
sedimentary
Sandstone
Sandstone (SiO2 dominated)
Mohs hardness: 6 to 7 (quartz-rich). Color: Buff, light brown, pinkish-tan. Luster: Earthy, dull, abrasive feel like sandpaper. Grain structure: Fine to medium sand-sized clastic grains cemented by silica, iron oxide, or calcite.
- Hardness
- 6 to 7 (quartz-rich)
- Color
- Buff, light brown, pinkish-tan
- Luster
- Earthy, dull, abrasive feel like sandpaper
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Physical properties
Mohs hardness: 6 to 7 (quartz-rich). Color: Buff, light brown, pinkish-tan. Luster: Earthy, dull, abrasive feel like sandpaper. Grain structure: Fine to medium sand-sized clastic grains cemented by silica, iron oxide, or calcite.
Formation & geological history
Formed by the compaction and cementation of sand-sized mineral particles or rock fragments, typically in ancient desert dunes, beaches, rivers, or delta environments.
Uses & applications
Widely used as a construction material, paving stone, decorative landscaping stone, and historically for grindstones and sculpture.
Geological facts
Sandstone accounts for roughly 10-20% of the Earth's sedimentary rocks. Red and orange hues are typically due to iron oxide minerals such as hematite acting as a natural cement.
Field identification & locations
Identified by its gritty sandpaper texture and visible layered or blocky fracture. Commonly found in sedimentary basins, canyons, and cliff faces worldwide.
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