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== Genesis and occurrence == Kainite was discovered in the [[Stassfurt]] salt mines in today's [[Saxony-Anhalt]], [[Germany]] in 1865 by the mine official Schöne and was first described by Carl Friedrich Jacob Zincken.<ref>Zincken, C. (1865): Mittheilung an Prof. H.B. Geinitz vom 18.März 1865 [Über ein neues Mineral, Kainit].- Neues Jahrbuch für Mineralogie, Geologie und Paläontologie, 310.</ref><ref>Zincken, C. (1865): Ueber die Zusammensetzung des Kainits von Leopoldshall bei Stassfurth.- Berg- und hüttenmännische Zeitung 24, 288.</ref> Kainite is a typical secondary mineral that forms through metamorphosis in marine deposits of [[potassium carbonate]], and is also occasionally formed through resublimation from volcanic vapours. It is often [[paragenesis|accompanied]] by [[anhydrite]], [[carnallite]], [[halite]], and [[kieserite]]. Kainite is only found in comparatively few places,<ref>{{cite web | url = http://www.mindat.org/show.php?id=2132&ld=2#themap | title = Kainite: Localities for Kainite | publisher = Mindat}}</ref> among them in salt mines in central and northern Germany, [[Bad Ischl]] (Austria), on [[Pasquasia]] in [[Sicily]], in [[Whitby]] (UK), and in the Carlsbad Potash District in [[New Mexico]], in volcanic deposits in [[Kamchatka]]<ref>Pekov, Igor V., et al. "New zinc and potassium chlorides from fumaroles of the Tolbachik volcano, Kamchatka, Russia: mineral data and crystal chemistry. II. Flinteite, K2ZnCl4." European Journal of Mineralogy (2015): ejm2459_pap_gsw.</ref> and in [[Iceland]],<ref>Jacobsson et al (1992) Encrustations from Lava Caves on Surtsey, Iceland. A Preliminary Report: Surtsey Research Progress Report X: 73-78 Reykjevik, Iceland.</ref> and in salt lakes in western [[China]]. It has also been identified in [[Gusev Crater]] on [[Mars]].<ref>Rice, M. S., et al. "Silica-rich deposits and hydrated minerals at Gusev Crater, Mars: Vis-NIR spectral characterization and regional mapping." Icarus 205.2 (2010): 375-395.</ref> It can also be produced from [[Bittern (salt)|bittern]] remaining after removal of table salt from seawater.
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