
sedimentary
Likely brown ironstone or limonite-rich rock fragment
Ironstone, chiefly iron oxides/hydroxides such as goethite (α-FeO(OH)) and limonite
AI-generated identification · may be incorrectSmall, rough, opaque brown specimen with an earthy to dull luster; hardness and specific gravity cannot be reliably determined from the photo. Ironstone is commonly massive rather than visibly crystalline, with variable hardness (about 4–6 for goethite-rich material).
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Physical properties
Small, rough, opaque brown specimen with an earthy to dull luster; hardness and specific gravity cannot be reliably determined from the photo. Ironstone is commonly massive rather than visibly crystalline, with variable hardness (about 4–6 for goethite-rich material).
Formation & geological history
Iron-rich minerals precipitated or accumulated during weathering and sedimentation; ironstone forms in many geological periods and environments. The specimen’s age and exact formation cannot be determined visually.
Uses & applications
Ironstone has historically been mined as iron ore; small fragments are mainly of educational or modest collector interest.
Geological facts
Brown iron-rich coatings and nodules can form as iron-bearing minerals oxidize near Earth’s surface.
Field identification & locations
Look for a dense, earthy brown fragment that may leave a reddish-brown streak; a streak test and hardness test can help distinguish iron oxides from other rocks. Common ironstone deposits occur worldwide.
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