
metamorphic
Banded green stone, likely serpentinite
Serpentinite (rock composed chiefly of serpentine-group minerals; exact identification requires testing)
AI-generated identification · may be incorrectDark green to gray-green with pale parallel bands and a dull to slightly waxy luster; serpentinite is commonly soft (about 2.5–4 Mohs), but hardness and banding vary with accessory minerals. The specimen appears naturally fractured and may show foliation or veining.
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Physical properties
Dark green to gray-green with pale parallel bands and a dull to slightly waxy luster; serpentinite is commonly soft (about 2.5–4 Mohs), but hardness and banding vary with accessory minerals. The specimen appears naturally fractured and may show foliation or veining.
Formation & geological history
Forms when water alters ultramafic rocks, especially peridotite, during metamorphism; it can occur in ancient and modern tectonic plate-boundary settings. The image does not establish its age or exact locality.
Uses & applications
Serpentinite is used as decorative stone, carvings, and occasionally dimension stone; identification is needed before assigning a specific commercial use.
Geological facts
The green color commonly comes from serpentine minerals, sometimes with magnetite or other dark accessories. Similar-looking banded rocks include green schist and other metamorphic stones.
Field identification & locations
Look for a green color, waxy feel, relatively low hardness, and veins or mesh-like alteration texture; avoid relying on color alone. Serpentinite occurs in many mountain belts and ophiolite complexes.
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