COLUMBITE
, a rare See also:mineral consisting of See also:iron niobate, FeNb206, in which the iron and niobium are replaced by varying amounts of See also:manganese and See also:tantalum respectively, the See also:general See also:formula being (Fe, Mn) (Nb, Ta)206
.
It was in this mineral that
See also:Charles Iatchett discovered, in 18or, the See also:element niobium, which he himself called See also:columbium after the See also:country (See also:Columbia or See also:America) whence came the specimen in the See also:British Museum collection which he examined
.
The See also:species . has also been called niobite
.
It crystallizes in the orthorhombic See also:system, and the See also: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 See also:face marked See also: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 See also: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 See also:granite and See also:pegmatite at Rabenstein in See also:Lower See also:Bavaria,
the Ilmen Mountains in the Urals, Haddam in See also:Connecticut, and several other localities in the See also:United States; also in the See also:cryolite of See also:Greenland
.
Tantalite is from See also:Finland, and it has recently been found in some abundance in the deposits of cassiterite in the See also:tin-See also:- FIELD (a word common to many West German languages, cf. Ger. Feld, Dutch veld, possibly cognate with O.E. f olde, the earth, and ultimately with root of the Gr. irAaror, broad)
- FIELD, CYRUS WEST (1819-1892)
- FIELD, DAVID DUDLEY (18o5-1894)
- FIELD, EUGENE (1850-1895)
- FIELD, FREDERICK (18o1—1885)
- FIELD, HENRY MARTYN (1822-1907)
- FIELD, JOHN (1782—1837)
- FIELD, MARSHALL (183 1906)
- FIELD, NATHAN (1587—1633)
- FIELD, STEPHEN JOHNSON (1816-1899)
- FIELD, WILLIAM VENTRIS FIELD, BARON (1813-1907)
field of Greenbushes in the See also:Blackwood See also:district, Western See also:Australia
.
Dimorphous with columbite and tantalite are the tetragonal minerals tapiolite (= skogbolite) and mossite, so that the four See also:form an isodimorphous See also:group with the general formula (Fe, Mn) (Nb, Ta)20s
.
Mossite is from a pegmatite vein near See also:Moss in See also:Norway, and tapiolite is from Finland
.
All these minerals contain tin in small amount
.
(L
.
J
.
End of Article: