ILMENORUTILE
Class : Oxides and hydroxides
Subclass : Oxides
Crystal system : Tetragonal
Chemistry : (Ti,Nb,Fe)TiO3
Rarity : Uncommon
Ilmenorutile is an oxide of titanium, niobium and iron from granitic pegmatites, carbonatites and alluvial placers in which its inalterability ensures good conservation. It is considered a variety of rutile by the IMA. Ilmenorutile often contains tantalum and forms a series with strüverite, with tantalum dominating niobium. Its name comes from its place of discovery, the Ilmen Mountains (Russia) and its composition close to that of rutile. Ilmenorutile occurs in bipyramidal prismatic crystals, black in color, very frequently in intergrowth with columbite, sometimes ilmenite.
Main photo : Ilmenorutile from Tulare County, California, USA © Rob Lavinsky
Ilmenorutile in the World
Twinning
No twins known for this mineral species.
Fakes and treatments
No fakes recorded for this mineral species.
Hardness : 6 to 6.5
Density : 4.23
Fracture : Conchoidal
Streak : Black
TP : Opaque
RI : -
Birefringence : -
Optical character : -
Pleochroism : None
Fluorescence : None
Solubility : -
Magnetism : ParamagneticRadioactivity : None to very low