Rock Identifier
Serpentinite (Serpentinite (Mg, Fe, Ni, Al, Zn, Mn)2-3(Si, Al, Fe)2O5(OH)4) — metamorphic
metamorphic

Serpentinite

Serpentinite (Mg, Fe, Ni, Al, Zn, Mn)2-3(Si, Al, Fe)2O5(OH)4

Hardness: 3-6 Mohs; Color: Dark green to black, often mottled or waxy; Luster: Greasy, waxy, or silky; Structure: Massive to fibrous; Specific Gravity: 2.5-2.6

Hardness
3-6 Mohs
Color
Dark green to black, often mottled or waxy
Luster
Greasy, waxy, or silky
Identified More metamorphic

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Physical properties

Hardness: 3-6 Mohs; Color: Dark green to black, often mottled or waxy; Luster: Greasy, waxy, or silky; Structure: Massive to fibrous; Specific Gravity: 2.5-2.6

Formation & geological history

Formed through the hydrothermal alteration of ultramafic rocks (peridotite/pyroxenite) from the Earth's mantle, typically at tectonic plate boundaries (subduction zones).

Uses & applications

Used as an architectural ornamental stone (verde antique), source for magnesium, and historically as a source of asbestos. Used in carvings and jewelry.

Geological facts

Serpentinite is the official state rock of California. It is often called 'serpentine,' though serpentine is technically the name of the mineral group it contains.

Field identification & locations

Identify by its characteristic 'snake-skin' appearance, greasy feel, and green color. Common in ophiolite complexes and mountain ranges like the Alps or the California Coast Ranges.