
sedimentary
Sandstone
Arenite (primarily SiO2)
AI-generated identification · may be incorrectHardness: 6.5–7 (Mohs scale); Color: tan, yellow, or buff; Luster: dull/earthy; Crystal structure: clastic/granular texture with visible sand grains (0.0625 to 2 mm); Cleavage: none; Specific gravity: 2.2–2.8.
- Hardness
- 6
- Color
- tan, yellow, or buff
- Luster
- dull/earthy
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Physical properties
Hardness: 6.5–7 (Mohs scale); Color: tan, yellow, or buff; Luster: dull/earthy; Crystal structure: clastic/granular texture with visible sand grains (0.0625 to 2 mm); 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. Typically deposited in deserts (aeolian), riverbeds (fluvial), or coastal beaches. Lithification occurs through compaction and cementation by silica, calcium carbonate, or iron oxide.
Uses & applications
Extensively used in construction as a building stone (dimension stone), flagstone for paving, and in the production of glass (if high silica content) and abrasive materials.
Geological facts
Sandstone accounts for roughly 20% of all sedimentary rocks on Earth. It is a major reservoir for groundwater, oil, and natural gas due to its high porosity and permeability.
Field identification & locations
Identify in the field by its sandpaper-like feel and visible grains that do not fizz with acid (unless a calcitic cement is present). It is found globally, with famous formations like the Navajo Sandstone in the USA. Collectors look for unique banding (wonderstone) or fossil inclusions.
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