Rock Identifier
Tumbled greenish stone, likely altered basalt or serpentinite (Probable basaltic/mafic rock with secondary chlorite, epidote, or serpentine minerals) — igneous
igneous

Tumbled greenish stone, likely altered basalt or serpentinite

Probable basaltic/mafic rock with secondary chlorite, epidote, or serpentine minerals

AI-generated identification · may be incorrect

Fine-grained, rounded and polished, with olive-green, brown, and rusty mottling; dull to slightly waxy luster and no visible cleavage. Estimated hardness is about 5–6 Mohs, though the porous weathered surface makes identification uncertain.

Identified More igneous
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Physical properties

Fine-grained, rounded and polished, with olive-green, brown, and rusty mottling; dull to slightly waxy luster and no visible cleavage. Estimated hardness is about 5–6 Mohs, though the porous weathered surface makes identification uncertain.

Formation & geological history

Likely a weathered stream or beach pebble derived from mafic volcanic rock and later hydrothermally altered; basalt commonly formed in the Mesozoic or younger, but its exact age cannot be determined from the image.

Uses & applications

Suitable for landscaping, craft stones, tumbling, and casual collecting; not typically used as a gemstone or high-value ornamental material.

Geological facts

Green coloration may result from chlorite, epidote, or serpentine replacing original basaltic minerals, while orange-brown patches are iron oxides.

Field identification & locations

A hand lens should reveal a fine crystalline texture; a streak, hardness, magnetism, and acid test can help distinguish basalt, serpentinite, and other greenstones. Common in volcanic terrains and glacial or stream gravels.