
sedimentary
Likely weathered sandstone or iron-rich sedimentary rock
Quartz-rich sandstone, possibly ferruginous sandstone
AI-generated identification · may be incorrectBrown-tan, dull and earthy, with a rough granular texture and apparent weak cementation; likely Mohs hardness about 6–7 for quartz grains but may crumble where weathered. No clear crystal faces or cleavage are visible; specific gravity is commonly 2.2–2.7.
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Physical properties
Brown-tan, dull and earthy, with a rough granular texture and apparent weak cementation; likely Mohs hardness about 6–7 for quartz grains but may crumble where weathered. No clear crystal faces or cleavage are visible; specific gravity is commonly 2.2–2.7.
Formation & geological history
Formed when sand-sized quartz and rock fragments were deposited, compacted, and cemented, typically in river, shoreline, or desert environments. Its precise geological age cannot be determined from the photograph.
Uses & applications
Usually used as building or paving stone when sound; small pieces have little commercial value but may be collected as geological specimens or jewelry curiosities.
Geological facts
The rusty coloration commonly comes from iron-oxide coatings or cement. The visible graininess and irregular weathering distinguish it from most crystalline minerals.
Field identification & locations
Look for individual sand grains, uneven fracture, and a lack of cleavage; a streak test, dilute acid test, and hand lens would improve identification. Sandstone occurs worldwide, especially in sedimentary basins.
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