
sedimentary
Sandstone (Ferruginous)
Arenite (with iron oxide cement)
Hardness: 6-7 on Mohs scale; Color: Reddish-brown to tan; Luster: Dull/Earthy; Crystal Structure: Clastic (composed of sand-sized mineral grains); Cleavage: None; Specific Gravity: 2.2-2.8
- Hardness
- 6-7 on Mohs scale
- Color
- Reddish-brown to tan
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 on Mohs scale; Color: Reddish-brown to tan; Luster: Dull/Earthy; Crystal Structure: Clastic (composed of sand-sized mineral grains); Cleavage: None; Specific Gravity: 2.2-2.8
Formation & geological history
Formed through the accumulation and cementation of sand-sized silicate grains (mostly quartz). The reddish hue is caused by the presence of iron oxide (hematite) during the lithification process. Common in prehistoric riverbeds, deserts, and coastal environments.
Uses & applications
Used extensively as a building and paving material, for grindstones, and sometimes as a source of high-purity silica for glassmaking. Also popular as a decorative landscaping stone.
Geological facts
Sandstone is one of the most common types of sedimentary rock and provides critical data for geologists to map paleo-environments and calculate the history of Earth's surface water and wind patterns.
Field identification & locations
Identify in the field by its gritty, sandpaper-like texture and visible grains. It is commonly found in the US Southwest, the UK, and Australia. Look for bedding planes or layering within larger outcrops.
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