
metamorphic
Serpentine-rich rock (likely antigorite serpentinite)
Serpentinite, composed mainly of serpentine-group minerals such as antigorite, lizardite, or chrysotile
AI-generated identification · may be incorrectPale yellow-green with dark gray veining and a dull to waxy luster; serpentine minerals have Mohs hardness about 2.5–4 and commonly form fine-grained, massive aggregates. The visible specimen is too small to assess texture or confirm its mineral identity reliably.
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Physical properties
Pale yellow-green with dark gray veining and a dull to waxy luster; serpentine minerals have Mohs hardness about 2.5–4 and commonly form fine-grained, massive aggregates. The visible specimen is too small to assess texture or confirm its mineral identity reliably.
Formation & geological history
Forms when water alters magnesium-rich mantle rocks, commonly peridotite, during serpentinization; this process occurs in oceanic crust and along tectonic plate boundaries. The age depends on the locality and cannot be determined from the image.
Uses & applications
Serpentinite is used as decorative stone, carved objects, and sometimes dimension stone; mineral identification is needed before handling or working it because some serpentinites contain asbestos-form chrysotile.
Geological facts
The contrasting gray material may be another mineral or host rock, but the image alone does not establish its identity. Serpentinite often shows mottled green colors and a smooth, soapy feel.
Field identification & locations
Look for green coloration, waxy surfaces, and association with ultramafic rocks in tectonic or mountain belts. A scratch test and mineralogical analysis can help distinguish it from other pale-green rocks.
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