Rock Identifier
Rounded red-brown ironstone cobble (Ferruginous sandstone or ironstone; commonly quartz grains cemented by iron oxides such as hematite and goethite) — sedimentary
sedimentary

Rounded red-brown ironstone cobble

Ferruginous sandstone or ironstone; commonly quartz grains cemented by iron oxides such as hematite and goethite

AI-generated identification · may be incorrect

Opaque, reddish-brown, with a rough, fine-grained surface and rounded shape. Likely hardness around 5–7 Mohs if quartz-rich; no obvious cleavage. Exact composition and density cannot be confirmed from the image.

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Physical properties

Opaque, reddish-brown, with a rough, fine-grained surface and rounded shape. Likely hardness around 5–7 Mohs if quartz-rich; no obvious cleavage. Exact composition and density cannot be confirmed from the image.

Formation & geological history

Likely formed as iron-rich sediment or sandstone cemented by iron oxides, then rounded by prolonged water transport. Its geological age and precise formation environment cannot be determined visually.

Uses & applications

Usually a decorative or collectible field specimen; iron-rich stone may also be used as low-grade iron ore or aggregate where composition and quality warrant.

Geological facts

Iron oxides produce the red-brown color, and rounded edges typically indicate abrasion during transport or weathering.

Field identification & locations

Look for a dense, earthy-red to brown stone with iron staining; a streak, magnetism test, or hardness test can help distinguish ironstone from other cobbles. Such material occurs in sedimentary deposits worldwide.