Rock Identifier
Green serpentine pebble (possibly serpentine-rich rock) (Serpentinite, composed chiefly of serpentine-group minerals such as antigorite, lizardite, or chrysotile; exact identification requires testing) — metamorphic
metamorphic

Green serpentine pebble (possibly serpentine-rich rock)

Serpentinite, composed chiefly of serpentine-group minerals such as antigorite, lizardite, or chrysotile; exact identification requires testing

AI-generated identification · may be incorrect

Green, mottled, and apparently polished or naturally rounded, with a waxy to greasy luster. Serpentine minerals are typically Mohs 2.5–4 and have a fine-grained structure; cleavage is usually not visible in a small pebble. The image alone cannot establish hardness or specific gravity.

Identified More metamorphic →
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Physical properties

Green, mottled, and apparently polished or naturally rounded, with a waxy to greasy luster. Serpentine minerals are typically Mohs 2.5–4 and have a fine-grained structure; cleavage is usually not visible in a small pebble. The image alone cannot establish hardness or specific gravity.

Formation & geological history

Forms when water alters ultramafic rocks, commonly at or near tectonic plate boundaries; the age varies with the host rock and alteration event.

Uses & applications

Serpentinite is used as decorative stone, carvings, and jewelry; some varieties have been used as building stone. Avoid handling or cutting unidentified fibrous material because chrysotile asbestos may be present.

Geological facts

Serpentine is a mineral group, not one single mineral, and its distinctive green color comes from iron and other trace elements.

Field identification & locations

A smooth green surface and mottled pattern are suggestive but not diagnostic; confirm by hardness, streak, and mineralogical testing. Serpentinite occurs in ophiolites and other ultramafic terranes worldwide.