
metamorphic
Tumbled serpentine (likely nephrite-like greenstone)
Serpentine-group minerals, chiefly antigorite/lizardite; possibly mixed with tremolite-actinolite
AI-generated identification · may be incorrectGreen to olive-brown, waxy to subvitreous luster, opaque, and smoothly polished; Mohs hardness about 2.5–5.5, with no obvious cleavage and commonly massive, mottled veining. The pale fibrous bands and translucency suggest serpentine or a related greenstone rather than jade certainty.
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Physical properties
Green to olive-brown, waxy to subvitreous luster, opaque, and smoothly polished; Mohs hardness about 2.5–5.5, with no obvious cleavage and commonly massive, mottled veining. The pale fibrous bands and translucency suggest serpentine or a related greenstone rather than jade certainty.
Formation & geological history
Forms when ultramafic mantle rocks undergo low-temperature hydration and metamorphism, commonly in tectonic shear zones and ophiolites. Most specimens are geologically Paleozoic to Mesozoic or younger, depending on locality.
Uses & applications
Used as decorative stone, carvings, cabochons, beads, and polished collectibles; serpentine is also used occasionally as an architectural stone. It should not be marketed as jade without laboratory testing.
Geological facts
Serpentine can resemble jade, especially when polished, but is generally softer and less tough. Some varieties may contain trace chrysotile asbestos, so avoid cutting, drilling, or creating dust unless composition is confirmed.
Field identification & locations
Common sources include California, Vermont, New Zealand, Italy, and Afghanistan. Check hardness, heft, translucency, and toughness; a gemological or mineralogical test is needed to distinguish it from nephrite jade.
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