Rock Identifier
Serpentine-rich metamorphic rock (Serpentinite; chiefly antigorite/lizardite Mg₃Si₂O₅(OH)₄, possibly with talc, chlorite, magnetite, or carbonate) — metamorphic
metamorphic

Serpentine-rich metamorphic rock

Serpentinite; chiefly antigorite/lizardite Mg₃Si₂O₅(OH)₄, possibly with talc, chlorite, magnetite, or carbonate

AI-generated identification · may be incorrect

Pale gray-green, mottled, dull to waxy luster, massive and fine-grained with no obvious crystals; Mohs hardness about 2.5–4, commonly low-to-moderate density. The image is consistent with serpentine but cannot confirm exact mineralogy visually.

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Physical properties

Pale gray-green, mottled, dull to waxy luster, massive and fine-grained with no obvious crystals; Mohs hardness about 2.5–4, commonly low-to-moderate density. The image is consistent with serpentine but cannot confirm exact mineralogy visually.

Formation & geological history

Forms when ultramafic mantle rocks such as peridotite hydrate during low-temperature metamorphism, commonly along faults and oceanic crust; ages range from Precambrian to modern tectonic settings.

Uses & applications

Used as decorative stone, carving material, countertops, and historically as a source of asbestos-group serpentine fibers; attractive polished pieces are collected.

Geological facts

Serpentinite may contain magnetite and can show weak magnetism. Fibrous varieties may contain chrysotile, so avoid cutting, sanding, or creating dust without testing and proper controls.

Field identification & locations

Common in ophiolites and subduction-zone mélanges, including California, Italy, New Zealand, and the Appalachians. Field clues are green color, waxy feel, softness, and reaction generally absent or weak with dilute acid.