
sedimentary
Ironstone concretion with iron-oxide/possibly hematite inclusions
Ferruginous sandstone or lateritic ironstone; inclusions likely hematite (Fe₂O₃) and/or goethite (FeO(OH))
AI-generated identification · may be incorrectReddish-brown, earthy, dull to submetallic surface with darker rusty inclusions; typical hardness ~5–6.5 for hematite-bearing material, variable porosity, and no obvious cleavage. The rounded shape suggests a naturally weathered concretion or pebble.
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Physical properties
Reddish-brown, earthy, dull to submetallic surface with darker rusty inclusions; typical hardness ~5–6.5 for hematite-bearing material, variable porosity, and no obvious cleavage. The rounded shape suggests a naturally weathered concretion or pebble.
Formation & geological history
Formed when iron oxides cemented sand, clay, or soil during weathering and groundwater movement; commonly Cenozoic to older, depending on its host deposit. Exact age cannot be determined from the photograph.
Uses & applications
Primarily a geological or educational specimen; iron-rich rocks have historically been mined as low-grade iron ore and used as pigments, aggregate, or building stone. This example is unlikely to have jewelry value.
Geological facts
Hematite produces red-brown streak and commonly gives ironstone its coloration; magnetism, if present, may indicate magnetite or maghemite rather than pure hematite.
Field identification & locations
Look for a red-to-reddish-brown streak on unglazed ceramic, heavy feel, and rusty weathering; a strong magnet suggests magnetite-bearing ironstone. Common in lateritic soils, stream gravels, banded iron formations, and sedimentary iron deposits worldwide.
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