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Encyclopedia Britannica



COLUMBITE

This article appears in Volume V06, Page 740 of the Encyclopedia Britannica.

Encyclopedia Britannica - Main :: CLI-COM
COLUMBITE , a rare
mineral
  consisting of iron niobate, FeNb206, in which the iron and niobium are replaced by varying amounts of manganese and
tantalum
  respectively, the general
formula
  being (Fe, Mn) (Nb, Ta)206. It was in this
mineral
  that
Charles Iatchett discovered, in 18or, the
element
  niobium, which he himself called columbium after the country (Columbia or America) whence came the specimen in the British Museum collection which he examined. The species . has also been called niobite. It crystallizes in the orthorhombic
system
 , and the black, opaque crystals are often very
brilliant with a sub-metallic lustre. Twinned crystals are not uncommon, and there is a distinct cleavage parallel to the face marked bin the figure. Hardness 6; specific gravity 5.3. With increasing amount of
tantalum
  the specific gravity increases up to 7.3, and members at this end of the
series
  are known as tantalite (FeTa2O6). Specimens in which the iron is largely replaced by manganese are known as manganocolumbite or manganotantalite, according as they contain more niobium or more tantalum. Columbite occurs as crystals and compact masses in granite and pegmatite at Rabenstein in Lower Bavaria,
the Ilmen Mountains in the Urals, Haddam in Connecticut, and several other localities in the United States; also in the cryolite of Greenland. Tantalite is from
Finland
 , and it has recently been found in some abundance in the deposits of cassiterite in the tin-field of Greenbushes in the Blackwood
district
 , Western Australia.
Dimorphous with columbite and tantalite are the tetragonal minerals tapiolite (= skogbolite) and mossite, so that the four form an isodimorphous group with the general
formula
  (Fe, Mn) (Nb, Ta)20s. Mossite is from a pegmatite vein near
Moss
  in Norway, and tapiolite is from
Finland
 . All these minerals contain tin in small amount. (L. J. S.)


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