HUBNERITE


Hubnerite belongs to a series with another mineral, Ferberite, FeWO4. Hubnerite is the Manganese rich end member while ferberite is the iron rich end member. Wolframite is the name of the series and the name applied to indistinguishable specimens and specimens intermediate between the two end members. Most specimens found in nature fall within 20 - 80% range of the series and these are termed wolframites, (Fe,Mn)WO4. Only if they are more pure than 80% manganese are they called Hubnerite. Hubnerite is more common than ferberite but not nearly as common as wolframite. The iron in wolframite and ferberite cause much of the differences between them and Hubnerite. Hubnerite tends to be light in color, with a lighter streak, more transparent and less dense. Ferberite, however, tends to be black colored, with a black streak, is opaque with a nearly submetallic luster, is denser and weakly magnetic. Wolframite is of course intermediate in characteristics.

Hubnerite can make a valuable and attractive specimen when associated with clear quartz clusters.

PHYSICAL CHARACTERISTICS:

 



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