
metamorphic
Green serpentine (likely serpentinite)
Serpentine-group minerals, commonly antigorite, lizardite, and/or chrysotile; rock name: serpentinite
AI-generated identification · may be incorrectSmall, rounded green specimen with mottled dark and pale areas and a waxy to slightly glossy luster. Serpentine minerals are typically Mohs 2.5–5.5, monoclinic or platy/fibrous, with variable cleavage; exact hardness and composition cannot be confirmed from the photo.
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Physical properties
Small, rounded green specimen with mottled dark and pale areas and a waxy to slightly glossy luster. Serpentine minerals are typically Mohs 2.5–5.5, monoclinic or platy/fibrous, with variable cleavage; exact hardness and composition cannot be confirmed from the photo.
Formation & geological history
Forms when water alters magnesium-rich ultramafic rocks, commonly at tectonic plate boundaries; the specimen’s age and locality cannot be determined from appearance alone.
Uses & applications
Serpentinite is used as decorative stone, carving material, and sometimes in jewelry; this small specimen is mainly suited to collecting.
Geological facts
Serpentine is a mineral group rather than a single mineral, and its color ranges from pale green to nearly black.
Field identification & locations
The mottled green color and waxy-looking surface fit serpentine, but visual identification is not definitive. It occurs in serpentinite belts worldwide; avoid scratching or cutting unknown material, as some serpentinite can contain asbestos-form chrysotile.
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