MELLITE
Class : Organic compounds
Subclass : -
Crystal system : Tetragonal
Chemistry : Al2C6(COO)6 16H2O
Rarity : Rare
Mellite is a rare organic mineral appearing secondarily in lignite (and more rarely coal) deposits, its formation being linked to the organic activity of plants. From a chemical point of view, it is a natural calcium oxalate which can contain up to 45% water. Its name comes from the Greek meli (honey) in allusion to its honey-yellow color. Mellite is transparent to translucent, resinous to vitreous in luster, sometimes sectile, it has a yellowish brown to brownish color, sometimes also reddish and exhibits blue fluorescence in the short wavelengths of ultraviolet. Mellite appears in massive (grains, nodules) or pseudo-octahedral form, most often small. Its low density (1.6) allows it to be distinguished from minerals of similar appearance.
Main photo : 6 cm octahedral mellite from Csordakúti Mine, Hungary © Dávid Szabó
Mellite in the World
Twinning
No twin known for this mineral species.
Fakes and treatments
No fakes recorded for this mineral species.
Hardness : 2 to 2.5
Density : 1.64
Fracture : Conchoidal
Streak : White
TP : Translucent to transparent
RI : 1.511 to 1539
Birefringence : 0.028
Optical character : Uniaxial -
Pleochroism : Low
Fluorescence : Yellow to blue
Solubility : Nitric acid, water
Magnetism : NoneRadioactivity : None