Rock Identifier
Likely tumbled green mineral (possibly serpentine or aventurine) (Indeterminate; possibilities include serpentine-group minerals, nephrite, or green aventurine quartz) — mineral
mineral

Likely tumbled green mineral (possibly serpentine or aventurine)

Indeterminate; possibilities include serpentine-group minerals, nephrite, or green aventurine quartz

AI-generated identification · may be incorrect

Smooth, rounded, opaque pale green surface with a waxy to dull luster; the image is too blurred to assess grains, cleavage, or crystal structure. Estimated hardness is roughly 2.5–7, depending on identity; a scratch test is needed.

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Physical properties

Smooth, rounded, opaque pale green surface with a waxy to dull luster; the image is too blurred to assess grains, cleavage, or crystal structure. Estimated hardness is roughly 2.5–7, depending on identity; a scratch test is needed.

Formation & geological history

Green serpentine forms by hydrothermal alteration of ultramafic rocks; nephrite forms in metamorphic zones; aventurine is quartzite containing fuchsite mica. These materials range from Precambrian to much younger geological ages.

Uses & applications

Commonly sold as tumbled stones, carvings, beads, and decorative pieces; nephrite and high-quality aventurine can have jewelry value, while common serpentine is inexpensive.

Geological facts

The specimen appears human-tumbled or polished rather than naturally weathered. Its uniform green color is compatible with several materials, and the photograph does not support a confident species-level identification.

Field identification & locations

Near 19.1°N, 72.9°E, weathered basalt, laterite, and imported decorative stones are more plausible than a rare gem deposit. Check streak, hardness, translucency, and a close-focus image: quartz-rich aventurine scratches glass, nephrite is tough and waxy, while serpentine is softer and is often scratched by a steel blade.