PARALAURIONITE
Class : Halides
Subclass : Oxychlorides
Crystal system : Monoclinic
Chemistry : PbCl(OH)
Rarity : Rare
Paralaurionite is a chloride from the surface oxidation zone of lead deposits. Its formation requires chlorine : it is therefore found in environments located near the marine coast or in closed evaporite basins. It is also found in certain industrial slags. Its name comes from the Greek para (near) and its dimorphic relationship with laurionite. Paralaurionite forms lamellar to tabular crystals, sometimes elongated, white to grayish, sometimes yellowish, with a strong adamantine luster. It is associated with other secondary lead minerals including abundant chlorides (penfieldite, phosgenite, etc...).
Main photo : Paralaurionite from Lavrion, Greece © Henry Minot
Paralaurionite in the World
Twinning
Contact twins on {100} are common, forming crystals with an orthorhombic appearance.
Fakes and treatments
No fakes listed for this mineral species.
Hardness : 3
Density : 6.15
Fracture : Undetermined
Streak : White
TP : Translucent to transparent
RI : 2.050 to 2.200
Birefringence : 0.150
Optical character : Biaxial -
Pleochroism : Visible
Fluorescence : None
Solubility : Nitric acid
Magnetism : NoneRadioactivity : None