5.1" Botryoidal Smithsonite Pseudomorph After Scalenohedral Calcite

Botryoidal Smithsonite Pseudomorph After Scalenohedral Calcite #211289

This is a gorgeous specimen of botryoidal smithsonite that formed as a pseudomorph after scalenohedral calcite. It comes out of the San Giovanni mine in Sardinia, Italy, and measures 5.1" wide. The layered smithsonite is visible where two terminations broke away, along the periphery of the specimen. Empty pockets where the calcite dissolved away can be found beneath the smithsonite.

It comes with an acrylic display stand.

Smithsonite forms in earthy botryoidal masses, sometimes forming grape-like structures. It can be found as a secondary mineral in oxidation zones of zinc ore deposits, in some sedimentary deposits, and as an oxidation product of sphalerite. The general chemical formula of smithsonite is ZnCO3, however Fe (iron), Mg (magnesium), Ca (calcium), Cd (cadmium), Cu (copper), and Co (cobalt) can take the place of Zn (zinc). This potential for elemental variation results in smithsonite's wide variety of colors, including blue, green, yellow, orange, pink, purple, brown, gray, white, and colorless.

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