Rock Identifier
Serpentinite (Rock of serpentine-group minerals, (Mg,Fe)3Si2O5(OH)4)
metamorphic

Serpentinite

Rock of serpentine-group minerals, (Mg,Fe)3Si2O5(OH)4

A green, often mottled metamorphic rock formed by the hydration of mantle rocks, soft and waxy with a smooth, slippery feel.

Mohs hardness
3-4 (variable, 2.5-5.5)
Color
Green to dark green, often mottled with yellow, black, or white
Type
metamorphic

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Overview

Serpentinite is a metamorphic rock composed largely of serpentine-group minerals (antigorite, lizardite, and chrysotile). It typically forms attractive mottled green masses, sometimes streaked with white veins or black magnetite, giving it a marbled, snakeskin-like appearance that inspired its name.

The rock is relatively soft, often feels smooth, greasy, or waxy, and takes a good polish. It is the dominant rock of the Earth's altered oceanic mantle and is commonly found in ophiolite complexes where slices of seafloor have been thrust onto continents.

Serpentinite is California's official state rock and is widely used as a decorative and carving stone, frequently marketed under the name serpentine.

Formation & geology

Serpentinite forms through serpentinization, a process in which water reacts with magnesium- and iron-rich ultramafic rocks such as peridotite and dunite from the Earth's mantle. This hydration alters olivine and pyroxene into serpentine minerals, releasing heat and dramatically changing the rock's volume and density.

The process occurs primarily at mid-ocean ridges and along subduction zones where seawater penetrates the oceanic crust and uppermost mantle. When ocean floor is later obducted onto continents as ophiolites, the serpentinite is exposed. Major occurrences include California, the Alps, Cyprus, Italy, and New Zealand.

How to identify it

Identify serpentinite by its green to dark-green color, often mottled or veined, and its characteristically smooth, waxy, or soapy feel. It is soft enough to scratch with a knife and frequently shows a slightly translucent, greasy luster on cut surfaces.

Its streak is white. Look-alikes include jade (nephrite and jadeite), which is much harder and tougher, and soapstone, which is even softer and dominated by talc. Marble is harder than typical serpentinite and fizzes in acid, whereas serpentinite does not react. Some serpentinite contains fibrous chrysotile (a form of asbestos), so handle dusty or fibrous specimens with care.

Uses & significance

Serpentinite is widely used as an ornamental and architectural stone for tiles, countertops, and facing slabs, often sold as 'green marble' or verd antique. Its softness makes it popular for carving figurines, bowls, and beads.

In the gem and metaphysical trade, attractive translucent varieties are cut as 'new jade' or 'healerite.' Industrially, magnesium-rich serpentinite is a source of magnesium and is studied for carbon sequestration. Historically chrysotile serpentinite was mined for asbestos, an application now largely abandoned for health reasons. Metaphysically it is associated with earth connection and healing, though such claims are not scientifically verified.

Frequently asked questions

Is serpentinite the same as serpentine?

Not exactly. Serpentine refers to the group of minerals, while serpentinite is the rock made mostly of those minerals. In the lapidary trade the names are often used interchangeably.

Is serpentinite dangerous because of asbestos?

Some serpentinite contains chrysotile, a fibrous asbestos mineral. Solid, polished pieces are generally safe to handle, but cutting, grinding, or breathing dust from fibrous specimens should be avoided.

Can serpentinite be mistaken for jade?

Yes, translucent green serpentinite is often sold as 'new jade.' True jade is far harder and tougher; serpentinite can be scratched with a knife while jade cannot.

Why is serpentinite green?

Its green color comes from iron and the serpentine minerals themselves. Black flecks are usually magnetite or chromite, and white veins are often calcite or additional serpentine.

Serpentinite identified by the community

Real specimens identified with Rock Identifier.

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