Picromerite
Picromerite is a mineral from the class of hydrous sulfates lacking additional anions, and containing medium to large cations according to the Nickel-Strunz classification.Etymology
The name comes from the Greek words πικρός for "bitter" and μέρος for "part", and relates to the bitter taste of the mineral.Occurrence
Picromerite is found on comparatively few places, currently only about 40 localities are known. It was first identified in active volcanic fumaroles on Mt. Vesuvius by Arcangelo Scacchi in 1855 and has also been found in volcanic deposits on Mt. Etna and on Hawai'i.
It is more commonly found in the kainite zones of some marine salt deposits, among them salt mines in Thuringia, Lower Saxony and Saxony-Anhalt, near Hall in Tirol, Hallstatt and Bad Ischl, near Whitby, and in the Carlsbad Potash District, also on salt lakes in western China.
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 anhydrite, epsomite, halite, hohmannite, kainite, metasideronatrite und metavoltine, depending on the locality.Properties
Picromerite dehydrates in dry air, and crystals then show dull, spherical dehydration zones. Progressive dehydration leads to leonite.
