PLUMBOGUMMITE
Class : Phosphates, arsenates, vanadates
Subclass : Hydrated phosphates
Crystal system : Trigonal
Chemistry : PbAl3(PO4)2(OH)5 H2O
Rarity : Uncommon
Plumbogummite is an hydrated phosphate from the oxidation zone of lead deposits, found in association with other secondary lead minerals and sometimes in replacement of pyromorphite or barite (pseudomorph). Its name comes from the Latin plumbum (lead) and gummi (gum) in allusion to its chemical composition and its appearance. Plumbogummite occurs in botryoidal, stalactitic and spherolitic masses with a concentric or fibroradiated texture, rarely in prismatic crystals with a hexagonal shape. Its color is extremely variable : gray-white, yellowish gray to reddish brown, sometimes green or blue.
Main photo : Plumbogummite from Yangshuo Mine, Guangxi, China © Rob Lavinsky
Plumbogummite in the World
Twinning
No twins known for this mineral species.
Fakes and treatments
No fakes listed for this mineral species.
Hardness : 4 to 5
Density : 4.01
Fracture : Irregular to sub-conchoidal
Streak : White
TP : Translucent
RI : 1.653 to 1.704
Birefringence : 0.022
Optical character : Uniaxial +
Pleochroism : Low
Fluorescence : Rarely bluish
Solubility : Acids
Magnetism : NoneRadioactivity : None