
metamorphic
Likely serpentinite (greenstone pebble)
Serpentinite, composed mainly of serpentine-group minerals (e.g., lizardite, chrysotile, or antigorite)
AI-generated identification · may be incorrectOlive-green with dark veins and a mottled, waxy-to-dull surface; serpentine minerals are Mohs 2.5–5.5, generally monoclinic or platy/fibrous. The image is not sharp enough to confirm mineral composition or hardness.
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Physical properties
Olive-green with dark veins and a mottled, waxy-to-dull surface; serpentine minerals are Mohs 2.5–5.5, generally monoclinic or platy/fibrous. The image is not sharp enough to confirm mineral composition or hardness.
Formation & geological history
Forms when water alters magnesium-rich ultramafic rocks, commonly during seafloor or subduction-zone metamorphism; its age depends on the source rock and cannot be determined from the photo.
Uses & applications
Serpentinite is used as decorative stone, carving material, and sometimes as a source of talc or asbestos-bearing minerals; this small pebble is primarily a collector specimen.
Geological facts
Green color and dark veining are common in serpentinite, but similar appearances occur in other altered rocks and minerals.
Field identification & locations
Look for a green, often waxy surface and softer, slick-feeling material; confirm with hardness and streak tests, since appearance alone is inconclusive. Serpentinite occurs in ultramafic belts worldwide.
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