Rock Identifier
Rounded yellow-green stone, likely serpentine or weathered greenstone (Serpentine-group minerals, commonly antigorite or lizardite; exact identification requires testing) — metamorphic
metamorphic

Rounded yellow-green stone, likely serpentine or weathered greenstone

Serpentine-group minerals, commonly antigorite or lizardite; exact identification requires testing

AI-generated identification · may be incorrect

Opaque olive-yellow green, dull to waxy luster, smoothly rounded and probably water-worn; likely Mohs hardness 2.5–4, with no visible crystals or cleavage. Specific gravity is commonly about 2.5–2.6.

Identified More metamorphic
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Physical properties

Opaque olive-yellow green, dull to waxy luster, smoothly rounded and probably water-worn; likely Mohs hardness 2.5–4, with no visible crystals or cleavage. Specific gravity is commonly about 2.5–2.6.

Formation & geological history

Serpentine forms when ultramafic rocks such as peridotite are hydrated during metamorphism, commonly in ophiolites and fault zones; its age depends on the host terrain. The rounded shape indicates later stream or beach transport.

Uses & applications

Usually collected as a curiosity or lapidary stone; suitable pieces may be polished for cabochons or carvings, but this small specimen has little industrial value.

Geological facts

The image alone cannot distinguish serpentine from epidote-rich greenstone, altered basalt, or another weathered rock. Some serpentine rocks may contain fibrous chrysotile, so avoid cutting, grinding, or creating dust until tested.

Field identification & locations

Look for a greasy or waxy feel, green-to-yellow color, low hardness, and possible white veining; a steel nail may scratch it. Common settings include California, Oregon, Italy, New Zealand, and ophiolite belts worldwide.