Rock Identifier
Rounded iron-rich stone, likely basalt or ironstone (Probably basalt (dark volcanic rock) with iron-oxide weathering; exact identification is uncertain from the photograph) — igneous
igneous

Rounded iron-rich stone, likely basalt or ironstone

Probably basalt (dark volcanic rock) with iron-oxide weathering; exact identification is uncertain from the photograph

AI-generated identification · may be incorrect

Dark brown-black, fine-grained, dull to slightly metallic surface, and smoothly water-worn; likely Mohs hardness 5–6, with no visible cleavage and very small interlocking crystals. The rusty coloration suggests oxidation of iron-bearing minerals.

Identified More igneous
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Physical properties

Dark brown-black, fine-grained, dull to slightly metallic surface, and smoothly water-worn; likely Mohs hardness 5–6, with no visible cleavage and very small interlocking crystals. The rusty coloration suggests oxidation of iron-bearing minerals.

Formation & geological history

If basalt, it formed from rapidly cooled mafic lava, commonly in volcanic flows, then became rounded by stream or coastal abrasion; likely Cenozoic or older. It could alternatively be a weathered ironstone pebble or slag, which would require testing to distinguish.

Uses & applications

Common basalt is used as aggregate, roadstone, riprap, and landscaping material; ironstone has limited industrial value. This individual pebble has little jewelry or commercial value.

Geological facts

Basalt commonly contains plagioclase, pyroxene, and sometimes olivine, while iron oxides produce red-brown weathering colors. Its smooth shape indicates transport or deliberate tumbling.

Field identification & locations

Look for a uniformly fine texture, heavy feel, and weak or absent magnetism; a streak test, magnet test, and fresh chip would help distinguish basalt from ironstone or slag. Common worldwide, especially near volcanic terrains and riverbeds.