Rock Identifier
Likely serpentine-rich metamorphic rock (Serpentinite; chiefly serpentine-group minerals (Mg₃Si₂O₅(OH)₄), possibly with magnetite and chlorite) — metamorphic
metamorphic

Likely serpentine-rich metamorphic rock

Serpentinite; chiefly serpentine-group minerals (Mg₃Si₂O₅(OH)₄), possibly with magnetite and chlorite

AI-generated identification · may be incorrect

Small dark green-gray, fine-grained, weakly lustrous specimen with a mottled texture. Serpentine has Mohs hardness about 2.5–4, no consistent cleavage, and commonly forms compact or waxy masses; the photo alone cannot confirm exact mineralogy.

Identified More metamorphic
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Physical properties

Small dark green-gray, fine-grained, weakly lustrous specimen with a mottled texture. Serpentine has Mohs hardness about 2.5–4, no consistent cleavage, and commonly forms compact or waxy masses; the photo alone cannot confirm exact mineralogy.

Formation & geological history

Forms when ultramafic mantle rocks such as peridotite are hydrated and metamorphosed, commonly along oceanic crust and tectonic plate boundaries. Serpentinization ranges from ancient Precambrian events to modern seafloor alteration.

Uses & applications

Used as ornamental stone, carvings, architectural stone, and historically as a source of asbestos minerals; attractive pieces are collected, though fibrous varieties should not be cut or powdered.

Geological facts

Often shows dark green to black color, slick or waxy surfaces, and may attract a magnet if magnetite is abundant. It can be confused with greenstone, jade, or chlorite-rich rocks.

Field identification & locations

Common in California, Italy, New Zealand, Canada, and ophiolite belts worldwide; test cautiously for softness and waxy texture, but laboratory testing is needed for reliable identification and asbestos screening.