
metamorphic
Likely pale green jasper or serpentine-bearing stone
Uncertain; possibly serpentinized ultramafic rock (serpentinite) or green jasper, mainly serpentine-group minerals or microcrystalline quartz
AI-generated identification · may be incorrectLight gray-green, opaque, with reddish-brown veins and a dull to waxy luster; hardness is approximately 3–6 depending on composition. Massive, fine-grained texture; no obvious cleavage or visible crystals.
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Physical properties
Light gray-green, opaque, with reddish-brown veins and a dull to waxy luster; hardness is approximately 3–6 depending on composition. Massive, fine-grained texture; no obvious cleavage or visible crystals.
Formation & geological history
If serpentinite, it formed when mantle peridotite was hydrated during tectonic alteration, commonly in ophiolite zones; if jasper, silica-rich fluids cemented or replaced rock. An exact age cannot be determined from the image.
Uses & applications
Decorative carving, cabochons, and inexpensive collecting specimens; serpentinite is also used as ornamental stone, while jasper is used in beads and polished objects.
Geological facts
The reddish veins may represent iron oxides, while the green body commonly indicates serpentine minerals or chlorite. Visual identification alone cannot reliably distinguish these materials.
Field identification & locations
Look for a smooth waxy feel, green mottling, and red veining; serpentinite is softer and may scratch with a steel knife, whereas jasper generally resists scratching. Common sources include California, Italy, New Zealand, Canada, and ophiolite belts worldwide.
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