
sedimentary
Sandstone
Quartz Arenite / Clastic Sedimentary Rock
Hardness: 6-7 on Mohs scale (due to quartz grains); Color: tan, yellow, brown, red, grey, or white; Luster: dull to earthy; Crystal structure: clastic (composed of mineral particles or rock fragments cemented together); Cleavage: none; Specific gravity: 2.2-2.8
- Hardness
- 6-7 on Mohs scale (due to quartz grains)
- Color
- tan, yellow, brown, red, grey, or white
- Luster
- dull to earthy
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Physical properties
Hardness: 6-7 on Mohs scale (due to quartz grains); Color: tan, yellow, brown, red, grey, or white; Luster: dull to earthy; Crystal structure: clastic (composed of mineral particles or rock fragments cemented together); Cleavage: none; Specific gravity: 2.2-2.8
Formation & geological history
Formed by the accumulation, compaction, and cementation of mineral particles or rock fragments (mostly quartz and feldspar) sized between 1/16 mm and 2 mm, typically deposited in environments like beaches, deserts, floodplains, and shallow marine waters over millions of years.
Uses & applications
Commonly used in construction as a building material, paving stone, landscaping, and historically for whetstones and grindstones.
Geological facts
Sandstone is porous, which allows it to act as an aquifer, storing large amounts of groundwater and trapping petroleum and natural gas.
Field identification & locations
Easily identifiable by its sandy texture, visible grain structure, and layered appearance. Found worldwide in sedimentary basins and eroded cliffs.
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