppings or as rounded river cobbles. Look for bedding planes or cross-bedding structures.
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