
sedimentary
Sandstone (Quartz-rich Cobble)
Arenite
Hardness: 6-7 (Mohs); Color: Tan, gray, or buff with orange iron oxidation spots; Luster: Dull/Earthy; Texture: Granular/Sand-like feel; Cleavage: None
- Hardness
- 6-7 (Mohs)
- Color
- Tan, gray, or buff with orange iron oxidation spots
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 (Mohs); Color: Tan, gray, or buff with orange iron oxidation spots; Luster: Dull/Earthy; Texture: Granular/Sand-like feel; Cleavage: None
Formation & geological history
Formed through the accumulation and cementation of sand-sized mineral grains, typically quartz and feldspar, in high-energy environments like rivers, beaches, or deserts. This specimen shows a rounded shape indicative of fluvial or glacial transport.
Uses & applications
Used widely in construction for building stone, paving, and as an abrasive. Crushed sandstone is used to make glass and for industrial sand-casting.
Geological facts
Sandstone makes up about 20-25% of all sedimentary rocks on Earth. The orange spots on this specimen are likely iron oxide (limonite or hematite) leached from internal minerals or environmental water.
Field identification & locations
Identify by its gritty texture (feels like sandpaper) and visible grains. It is extremely common in riverbeds, canyons, and mountainous regions worldwide. It often preserves fossils and ripple marks from ancient environments.
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