Rock Identifier
Likely polished green serpentine or aventurine (Serpentine-group minerals, commonly antigorite/lizardite; alternatively quartz-rich green aventurine) — mineral
mineral

Likely polished green serpentine or aventurine

Serpentine-group minerals, commonly antigorite/lizardite; alternatively quartz-rich green aventurine

AI-generated identification · may be incorrect

Small rounded specimen with dark olive-green color and glittery surface, likely polished or wet. Serpentine has Mohs hardness 2.5–4, waxy to greasy luster, poor cleavage, and specific gravity about 2.5–2.6; aventurine is harder, about 6.5–7, with quartz’s vitreous luster.

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Physical properties

Small rounded specimen with dark olive-green color and glittery surface, likely polished or wet. Serpentine has Mohs hardness 2.5–4, waxy to greasy luster, poor cleavage, and specific gravity about 2.5–2.6; aventurine is harder, about 6.5–7, with quartz’s vitreous luster.

Formation & geological history

Serpentine forms when ultramafic rocks such as peridotite undergo hydrothermal alteration, commonly during mountain-building; aventurine forms in silica-rich veins or metamorphic rocks. Exact age cannot be determined from the image.

Uses & applications

Serpentine is used for carvings, ornamental stone, and historically some architectural materials; green aventurine is used for beads, cabochons, and inexpensive jewelry.

Geological facts

The glitter may come from magnetite, mica, or polished reflective mineral grains. Serpentine can resemble jade but is generally softer and less dense.

Field identification & locations

Field tests are useful: serpentine is relatively soft and may scratch with a steel knife, whereas aventurine will not; a close inspection or hardness test is needed for confident identification. Common sources include California, Italy, New Zealand, Canada, and Russia.