Rock Identifier
Tumbled green stone, possibly serpentine or aventurine (Serpentine-group minerals (mainly antigorite/lizardite) or quartz-rich green aventurine; image insufficient for certainty) — mineral
mineral

Tumbled green stone, possibly serpentine or aventurine

Serpentine-group minerals (mainly antigorite/lizardite) or quartz-rich green aventurine; image insufficient for certainty

AI-generated identification · may be incorrect

Small, rounded and polished, dark to medium green with a waxy-to-glassy luster. Serpentine is Mohs 2.5–4 and commonly massive with no visible cleavage; aventurine is quartz (Mohs 7) and may show mica sparkle. Specific gravity is roughly 2.5–2.7.

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Physical properties

Small, rounded and polished, dark to medium green with a waxy-to-glassy luster. Serpentine is Mohs 2.5–4 and commonly massive with no visible cleavage; aventurine is quartz (Mohs 7) and may show mica sparkle. Specific gravity is roughly 2.5–2.7.

Formation & geological history

Serpentine forms when ultramafic rocks hydrate during hydrothermal alteration; aventurine forms when quartz crystallizes with green mica or fuchsite. Both are geologically common, including in central Europe, but age cannot be determined from this photo.

Uses & applications

Used as tumbled stones, carvings, ornamental stone, and occasionally jewelry; serpentine is also used decoratively in slabs, while aventurine is popular for inexpensive cabochons.

Geological facts

The smooth shape indicates human tumbling or natural abrasion. A steel scratch test can help: serpentine scratches relatively easily, whereas quartz-rich aventurine does not.

Field identification & locations

The specimen is visually more consistent with polished serpentine than aventurine because it appears uniformly waxy and lacks obvious glitter. In the Thuringia area, serpentinized ultramafic rocks are a plausible regional source; confirm with hardness, streak, and a close examination for mica sparkle.