
sedimentary
Sandstone
Arenite (clastic sedimentary rock)
Hardness: 6-7 (individual grains); Color: tan, buff, beige with reddish speckles; Luster: dull to earthy; Texture: clastic/granular (sand-sized grains); Cleavage: none.
- Hardness
- 6-7 (individual grains)
- Color
- tan, buff, beige with reddish speckles
- Luster
- dull to earthy
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Physical properties
Hardness: 6-7 (individual grains); Color: tan, buff, beige with reddish speckles; Luster: dull to earthy; Texture: clastic/granular (sand-sized grains); Cleavage: none.
Formation & geological history
Formed from the accumulation and cementation of sand-sized mineral grains or rock fragments, typically through lithification in river beds, deserts, or marine environments. Some specimens date back hundreds of millions of years.
Uses & applications
Widely used as a building material, road base, for making grindstones, and as a reservoir rock for oil and natural gas.
Geological facts
Sandstone represents about 20% of all sedimentary rocks on Earth. The red and gold colors often seen are due to iron oxide (hematite) or limonite impurities.
Field identification & locations
Identify by its gritty feel (like sandpaper) and visible grains. Found globally in canyon walls, plateaus, and coastal cliffs. Collectors look for specific patterns like cross-bedding.
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Cone-in-cone structure (Secondary Sedimentary Structure)
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Sandstone Grain
Clastic Sedimentary Rock Grain (SiO2 dominated)
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Brecciated Chert (Microcrystalline Silica)
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Shale or Slaty Mudstone
Argillaceous sedimentary rock
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Sandstone
Arenite (primarily SiO2)
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