Smithsonite is a classic secondary mineral in oxidized ore deposits, forming characteristic platy to massive crystal aggregates. This unique flat originates from Laurion, Greece, a historic mining district renowned since antiquity for its rich lead and zinc resources.
The specimens exhibit well-developed crystal habits with sharp outlines and strong matrix attachment. Collectors value Smithsonite from Laurion for its documented provenance and classic paragenesis alongside other secondary minerals. The sturdy matrix bond allows secure handling and impressive showcase display.
This one-of-a-kind flat makes an excellent addition to systematic collections focused on notable localities and reference materials. It is equally suited for educational exhibits and high-end display cabinets—offering a valuable piece of Greece’s mining and geological heritage.