THAUMASITE
Class : Sulfates, chromates, molybdates
Subclass : Hydrated sulfates
Crystal system : Hexagonal
Chemistry : Ca3Si(SO4)(CO3)(OH)6 12H2O
Rarity : Uncommon
Thaumasite is a mineral whose place in the classification remains debated : complex sulfates for some, silicates admitting SO4 and CO3 groups for others. The position of the silicon atoms at the center of the octahedron and not in the framework of SiO4 tetrahedra argues in favor of belonging to the sulfates ; it is then integrated into the ettringite group. It is a late mineral present in sulfide deposits, in contact metamorphic rocks, and also a reaction product of geothermal or marine waters on basalts and tuffs. Its name comes from the Greek thaumazein (to be surprised), because of its very particular chemical composition. Thaumasite rarely forms acicular prismatic crystals grouped in fibroradiate aggregates, it occurs more readily in powdery masses. It is colorless, white or slightly yellowish. It is sometimes cut as a fine gemstone.
Main photo : Thaumasite from N'Chwaning II Mine, South Africa © Chris Emproto
Thaumasite in the World
Twinning
No twinning known for this mineral species.
Fakes and treatments
No fakes listed for this mineral species.
Hardness : 3.5
Density : 1.877
Fracture : Sub-conchoidal
Streak : White
TP : Translucent to transparent
RI : 1.468 to 1.507
Birefringence : 0.039
Optical character : Uniaxial -
Pleochroism : None
Fluorescence : None
Solubility : -
Magnetism : NoneRadioactivity : None