
sedimentary
Weathered iron-rich sandstone or ferruginous quartzite pebble
Ferruginous sandstone, primarily quartz (SiO₂) with iron oxides/hydroxides
AI-generated identification · may be incorrectHardness about 5.5–7 Mohs; reddish-brown, fine-grained, dull to weakly earthy luster, rounded and strongly weathered. The porous, granular texture suggests sandstone rather than a crystalline quartzite; no visible cleavage.
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Physical properties
Hardness about 5.5–7 Mohs; reddish-brown, fine-grained, dull to weakly earthy luster, rounded and strongly weathered. The porous, granular texture suggests sandstone rather than a crystalline quartzite; no visible cleavage.
Formation & geological history
Likely a water-worn sedimentary pebble cemented by silica and iron oxides, then rounded by stream or beach transport. Its exact geological age cannot be determined from the image; ferruginous sandstones occur from Precambrian to modern formations.
Uses & applications
Common material for landscaping, decorative stone, crafts, and educational collections; generally little commercial value unless unusually patterned or locality-specific.
Geological facts
The red-brown color is produced mainly by hematite and/or goethite coatings between quartz grains. Its smooth shape indicates prolonged abrasion in flowing water or surf.
Field identification & locations
Identify it by its gritty granular surface, rusty-red coloration, rounded form, and lack of visible crystals; a streak, acid, hardness, and specific-gravity test would refine identification. Common in stream gravels, beaches, and weathered sandstone outcrops worldwide.
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