NATRON

    Class : Carbonates, nitrates, borates
    Subclass : Hydrated carbonates
    Crystal system : Monoclinic
    Chemistry : Na2CO3 10H2O
    Rarity : Uncommon to fairly common


Natron is mainly a mineral of evaporitic origin, sometimes present, but more rarely, in volcanic solfataras (Etna, Vesuvius, Italy). It is a hydrated sodium carbonate that forms during the evaporation of sodium-rich lakes (Searles Lake, California, Gobi Desert, China and Mongolia), associated with thermonatrite, trona, gaylussite and calcite. Natron is a very fragile mineral : easily soluble and easily dehydrated to thermonatrite in dry air. Its name comes from the Arabic natrun which designated rock salt, it is a mineral known since Antiquity. It most often appears in efflorescences without distinct crystalline forms, more rarely in rhomboidal tablets with clear cleavage, white to white-gray in color, sometimes yellowish. It is a notable sodium ore.

Main photo : Natron from Wyoming, USA © Steve Hardinger

Natron in the World

Natron is very abundant in some salt lakes in California (Dearles Lake), Nevada (Ragtown), and British Columbia (Clinton).

Natron in France

In France, natron is known in acicular crystals in tiny cracks in the granite used for the construction of the church of Saint-Nonna in Penmarc'h (Finistère), this formation is linked to sea spray.

Twinning

Twins are known on {001}.

Fakes and treatments

No fakes recorded for this mineral species.



Hardness : 1 to 1.5
Density : 1.478
Fracture : Conchoidal
Streak : White


TP : Translucent to transparent
RI : 1.405 to 1.440
Birefringence : 0.035
Optical character : Biaxial -
Pleochroism : None
Fluorescence : None


Solubility : Acids, water

Magnetism : NoneRadioactivity : None