Rock Identifier
Likely polished green aventurine or serpentine pebble (Quartz-rich aventurine (SiO₂) or serpentine-group mineral; exact identification requires testing) — mineral
mineral

Likely polished green aventurine or serpentine pebble

Quartz-rich aventurine (SiO₂) or serpentine-group mineral; exact identification requires testing

AI-generated identification · may be incorrect

Small rounded, polished dark green-gray specimen with pale reflective speckles and a subdued vitreous-to-waxy luster. Aventurine is Mohs 6.5–7 with no obvious cleavage; serpentine is softer, Mohs 2.5–5.5, and commonly waxy.

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Physical properties

Small rounded, polished dark green-gray specimen with pale reflective speckles and a subdued vitreous-to-waxy luster. Aventurine is Mohs 6.5–7 with no obvious cleavage; serpentine is softer, Mohs 2.5–5.5, and commonly waxy.

Formation & geological history

Aventurine forms when quartz crystallizes with mica or other inclusions, commonly in metamorphic veins; serpentine forms by hydration of ultramafic rocks. Precise age and origin cannot be determined visually.

Uses & applications

Used for beads, cabochons, carvings, ornaments, and lapidary tumbling; serpentine is also a decorative building stone.

Geological facts

The glittering effect in aventurine is called aventurescence, caused mainly by included mica or hematite. A strong steel-scratch resistance favors aventurine over serpentine.

Field identification & locations

Common sources include India, Brazil, Russia, and Zimbabwe for green aventurine; serpentine occurs worldwide. Test inconspicuously with a steel blade, inspect streak/powder, and use a refractometer or Raman/XRF for confirmation.