Rock Identifier
Likely brown ironstone or limonite-rich rock fragment (Ironstone, chiefly iron oxides/hydroxides such as goethite (α-FeO(OH)) and limonite) — sedimentary
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 incorrect

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).

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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.