Columbite

Columbite specimens for sale

29 for sale · $120–$7,500 USD

34 in the gallery

Columbite is a niobium-rich mineral with the formula Fe2+Nb2O6, typically forming elongated, prismatic crystals and brownish-black to steel-gray metallic luster. It often occurs in granular to massive aggregates within pegmatites and granitic rocks, and can display a submetallic to adamantine sheen on sharper faces. Associated minerals in pegmatites include tantalite and various spodumene-bearing assemblages, reflecting its geological environment.

Formula
Fe2+Nb2O6
Rarity
Common
Stability
Stable
Collector interest
Moderate Interest
Classification notes
Oxide mineral; niobate group; Nb-oxide (IMA: Columbite)

Buy Columbite specimens

View all 29
Columbite image
Columbite
Crystal Classics
Updated 3d ago
$150
Columbite image
Columbite
Crystal Classics
Updated 3d ago
$150
Columbite image
Columbite
Crystal Classics
Updated 3d ago
$150
Columbite image
Columbite
Crystal Classics
Updated 3d ago
$7,500
Columbite image
Columbite
Crystal Classics
Updated 3d ago
$7,500
Columbite image
Columbite
Crystal Classics
Updated 3d ago
$7,500
Columbite image
Columbite
Crystal Classics
Updated 3d ago
$950
Columbite image
Columbite
Crystal Classics
Updated 3d ago
$950
Columbite image
Columbite
Crystal Classics
Updated 3d ago
$950
Columbite image
Columbite
Crystal Classics
Updated 3d ago
$7,500
Columbite image
Columbite
Crystal Classics
Updated 3d ago
$7,500
Columbite image
Columbite
Crystal Classics
Updated 3d ago
$7,500

Where Columbite is found

About Columbite

Prominent specimens come from classic pegmatite deposits in the United States, notably in Alaska and Ontario-like contexts, as well as famous occurrences in Brazil and Madagascar. Lesser-known but scientifically valuable finds come from Afghanistan and Australia, contributing to the mineral’s diversity in habit and size. Collectors value well-formed crystals, durability, and the contrast between a dark body and bright luster, as well as the insight Columbite provides into niobium-bearing mineral systems and pegmatite genesis.