
Iron-stained breccia or weathered conglomerate pebble
Clastic sedimentary rock; likely quartz-rich sandstone/breccia with dark mafic or iron-manganese fragments
AI-generated identification · may be incorrectTan, fine-to-medium clastic matrix with irregular dark gray-black patches; likely Mohs 5–7, dull to earthy luster, no visible cleavage, and probable quartz-bearing composition. The rounded shape indicates natural water abrasion or tumbling.
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