Rock Identifier
Polished serpentine (often sold as “new jade” or lemon serpentine) (Serpentine-group minerals, chiefly antigorite and lizardite; approximate formula Mg₃Si₂O₅(OH)₄) — metamorphic
metamorphic

Polished serpentine (often sold as “new jade” or lemon serpentine)

Serpentine-group minerals, chiefly antigorite and lizardite; approximate formula Mg₃Si₂O₅(OH)₄

AI-generated identification · may be incorrect

Mohs hardness 2.5–4; pale yellow-green to olive-green, mottled and waxy with a greasy or subvitreous luster. Typically massive and fine-grained, with no visible crystal cleavage; specific gravity about 2.5–2.6.

Identified More metamorphic
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Physical properties

Mohs hardness 2.5–4; pale yellow-green to olive-green, mottled and waxy with a greasy or subvitreous luster. Typically massive and fine-grained, with no visible crystal cleavage; specific gravity about 2.5–2.6.

Formation & geological history

Formed when ultramafic mantle rocks such as peridotite hydrate during low-temperature metamorphism, commonly in oceanic crust and subduction zones. Serpentinization ranges from Paleozoic to modern geological settings.

Uses & applications

Used for carvings, cabochons, beads, ornamental stone, and architectural facing; attractive pieces have modest lapidary value.

Geological facts

“New jade” is a trade name and is not true jadeite or nephrite. Some serpentine contains chrysotile asbestos, so avoid cutting or generating dust unless tested and handled safely.

Field identification & locations

Identify by its soft, waxy feel, green-yellow mottling, rounded polish, and ability to scratch with a steel knife; it is commonly found in serpentinite belts worldwide, including California, Italy, New Zealand, and Canada.