
sedimentary
Sandstone
Sedimentary Rock (Quartz arenite / Lithic sandstone)
AI-generated identification · may be incorrectHardness: 6 to 7 on the Mohs scale (depending on cementation); Color: Tan, brown, yellow, red, grey, or white; Luster: Dull to earthy; Crystal structure: Clastic (composed of mineral particles or rock fragments, predominantly quartz); Cleavage: None (fractures unevenly); Specific Gravity: 2.2 to 2.8
- Hardness
- 6 to 7 on the Mohs scale (depending on cementation)
- Color
- Tan, brown, yellow, red, grey, or white
- Luster
- Dull to earthy
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Physical properties
Hardness: 6 to 7 on the Mohs scale (depending on cementation); Color: Tan, brown, yellow, red, grey, or white; Luster: Dull to earthy; Crystal structure: Clastic (composed of mineral particles or rock fragments, predominantly quartz); Cleavage: None (fractures unevenly); Specific Gravity: 2.2 to 2.8
Formation & geological history
Formed through the accumulation, compaction, and cementation of mineral particles or rock fragments (mainly quartz and feldspar) of sand size, typically in environments such as beaches, deserts, floodplains, and shallow marine areas over millions of years.
Uses & applications
Widely used in construction as a building stone, paving material, for making grindstones, and as a reservoir rock for petroleum and natural gas.
Geological facts
Many of the world's most famous monuments and ancient structures, including the Treasury in Petra and parts of the Egyptian temples, were carved directly out of massive sandstone formations.
Field identification & locations
Identified by its gritty texture (feels like sandpaper) and visible sand grains. Found worldwide in sedimentary basins, deserts, and ancient riverbeds. Collectors look for unique banding or fossil impressions.
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