
sedimentary
Sandstone Pebble
Arenite (SiO2 primarily)
Hardness: 6-7 (Mohs scale); Color: Tan, brown, or buff; Luster: Dull/Earthy; Crystal Structure: Clastic (sand grains); Cleavage: None; Specific Gravity: 2.2-2.8
- Hardness
- 6-7 (Mohs scale)
- Color
- Tan, brown, or buff
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 (Mohs scale); Color: Tan, brown, or buff; Luster: Dull/Earthy; Crystal Structure: Clastic (sand grains); Cleavage: None; Specific Gravity: 2.2-2.8
Formation & geological history
Formed by the accumulation and cementation of sand-sized mineral grains, typically quartz or feldspar, over millions of years in riverbeds, deserts, or beaches (Phanerozoic Eon).
Uses & applications
Used extensively in construction as building stone, road base, or aggregate; fine-grained varieties are used for sharpening tools or as decorative landscaping stones.
Geological facts
Sandstone can hold significant amounts of water or oil in its pore spaces, making it a vital reservoir rock for groundwater aquifers and petroleum resources.
Field identification & locations
Identify by its gritty, sandpaper-like feel and visible clastic grains. Commonly found in riverbeds, canyons, and sedimentary basins worldwide. Look for layered structures and rounded edges if water-worn.
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Cone-in-cone structure (Secondary Sedimentary Structure)
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Clastic Sedimentary Rock Grain (SiO2 dominated)
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Sandstone
Arenite (primarily SiO2)
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