
sedimentary
Sandstone Pebble
Arenite (primarily SiO2)
Hardness: 6-7 on Mohs scale; Color: Tan, beige, or yellowish-brown; Luster: Dull/Earthy; Crystal Structure: Clastic (sand-sized grains); Cleavage: None (conchoidal fracture on grains); Specific Gravity: 2.2-2.8
- Hardness
- 6-7 on Mohs scale
- Color
- Tan, beige, or yellowish-brown
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 on Mohs scale; Color: Tan, beige, or yellowish-brown; Luster: Dull/Earthy; Crystal Structure: Clastic (sand-sized grains); Cleavage: None (conchoidal fracture on grains); Specific Gravity: 2.2-2.8
Formation & geological history
Formed through the accumulation and cementation of mineral particles or rock fragments (sand) in environments like riverbeds, deserts, or beaches. This specimen appears water-worn and rounded by fluvial or coastal transport.
Uses & applications
Used primarily as construction aggregate, road base, and decorative landscaping gravel. In larger forms, sandstone is a major dimension stone for architecture.
Geological facts
Sandstone comprises about 20-25% of all sedimentary rocks on Earth. It often acts as a massive reservoir for groundwater, oil, and natural gas due to its high porosity.
Field identification & locations
Identify in the field by its gritty, sandpaper-like feel and the visible presence of small, cemented sand grains. Common in riverbeds and ancient sedimentary basins worldwide.
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