Rock Identifier
Serpentine-rich metamorphic rock (Serpentinite, primarily serpentine-group minerals [Mg₃Si₂O₅(OH)₄], possibly with magnetite and/or chromite) — metamorphic
metamorphic

Serpentine-rich metamorphic rock

Serpentinite, primarily serpentine-group minerals [Mg₃Si₂O₅(OH)₄], possibly with magnetite and/or chromite

AI-generated identification · may be incorrect

Dark olive-green to gray, mottled and waxy-looking with a dull to greasy luster; typically massive rather than visibly crystalline. Hardness is about 2.5–4 Mohs, with poor cleavage and specific gravity around 2.5–2.6.

Identified More metamorphic
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Physical properties

Dark olive-green to gray, mottled and waxy-looking with a dull to greasy luster; typically massive rather than visibly crystalline. Hardness is about 2.5–4 Mohs, with poor cleavage and specific gravity around 2.5–2.6.

Formation & geological history

Forms when ultramafic mantle rocks such as peridotite undergo low-temperature hydrothermal alteration and hydration, commonly along faults and oceanic crust; ages vary widely. The image is insufficient for precise locality or age determination.

Uses & applications

Used as decorative and architectural stone, carvings, countertops, and occasionally jewelry; attractive polished material can have modest collector value.

Geological facts

Serpentinite may contain magnetite, causing weak magnetic response, and may host asbestos-forming minerals; avoid cutting, grinding, or creating dust until professionally tested.

Field identification & locations

Look for a green-black mottled color, unusually soft/waxy surface, and possible magnetism; distinguish it from jade with hardness and laboratory testing. Common in California, Italy, New Zealand, Canada, and ophiolite belts worldwide.