Rock Identifier
Tumbled green stone, possibly serpentine or epidote-bearing rock (Uncertain from image; likely serpentine-group mineral (Mg₃Si₂O₅(OH)₄) or epidote-rich metamorphic rock) — mineral
mineral

Tumbled green stone, possibly serpentine or epidote-bearing rock

Uncertain from image; likely serpentine-group mineral (Mg₃Si₂O₅(OH)₄) or epidote-rich metamorphic rock

AI-generated identification · may be incorrect

Small rounded pebble with mottled olive-green and gray coloration, dull to slightly waxy luster, and no visible crystal faces. Serpentine has Mohs hardness 2.5–4; epidote-rich material is typically 6–7; cleavage and specific gravity cannot be determined visually.

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Physical properties

Small rounded pebble with mottled olive-green and gray coloration, dull to slightly waxy luster, and no visible crystal faces. Serpentine has Mohs hardness 2.5–4; epidote-rich material is typically 6–7; cleavage and specific gravity cannot be determined visually.

Formation & geological history

Likely formed by hydrothermal alteration of ultramafic rocks (serpentine) or regional metamorphism producing epidote-rich rock; age depends on locality and may range from Paleozoic to recent geologic settings.

Uses & applications

Commonly sold as a tumbled decorative stone, carving material, or inexpensive lapidary specimen; serpentine is also used ornamentally in larger pieces.

Geological facts

The image does not show diagnostic features sufficient for a confident species identification; similar green pebbles may also be jade, chlorite schist, or greenstone.

Field identification & locations

Test hardness, streak, translucency, and density; serpentine is relatively soft and often waxy, whereas jade is tougher and harder. Common sources include California, New Zealand, Italy, Canada, and Afghanistan.