
sedimentary
Sandstone
Sandstone (composed predominantly of Quartz, SiO2, with Feldspar and Clay minerals)
Hardness: 6-7 (varies based on cementation); Color: Yellowish-brown, tan, reddish-brown, green tint from lichen/weathering; Luster: Dull, earthy; Crystal structure: Granular, clastic texture; Cleavage: None; Specific Gravity: 2.2-2.8
- Hardness
- 6-7 (varies based on cementation)
- Luster
- Dull, earthy
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Physical properties
Hardness: 6-7 (varies based on cementation); Color: Yellowish-brown, tan, reddish-brown, green tint from lichen/weathering; Luster: Dull, earthy; Crystal structure: Granular, clastic texture; Cleavage: None; Specific Gravity: 2.2-2.8
Formation & geological history
Formed by the compaction and cementation of mineral particles or rock fragments, usually quartz and feldspar, deposited in desert, river, beach, or shallow sea environments over millions of years.
Uses & applications
Widely used as a construction material, paving stone, decorative landscaping stone, and historically for grindstones and sculpture. Important reservoir rock for groundwater and petroleum.
Geological facts
Sandstone accounts for roughly 20 to 25 percent of all sedimentary rocks. Famous landmarks made of sandstone include Petra in Jordan and the Grand Canyon strata in the USA.
Field identification & locations
Identified in the field by its distinctive gritty feel, coarse sand-sized grains, and often visible layering or bedding planes. Very common globally in sedimentary basins, riverbeds, and cliffs.
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