Rock Identifier
Tumbled green-gray stone, likely prehnite or serpentine (Likely prehnite, Ca₂Al₂Si₃O₁₀(OH)₂; identification is uncertain from the photograph) — mineral
mineral

Tumbled green-gray stone, likely prehnite or serpentine

Likely prehnite, Ca₂Al₂Si₃O₁₀(OH)₂; identification is uncertain from the photograph

AI-generated identification · may be incorrect

Pale green-gray, opaque to translucent, with a dull-to-waxy luster and rounded tumbled form; likely Mohs 6–6.5 if prehnite, or 2.5–4 if serpentine. No visible crystal faces or cleavage are apparent.

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Physical properties

Pale green-gray, opaque to translucent, with a dull-to-waxy luster and rounded tumbled form; likely Mohs 6–6.5 if prehnite, or 2.5–4 if serpentine. No visible crystal faces or cleavage are apparent.

Formation & geological history

Prehnite forms in low-temperature hydrothermal veins and cavities of basaltic rocks, commonly during alteration of volcanic rocks; many deposits are Mesozoic to younger. Serpentine instead forms by hydration of ultramafic mantle rocks.

Uses & applications

Used as a lapidary stone, cabochon, bead, and collector specimen; not generally used for construction in this small polished form.

Geological facts

Prehnite commonly shows pale green color and botryoidal or fibrous interiors, sometimes with darker inclusions. A hardness or specific-gravity test is needed to distinguish it from serpentine, jade, or dyed quartz.

Field identification & locations

Common sources include Australia, South Africa, China, India, and the United States. Check streak, hardness, translucency, and heft; avoid relying on color alone because the image is insufficient for confident identification.