
sedimentary
Sandstone (Quartzose)
Arenite (SiO2 principal)
Hardness: 6-7 on Mohs scale (due to quartz grains); Color: Tan, buff, or light brown; Luster: Dull/Earthy; Crystal structure: Clastic (granular); Cleavage: None; Specific Gravity: 2.2-2.8.
- Hardness
- 6-7 on Mohs scale (due to quartz grains)
- Color
- Tan, buff, or light brown
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 on Mohs scale (due to quartz grains); Color: Tan, buff, or light brown; Luster: Dull/Earthy; Crystal structure: Clastic (granular); Cleavage: None; Specific Gravity: 2.2-2.8.
Formation & geological history
Formed from the accumulation and cementation of sand-sized mineral grains or rock fragments. This specimen appears water-worn, suggesting a fluvial or coastal environment where it was tumbled and rounded over time.
Uses & applications
Commonly used as a building material, in the manufacture of glass (if high purity quartz), and as a reservoir rock for oil and natural gas. Smaller pebbles are used for landscaping.
Geological facts
Sandstone makes up about 20-25% of all sedimentary rocks on Earth. The 'Old Red Sandstone' is a famous geological formation in Britain that helped pioneers of geology understand Earth's history.
Field identification & locations
Identify in the field by its gritty texture (feels like sandpaper) and visible grains. Often found in riverbeds, beaches, and desert outcrops. It often shows bedding layers in larger specimens.
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