URANOPILITE
Class : Sulfates, chromates, molybdates
Subclass : Hydrated sulfates
Crystal system : Monoclinic
Chemistry : (UO2)6(SO4)(OH)10 12H2O
Rarity : Uncommon to fairly common
Uranopilite is a hydrated uranyl sulfate that is easily soluble and therefore of ephemeral existence. It is a neoformation mineral well known in uranium mine dumps and galleries, where it crystallizes (often on timbering) by the action of sulfuric acid formed from iron sulfides on uraninite. Exposed to UV, uranopilite is highly fluorescent in a bright yellow-green color. Its name comes from its chemical composition and from the Greek pilos (felt) in reference to its appearance. Uranopilite typically occurs as bright yellow velvety coatings or encrustations of extremely fine acicular crystals on or in close proximity to uraninite. Industrial ore leaching processes (selective dissolution of certain metals by acids) recover uranium carried in acid solutions by induced crystallization of uranopilite.
Main photo : Uranopyrite from Pribram, Czech Republic © Bohuslav Bures
Uranopilite in the World
Twinning
No twinning known for this mineral species.
Fakes and treatments
No fakes listed for this mineral species.
Hardness : Undetermined
Density : 3.7 to 4
Fracture : Undetermined
Streak : Undetermined
TP : Translucent
RI : 1.621 to 1.634
Birefringence : 0.011
Optical character : Biaxial +
Pleochroism : Visible
Fluorescence : Yellow-green
Solubility : Nitric acid, hydrochloric acid, water
Magnetism : NoneRadioactivity : Very strong