
sedimentary
Sandstone
Arenite (SiO2 based)
AI-generated identification · may be incorrectHardness: 6-7 (Mohs); Color: Tan, yellowish-brown, buff; Luster: Dull, earthy; Texture: Granular, feels like sandpaper; Crystal Structure: Clastic grains; Specific Gravity: 2.2-2.8
- Hardness
- 6-7 (Mohs)
- Color
- Tan, yellowish-brown, buff
- Luster
- Dull, earthy
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Physical properties
Hardness: 6-7 (Mohs); Color: Tan, yellowish-brown, buff; Luster: Dull, earthy; Texture: Granular, feels like sandpaper; Crystal Structure: Clastic grains; Specific Gravity: 2.2-2.8
Formation & geological history
Formed through the accumulation and cementation of sand-sized grains (mostly quartz and feldspar). These deposits occur in deserts, riverbeds, and coastal environments where compaction and mineral precipitation (like silica or calcium carbonate) bind the grains over millions of years.
Uses & applications
Extensively used as a building material, paving stone, and decorative landscaping rock. High-purity sandstones are used in glass manufacturing and as industrial abrasives.
Geological facts
Sandstone is one of the most common sedimentary rocks on Earth. Famous landmarks like the Grand Canyon are composed of massive sandstone layers, and many ancient monuments like those in Petra, Jordan, are carved directly into sandstone cliffs.
Field identification & locations
Identify in the field by its distinctive 'sandpaper' feel and visible grain structure under a magnifying glass. It often shows bedding planes or layers. It is found globally in sedimentary basins.
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Other sedimentary specimens
Fossiliferous Sedimentary Rock
Sedimentary limestone with invertebrate fossil imprint
fossil
Sandstone or Siltstone
Arenite (if sandstone)
Sedimentary
Sandstone
Arenite
sedimentary
Quartz pebble
Silicon dioxide (SiO2)
sedimentary
Shale
Shale (clastic sedimentary rock)
sedimentary
Shale (or Mudstone/Siltstone)
Sedimentary Mudrock (SiO2, Al2O3 base with clay minerals)
sedimentary