Rock Identifier
Tumbled blue-green stone, possibly chrysocolla or serpentine (Indeterminate from photograph; likely chrysocolla (hydrated copper silicate) or green serpentine (serpentine-group minerals)) — mineral
mineral

Tumbled blue-green stone, possibly chrysocolla or serpentine

Indeterminate from photograph; likely chrysocolla (hydrated copper silicate) or green serpentine (serpentine-group minerals)

AI-generated identification · may be incorrect

Smooth, polished, blue-green, opaque, with dark linear veining and a dull to waxy luster. Chrysocolla has Mohs hardness 2–4; serpentine is typically 2.5–4. Specific gravity is approximately 2.0–2.6. No crystal faces are visible.

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Physical properties

Smooth, polished, blue-green, opaque, with dark linear veining and a dull to waxy luster. Chrysocolla has Mohs hardness 2–4; serpentine is typically 2.5–4. Specific gravity is approximately 2.0–2.6. No crystal faces are visible.

Formation & geological history

Chrysocolla forms in oxidized zones of copper deposits; serpentine forms when ultramafic rocks are hydrothermally altered. The specimen is likely tumbled or naturally water-worn, so its geological age cannot be determined visually.

Uses & applications

Used as a lapidary stone, cabochon, bead, or decorative specimen. Chrysocolla is generally too soft for everyday rings; serpentine is used ornamentally and sometimes carved.

Geological facts

The color may also indicate dyed howlite, turquoise, or a mixture such as chrysocolla-bearing quartz. A hardness test and copper-related color zoning would help distinguish possibilities.

Field identification & locations

The Veracruz region near 18.8°N, 95.8°W contains volcanic and hydrothermal rocks, making copper minerals plausible, though this small polished stone cannot be confidently localized. Avoid scratching glass unless testing: chrysocolla and serpentine usually scratch with a steel blade, while turquoise generally does not.