
sedimentary
Sandstone
Arenite (siliciclastic sedimentary rock composed mostly of quartz)
Hardness: 6-7 on Mohs scale (due to quartz grains); Color: reddish-brown, tan, or iron-stained orange; Luster: dull to earthy; Texture: granular, feel like sandpaper; Cleavage: none; Specific Gravity: 2.2-2.8
- Hardness
- 6-7 on Mohs scale (due to quartz grains)
- Color
- reddish-brown, tan, or iron-stained orange
- Luster
- dull to earthy
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Physical properties
Hardness: 6-7 on Mohs scale (due to quartz grains); Color: reddish-brown, tan, or iron-stained orange; Luster: dull to earthy; Texture: granular, feel like sandpaper; Cleavage: none; Specific Gravity: 2.2-2.8
Formation & geological history
Formed through the accumulation, compaction, and cementation of sand-sized mineral particles or rock fragments, usually deposited in desert dunes, riverbeds, beaches, or shallow seas over millions of years.
Uses & applications
Widely used as a construction and paving material, in dimension stone for architecture, as crushed stone, and historically for grindstones. Naturally porous varieties serve as reservoirs for petroleum and groundwater.
Geological facts
Sandstone makes up about 20% of all sedimentary rocks on Earth. The famous red rock formations of Sedona, Arizona, and Zion National Park in Utah are made largely of iron-rich sandstone layers.
Field identification & locations
Identified by its distinctly gritty, sandpaper-like surface feel and visible quartz sand grains. Commonly found near ancient or active river valleys, coastal cliffs, and desert environments worldwide.
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