
sedimentary
Sandstone
Arenite (SiO2 based)
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
- Hardness
- 6-7 (Mohs)
- Color
- Tan, yellowish-brown, buff
- Luster
- Dull, earthy
Identified More sedimentary →
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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
Sandstone or Siltstone
Arenite (if sandstone)
Sedimentary
Fossiliferous Concretion
Septarian Concretion containing Brachiopods/Crinoids
fossil
Shale
Shale (clastic sedimentary rock)
sedimentary
Brown Sandstone (River Rock)
Arenite
sedimentary
Cone-in-cone structure (Limestone)
Cone-in-cone structure (Secondary Sedimentary Structure)
sedimentary
Shale
Argillaceous sedimentary rock
sedimentary