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alleghanyite is dimorphous (having the same chemical composition but a different atomic structure) with ribbeite and forms a series with chondrodite [(Mg,Fe2+)5(SiO4)2(F,OH)2] – both minerals of the humite group. It forms as a hydrothermal mineral in manganese-rich veins and it is typically associated with a wide range of other manganese minerals, particularly silicates and oxides.
the occurrence of alleghanyite in Wales is restricted to the manganese ore deposits at Benallt Mine, Llŷn. The ore minerals are believed to have been derived from hydrothermal activity involving manganese-rich fluids exhaled onto the Ordovician sea floor (Brown & Evans, 1989).