Blocky Black Tantalite
OXIDES; MULTIPLE OXIDES · ORTHORHOMBIC

Tantalite

Ferrotantalite: (Fe,Mn)(Ta,Nb)2O6
Manganotantalite: (Mn,Fe)(Ta,Nb)2O6Magnesiotantalite: (Mg,Mn,Fe)(Ta,Nb)2O6

Hardness
6–6.5
Streak
Dark red, dark brown, black
Spec. Gravity
6.5–8.3
System
Orthorhombic

About

Tantalite forms a solid solution series with Columbite known as the Columbite-Tantalite series. Tantalite is the tantalum-rich member, and Columbite is the niobium-rich member. Tantalite is named after its tantalum content, and, together with Columbite, are the most important minerals containing the rare element tantalum.
The name Tantalite has been discredited by the IMA, with the more specific designations of Tantalite-(Fe) (also known as Ferrotantalite), and Tantalite-(Mn) (also known as Manganotantalite) being used for this mineral's IMA-accepted nomenclature. Ferrotantalite is always dark and opaque; Manganotantalite is usually reddish-brown and may exhibit transparency. An even rarer member of this series is Tantalite-(Mg) (Magnesiotantalite), a magnesium-rich member. In general, despite being discredited, the name Tantalite is still used without further designation, and often it is simply labelled as Columbite-Tantalite, since the exact species can be difficult to determine.

Crystal Forms & Aggregates

In prismatic and tabular crystals, often with a somewhat flattened or blocky appearance. Crystals may be striated or have growth patterns, and sometimes have complex terminations including uneven tapering habits and pyramidal. Crystals are often crudely formed, and may have undefined faces. Also bladed, grainy, and massive.

Striking Features

Environment

Polymorphs

Tapiolite

Uses

Tantalite is as an ore of the rare elements tantalum and niobium.

Noteworthy Localities

Localities for Tantalite are pretty much the same as Columbite, and it often is not identified individually but more generally as Columbite-Tantalite. Specific localities that have produced exceptional Tantalite include the São Pedro Mine, Malacacheta, Minas Gerais, Brazil, where it was found in blocky crystals; the Shigar Valley, Skardu, Gilgit-Baltistan, Pakistan, as pseudomorphs of Microlite; and Ankole, Mbarara District, Uganda; where the manganese-rich end member has been found in dark red, translucent crystals.

Common Mineral Associations

Distinguishing Similar Minerals

Crystal forms

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Modified Tabular