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Västerby, Askersund, Närke, Sweden
© Rob Lavinsky
Fine-grained pseudomorphs after silicate minerals, especially cordierite, nepheline and scapolite. Mineralogically, "pinite" is primarily composed of mica (usually muscovite) and clay group minerals.
First reported from Pini adit, Aue, Erzgebirge, Saxony, Germany.
(TL) indicates type locality. ? indicates mineral may be doubtful at this locality. All other localities listed without reference should be considered as uncertain and unproven until references can be found.
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