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Picromerite
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Picromerite (synonyms: schoenite, schönite) is a mineral from the class of hydrous lacking additional anions, and containing medium to large cations according to the Nickel–Strunz classification.


Etymology
The name comes from the Greek words πικρός pikros for "bitter" and μέρος meros for "part", and relates to the bitter taste of the mineral.


Occurrence
Picromerite is found on comparatively few places, currently (2015) only about 40 localities are known. It was first identified in active volcanic fumaroles on by Arcangelo Scacchi in 1855 and has also been found in volcanic deposits on and on Hawai'i.

It is more commonly found in the zones of some marine salt deposits, among them salt mines in , and (Germany), near Hall in Tirol, and (Austria), near (UK), and in the Carlsbad Potash District (New Mexico), also on salt lakes in western .

Picromerite can also form in sulfate-rich hydrothermal ore deposits and is found in slag heaps of some ore and coal mines.

Picromerite is often accompanied by , , , , , metasideronatrite and , depending on the locality.


Properties
Picromerite dehydrates in dry air, and crystals then show dull, spherical dehydration zones. Progressive dehydration leads to .


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