
sedimentary
Sandstone
Arenite (SiO2 primarily)
Color: tan, brown, or buff; Hardness: 6-7 Mohs (on individual quartz grains); Luster: earthy/dull; Texture: clastic/gritty like sandpaper; Structure: massive or bedded; Cleavage: none.
- Hardness
- 6-7 Mohs (on individual quartz grains)
- Color
- tan, brown, or buff
- Luster
- earthy/dull
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Physical properties
Color: tan, brown, or buff; Hardness: 6-7 Mohs (on individual quartz grains); Luster: earthy/dull; Texture: clastic/gritty like sandpaper; Structure: massive or bedded; Cleavage: none.
Formation & geological history
Formation occurs over millions of years through the accumulation, compaction, and cementation of sand-sized mineral grains or rock fragments, typically in river beds, beaches, or deserts.
Uses & applications
Used extensively in construction as building stone, pavers, and as a source for silica in glass manufacturing. Fine specimens are popular for amateur rock collecting.
Geological facts
Sandstone can preserve fossilized footprints and ripple marks from ancient water currents. It is a major reservoir rock for underground water and petroleum.
Field identification & locations
Identified by its sandy, abrasive texture when rubbed. It is globally ubiquitous, found in many canyons and outcrops. Collectors should look for unique layering or fossils.
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