Rock Identifier
Tumbled iron-rich concretion or ironstone pebble (Goethite–hematite-rich ironstone; commonly limonite (FeO(OH)·nH₂O) with hematite (Fe₂O₃)) — sedimentary
sedimentary

Tumbled iron-rich concretion or ironstone pebble

Goethite–hematite-rich ironstone; commonly limonite (FeO(OH)·nH₂O) with hematite (Fe₂O₃)

AI-generated identification · may be incorrect

Dark brown to black, opaque, earthy to submetallic luster, smoothly water-worn or tumbled, with faint fibrous/striated textures. Hardness is approximately 5–6.5 Mohs; no obvious cleavage; specific gravity commonly 3.0–4.3.

Identified More sedimentary
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Physical properties

Dark brown to black, opaque, earthy to submetallic luster, smoothly water-worn or tumbled, with faint fibrous/striated textures. Hardness is approximately 5–6.5 Mohs; no obvious cleavage; specific gravity commonly 3.0–4.3.

Formation & geological history

Likely formed as an iron-oxide/hydroxide concretion or weathering product that became rounded in sediment or stream transport; exact age and locality cannot be determined from the image. Ironstones form in many sedimentary and lateritic environments.

Uses & applications

Primarily a collector or teaching specimen; ironstone is mined as iron ore, while attractive polished pieces may be used decoratively. It is generally not a jewelry gemstone.

Geological facts

Its unusually heavy appearance and rusty-brown color reflect concentrated iron minerals. The surface pattern may result from botryoidal or fibrous goethite growth and subsequent polishing.

Field identification & locations

Test for strong heft, streak, and possible magnetism; a yellow-brown streak suggests goethite/limonite, while a red-brown streak suggests hematite. Common in iron-rich soils, river gravels, and banded-iron regions worldwide.