Rock Identifier
Rounded iron-rich pebble, possibly weathered laterite or ironstone (Ironstone/lateritic ferricrete; predominantly goethite–hematite with clay and quartz impurities) — sedimentary
sedimentary

Rounded iron-rich pebble, possibly weathered laterite or ironstone

Ironstone/lateritic ferricrete; predominantly goethite–hematite with clay and quartz impurities

AI-generated identification · may be incorrect

Hardness typically 4–6 Mohs; rusty orange-brown, dull to earthy luster, fine-grained and noncrystalline-looking, with possible pale quartz or clay spots. Specific gravity commonly about 2.5–4.0, depending on iron content.

Identified More sedimentary
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Physical properties

Hardness typically 4–6 Mohs; rusty orange-brown, dull to earthy luster, fine-grained and noncrystalline-looking, with possible pale quartz or clay spots. Specific gravity commonly about 2.5–4.0, depending on iron content.

Formation & geological history

Likely formed by intense chemical weathering and iron accumulation in tropical or subtropical soils, then rounded by transport; age cannot be determined from the image. It could also be an iron-rich concretion or weathered volcanic fragment.

Uses & applications

Used as iron ore when sufficiently rich, and as aggregate or lapidary material; this small rounded specimen has mainly educational or decorative value.

Geological facts

Iron oxides produce the orange-brown color, while dark gray areas may contain manganese oxides or hematite. A streak test and magnet test would help distinguish it from ordinary brown sandstone or volcanic rock.

Field identification & locations

Look for a yellow-brown to red streak, earthy texture, and locally strong magnetism; a fresh surface may reveal metallic gray hematite. Common in tropical weathering profiles, river gravels, and iron-rich sedimentary terrains.