Moschellandsbergite
{{Short description|Isometric mineral made up of a silver-white amalgam of mercury and silver}}
{{Infobox mineral
| name = Moschellandsbergite
| category = Metals and intermetallic alloys
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| image = Moschellandsbergite-21591.jpg
| imagesize = 260px
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| formula = silver amalgam, Ag2Hg3
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| strunz = 1.AD.15d
| system = Isometric
| class = Tetartoidal (23)
(same H-M symbol)
| symmetry = I23
| unit cell = a = 10.04 Å, Z = 10
| color = white, tarnishes grey
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| cleavage = brittle
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| mohs = 3.5
| luster = metallic
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| gravity = 13.48
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| references = [https://www.mineralienatlas.de/lexikon/index.php/MineralData?mineral=Moschellandsbergite Mineralienatlas][http://www.handbookofmineralogy.org/pdfs/moschellandsbergite.pdf Mineral Handbook][http://www.mindat.org/min-2789.html Mindat][http://webmineral.com/data/Moschellandsbergite.shtml Webmineral]
}}
Moschellandsbergite is a rare isometric mineral made up of a silver-white amalgam of mercury and silver with the chemical makeup Ag2Hg3.
It was first described in 1938 and named after Moschellandsberg Mountain near Obermoschel, Rhineland-Palatinate, Germany.{{Cite book | author= American Geological Institute | title = Dictionary of Mining, Mineral, and Related Terms | publisher = Birkhäuser | location = Alexandria, Virginia | pages = 356 | year = 1997 | isbn = 0-922152-36-5}} It is considered a low-temperature hydrothermal mineral which occurs with metacinnabar, cinnabar, mercurian silver, tetrahedrite–tennantite, pyrite, sphalerite and chalcopyrite.