
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 incorrectGreen, 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.
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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.
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