[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:2633":3},{"id":4,"longid":5,"guid":6,"name":7,"shortcode_ima":8,"entrytype":9,"entrytype_text":10,"varietyof":11,"synid":11,"polytypeof":11,"groupid":12,"weighting":13,"nolocadd":14,"blacklisted":14,"mindat_formula":15,"mindat_formula_note":16,"ima_formula":17,"elements":18,"sigelements":23,"key_elements":11,"impurities":24,"cim":25,"ima_status":26,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":11,"discovery_year":29,"strunz10ed1":30,"strunz10ed2":31,"strunz10ed3":32,"strunz10ed4":33,"dana8ed1":34,"dana8ed2":35,"dana8ed3":36,"dana8ed4":37,"csystem":38,"cclass":39,"spacegroup":40,"spacegroupset":41,"a":42,"b":43,"c":44,"alpha":45,"beta":46,"gamma":45,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":47,"csmetamict":14,"commentcrystal":11,"twinning":48,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":49,"tlform":11,"hmin":50,"hmax":50,"hardtype":51,"vhnmin":45,"vhnmax":45,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":52,"dmeas2":52,"dcalc":53,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":54,"commentluster":11,"diapheny":55,"streak":56,"colour":57,"commentcolor":58,"colors":59,"streak_colors":64,"luminescence":11,"uv":11,"cleavage":65,"cleavagetype":66,"fracturetype":67,"tenacity":68,"commentbreak":11,"opticaltype":69,"opticalsign":70,"opticalalpha":71,"opticalalpha2":72,"opticalalphaerror":11,"opticalbeta":73,"opticalbeta2":74,"opticalbetaerror":11,"opticalgamma":75,"opticalgamma2":45,"opticalgammaerror":11,"opticalomega":45,"opticalomega2":45,"opticalomegaerror":11,"opticalepsilon":45,"opticalepsilon2":45,"opticalepsilonerror":11,"opticaln":45,"opticaln2":45,"opticalnerror":11,"optical2vcalc":76,"optical2vcalc2":45,"optical2vcalcerror":11,"optical2vmeasured":77,"optical2vmeasured2":45,"optical2vmeasurederror":11,"rimin":78,"rimax":79,"opticaldispersion":80,"opticalpleochroism":11,"opticalpleochorismdesc":11,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":11,"opticalr":11,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":81,"industrial":11,"occurrence":11,"otheroccurrence":82,"type_specimen_store":11,"description_short":83,"aboutname":84,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":85,"reviewed_at":11,"variety_of":11,"varieties":86,"group_members":100,"associates":138,"confused_with":187,"type_localities":189,"occurrence_total":190,"citations":191,"images":362,"structures":470,"synonyms":498,"language_names":517,"wikidata_qid":624,"texts":625},2633,"1:1:2633:4","d29ceb9f-bf0a-4b87-810d-6b70e647f270","Melanterite","Mln",0,"mineral",null,29309,3220,false,"Fe\u003Csup>2+\u003C\u002Fsup>(H\u003Csub>2\u003C\u002Fsub>O)\u003Csub>6\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)·H\u003Csub>2\u003C\u002Fsub>O","Six of the water molecules are coordinated with iron.\r\nOften contains minor Cu, colouring the mineral pale bluish to greenish blue to blue.","Fe(SO\u003Csub>4\u003C\u002Fsub>) · 7H\u003Csub>2\u003C\u002Fsub>O",[19,20,21,22],"Fe","O","S","H",[19,20,21,22],",Cu,Mg,,","25.10.5",[27,28],"APPROVED","GRANDFATHERED","Know","7","C","B","35","29","6","10","1","Monoclinic",5,14,"P21\u002Fc ","14.077","6.509","11.054","0","105.6",4,"None reported.","Crystals rare, equant to short prismatic parallel to [001] with prominent {110} and {001}; thick tabular {010} or {10_1}, also pseudo-octahedral due to equal development of {110}, {001}, and {_101}; more typically found as beard-like efflorescences, or as capillary to fibrous aggregates; it may also be stalactic or concretionary.",2,3,"1.89","1.893","Vitreous","Translucent,Opaque","White.","Colorless to white or green, also greenish-blue to blue with increased Cu content; colourless to pale green in transmitted light.","Usually a yellowish-white after exposure to air and moisture.",[60,61,62,63],"colorless","white","green","blue",[61],"Perfect on {001}, distinct on {110}.","Perfect","Conchoidal","brittle","Biaxial","+","1.47","1.471","1.4765","1.4795","1.486","80","86",1.47,1.486,"none","Soluble in water","A secondary mineral formed by the oxidation of iron sulfide minerals, such as pyrite and marcasite, it is found occurring naturally in sheltered crevices and cavities in sulfidic sedimentary and metamorphic rocks, and in coal and lignite deposits.  It also forms readily on the walls, timbers, and other structures in mines.","Melanterite Group.\r\nIron analogue of boothite and zincmelanterite.\r\n\r\nMelanterite is a hydrated iron sulphate formed after the decomposition of pyrite or other (metal-)iron sulphide minerals due to the action of surface waters. It is often found in min...","Named in 1850 from the Greek μελαντηρία for \"copperas,\" meaning ferrous sulfate.","2026-05-05 19:27:05",[87,91,96],{"id":88,"name":89,"entrytype":50,"csystem":11,"ima_formula":11,"mindat_formula":90,"hmin":11,"hmax":11,"dmeas":45,"dcalc":45,"primary_image_id":11},11185,"Copper-bearing Melanterite","(Fe,Cu)SO\u003Csub>4\u003C\u002Fsub>·7H\u003Csub>2\u003C\u002Fsub>O",{"id":92,"name":93,"entrytype":50,"csystem":11,"ima_formula":11,"mindat_formula":94,"hmin":11,"hmax":11,"dmeas":45,"dcalc":45,"primary_image_id":95},31697,"Kirovite","(Fe,Mg)SO\u003Csub>4\u003C\u002Fsub>·7H\u003Csub>2\u003C\u002Fsub>O",62796,{"id":97,"name":98,"entrytype":50,"csystem":11,"ima_formula":11,"mindat_formula":99,"hmin":11,"hmax":11,"dmeas":45,"dcalc":11,"primary_image_id":11},9516,"Manganese-bearing Melanterite","(Fe,Mn)SO\u003Csub>4\u003C\u002Fsub>·7H\u003Csub>2\u003C\u002Fsub>O",[101,109,117,124,131],{"id":102,"name":103,"entrytype":9,"csystem":38,"ima_formula":104,"mindat_formula":105,"hmin":106,"hmax":106,"dmeas":45,"dcalc":107,"primary_image_id":108},27526,"Alpersite","Mg(SO\u003Csub>4\u003C\u002Fsub>) · 7H\u003Csub>2\u003C\u002Fsub>O","(Mg,Cu\u003Csup>2+\u003C\u002Fsup>)(H\u003Csub>2\u003C\u002Fsub>O)\u003Csub>6\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)·H\u003Csub>2\u003C\u002Fsub>O",2.5,"1.820",892,{"id":110,"name":111,"entrytype":9,"csystem":38,"ima_formula":112,"mindat_formula":113,"hmin":50,"hmax":50,"dmeas":114,"dcalc":115,"primary_image_id":116},664,"Bieberite","Co(SO\u003Csub>4\u003C\u002Fsub>) · 7H\u003Csub>2\u003C\u002Fsub>O","Co\u003Csup>2+\u003C\u002Fsup>(H\u003Csub>2\u003C\u002Fsub>O)\u003Csub>6\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)·H\u003Csub>2\u003C\u002Fsub>O","1.96","1.83",3242,{"id":118,"name":119,"entrytype":9,"csystem":38,"ima_formula":120,"mindat_formula":121,"hmin":50,"hmax":106,"dmeas":122,"dcalc":45,"primary_image_id":123},720,"Boothite","Cu(SO\u003Csub>4\u003C\u002Fsub>) · 7H\u003Csub>2\u003C\u002Fsub>O","Cu\u003Csup>2+\u003C\u002Fsup>(H\u003Csub>2\u003C\u002Fsub>O)\u003Csub>6\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)·H\u003Csub>2\u003C\u002Fsub>O","1.94",2033,{"id":125,"name":126,"entrytype":9,"csystem":38,"ima_formula":127,"mindat_formula":128,"hmin":50,"hmax":50,"dmeas":129,"dcalc":130,"primary_image_id":11},2555,"Mallardite","Mn(SO\u003Csub>4\u003C\u002Fsub>) · 7H\u003Csub>2\u003C\u002Fsub>O","Mn\u003Csup>2+\u003C\u002Fsup>(H\u003Csub>2\u003C\u002Fsub>O)\u003Csub>6\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)·H\u003Csub>2\u003C\u002Fsub>O","1.846","1.838",{"id":132,"name":133,"entrytype":9,"csystem":38,"ima_formula":134,"mindat_formula":135,"hmin":50,"hmax":106,"dmeas":136,"dcalc":137,"primary_image_id":11},4406,"Zincmelanterite","Zn(SO\u003Csub>4\u003C\u002Fsub>) · 7H\u003Csub>2\u003C\u002Fsub>O","Zn(H\u003Csub>2\u003C\u002Fsub>O)\u003Csub>6\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)·H\u003Csub>2\u003C\u002Fsub>O","2.02","1.93",[139,148,157,166,172,179],{"id":140,"name":141,"entrytype":9,"csystem":142,"ima_formula":143,"mindat_formula":144,"hmin":145,"hmax":50,"dmeas":45,"dcalc":146,"primary_image_id":147},162,"Alunogen","Triclinic","Al\u003Csub>2\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)\u003Csub>3\u003C\u002Fsub>(H\u003Csub>2\u003C\u002Fsub>O)\u003Csub>12\u003C\u002Fsub> · 5H\u003Csub>2\u003C\u002Fsub>O","Al\u003Csub>2\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)\u003Csub>3\u003C\u002Fsub>·17H\u003Csub>2\u003C\u002Fsub>O",1.5,"1.732",29065,{"id":149,"name":150,"entrytype":9,"csystem":151,"ima_formula":152,"mindat_formula":153,"hmin":51,"hmax":47,"dmeas":154,"dcalc":155,"primary_image_id":156},1279,"Diadochite","Amorphous","Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)(SO\u003Csub>4\u003C\u002Fsub>)(OH) · 6H\u003Csub>2\u003C\u002Fsub>O","Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)(SO\u003Csub>4\u003C\u002Fsub>)(OH)·6H\u003Csub>2\u003C\u002Fsub>O","2.0","2.32",7108,{"id":158,"name":159,"entrytype":9,"csystem":160,"ima_formula":161,"mindat_formula":162,"hmin":50,"hmax":106,"dmeas":163,"dcalc":164,"primary_image_id":165},1544,"Fibroferrite","Trigonal","Fe\u003Csup>3+\u003C\u002Fsup>(SO\u003Csub>4\u003C\u002Fsub>)(OH) · 5H\u003Csub>2\u003C\u002Fsub>O","Fe\u003Csup>3+\u003C\u002Fsup>(SO\u003Csub>4\u003C\u002Fsub>)(OH)·5H\u003Csub>2\u003C\u002Fsub>O","1.84","1.996",8890,{"id":167,"name":168,"entrytype":9,"csystem":151,"ima_formula":169,"mindat_formula":170,"hmin":11,"hmax":11,"dmeas":45,"dcalc":45,"primary_image_id":171},2015,"Ilsemannite","Mo\u003Csub>3\u003C\u002Fsub>O\u003Csub>8\u003C\u002Fsub> · nH\u003Csub>2\u003C\u002Fsub>O (?)","Mo\u003Csub>3\u003C\u002Fsub>O\u003Csub>8\u003C\u002Fsub>·nH\u003Csub>2\u003C\u002Fsub>O",12169,{"id":173,"name":174,"entrytype":9,"csystem":151,"ima_formula":175,"mindat_formula":176,"hmin":50,"hmax":51,"dmeas":177,"dcalc":45,"primary_image_id":178},3224,"Pitticite","[Fe,AsO\u003Csub>4\u003C\u002Fsub>,SO\u003Csub>4\u003C\u002Fsub>,H\u003Csub>2\u003C\u002Fsub>O] (?)","(Fe, AsO\u003Csub>4\u003C\u002Fsub>, H\u003Csub>2\u003C\u002Fsub>O) (?)","2.2",30484,{"id":180,"name":181,"entrytype":9,"csystem":38,"ima_formula":182,"mindat_formula":183,"hmin":50,"hmax":51,"dmeas":184,"dcalc":185,"primary_image_id":186},3469,"Rozenite","Fe\u003Csup>2+\u003C\u002Fsup>(SO\u003Csub>4\u003C\u002Fsub>) · 4H\u003Csub>2\u003C\u002Fsub>O","FeSO\u003Csub>4\u003C\u002Fsub>·4H\u003Csub>2\u003C\u002Fsub>O","2.293","2.29",21251,[188],{"id":102,"name":103,"entrytype":9,"csystem":38,"ima_formula":104,"mindat_formula":105,"hmin":106,"hmax":106,"dmeas":45,"dcalc":107,"primary_image_id":108},[],848,[192,195,199,203,207,211,215,219,223,227,231,235,239,244,249,253,257,260,264,268,273,277,281,284,288,293,298,302,306,311,315,320,324,328,333,337,341,345,349,353,357],{"id":193,"year":11,"html":194,"doi":11},16116724,"1167–1174.",{"id":196,"year":197,"html":198,"doi":11},18530121,1832,"Beudant, François-Sulpice (1832) \u003Ci>Traité élémentaire de minéralogie. Deuxiéme Edition [Elementary Treatise on Mineralogy. Second Edition]\u003C\u002Fi> (2nd ed.) Vol. 2 - Tome II [Volume  II]. Chez Verdière. \u003Ca target='_blank' href='https:\u002F\u002Farchive.org\u002Fdownload\u002Fbub_gb_XSRCAAAAcAAJ\u002Fbub_gb_XSRCAAAAcAAJ.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":200,"year":201,"html":202,"doi":11},16116698,1843,"Chapman, E.J. (1843) Practical Mineralogy. London, Paris, and Leipzig: 14 (as Melantherite).",{"id":204,"year":205,"html":206,"doi":11},16116699,1850,"Haidinger, Wm. (1850) Handbuch der bestimmenden Mineralogie. Vienna, 2nd. Edition: 489 (as Melanterit).",{"id":208,"year":209,"html":210,"doi":11},16116700,1867,"Erofejeff (1867) Konigliche Akademie der Wissenschaften, Vienna, Sitzber.: 56: 63.",{"id":212,"year":213,"html":214,"doi":11},16116702,1879,"Zepharovich (1879) Konigliche Akademie der Wissenschaften, Vienna, Sitzber.: 79: 183.",{"id":216,"year":217,"html":218,"doi":11},16116703,1889,"Retgers (1889) Zeitschrift für Physikalische Chemie, Leipzig, Berlin: 3: 534.",{"id":220,"year":221,"html":222,"doi":11},16116704,1894,"Michel (1894) Bulletin de la Société française de Minéralogie: 17: 204.",{"id":224,"year":225,"html":226,"doi":11},16116705,1901,"Edgren (1901) Geologiska Föeningens I Stockholm. Förhandlinger, Stockholm: 23: 329.",{"id":228,"year":229,"html":230,"doi":11},16156294,1903,"Schaller, Waldemar Theodore (1903) Minerals from Leona Heights, Alameda County, California. University of California, Department of Geological Sciences Bulletin: 3: 191-217.",{"id":232,"year":233,"html":234,"doi":11},16116706,1915,"Pilipenko (1915) Bull. Imp. Tomsk. Univ., no. 63 [Min. Abs.: 2: 113 (1923)].",{"id":236,"year":237,"html":238,"doi":11},4468625,1916,"(1916) \u003Ci>Atlas Der Krystallformen\u003C\u002Fi> Vol. 3 - Text - Band III - Danalith-Feldspat-Gruppe. Carl Winters Universitätsbuchhandlung, Heidelberg.",{"id":240,"year":241,"html":242,"doi":243},647767,1921,"Larsen, Esper S. (1921) The microscopic determination of the nonopaque minerals. \u003Ci>Bulletin\u003C\u002Fi> 679. US Geological Survey \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3133\u002Fb679'>doi:10.3133\u002Fb679\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fpubs.usgs.gov\u002Fbul\u002F0679\u002Freport.pdf' class='refpdflink'>\u003C\u002Fa>","10.3133\u002Fb679",{"id":245,"year":246,"html":247,"doi":248},6220654,1923,"Collins, Henry F. (1923) On some crystallized sulphates from the province of Huelva, Spain. \u003Ci>Mineralogical Magazine and Journal of the Mineralogical Society\u003C\u002Fi>, 20 (100). 32-38 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1923.020.100.05'>doi:10.1180\u002Fminmag.1923.020.100.05\u003C\u002Fa>","10.1180\u002Fminmag.1923.020.100.05",{"id":250,"year":251,"html":252,"doi":11},16116710,1924,"Niggli and Faesy (1924) Zeitschrift für Kristallographie, Mineralogie und Petrographie, Leipzig: 59: 258.",{"id":254,"year":255,"html":256,"doi":11},16116711,1927,"Vavrinecz (1927) Zeitschrift für Kristallographie, Mineralogie und Petrographie, Leipzig: 66: 167.",{"id":258,"year":255,"html":259,"doi":11},16116712,"Westenbrink (1927) Recueil des travaux chimiques des Pays-Bas et de la Belgique, Leyden: 46: 105.",{"id":261,"year":262,"html":263,"doi":11},16116713,1928,"Zsivny (1928) Zeitschrift für Kristallographie, Mineralogie und Petrographie, Leipzig: 66: 651.",{"id":265,"year":266,"html":267,"doi":11},16111340,1929,"Vavrinecz (1929) Magyar Chemiai Folyóirat, Budapest: 35: 1.",{"id":269,"year":270,"html":271,"doi":272},7106,1930,"Hey, Max H. (1930) Cupriferous melanterite from the Skouriotissa mine, Cyprus. \u003Ci>Mineralogical Magazine and Journal of the Mineralogical Society\u003C\u002Fi>,  22 (131) 413-418 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1930.022.131.02'>doi:10.1180\u002Fminmag.1930.022.131.02\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_22\u002F22-131-413.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1930.022.131.02",{"id":274,"year":275,"html":276,"doi":11},520137,1933,"Eckel, Edwin B. (1933) Stability relations of a Colorado pisanite (cuprian melanterite) \u003Ci>American Mineralogist\u003C\u002Fi>,  18 (10) 449-453 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM18\u002FAM18_449.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":278,"year":279,"html":280,"doi":11},16116716,1935,"Machatschki (1935) Zbl. Min.: 53.",{"id":282,"year":279,"html":283,"doi":11},16116717,"Ungemach (1935) Bulletin de la Société française de Minéralogie: 58: 159.",{"id":285,"year":286,"html":287,"doi":11},16116718,1937,"Simpson (1937) Journal of the Royal Society of Western Australia: 23: 17.",{"id":289,"year":290,"html":291,"doi":292},233820,1938,"Milton, Charles, Johnston, William Drum (1938) Sulphate minerals of the Comstock Lode, Nevada. \u003Ci>Economic Geology\u003C\u002Fi>,  33 (7) 749-771 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2113\u002Fgsecongeo.33.7.749'>doi:10.2113\u002Fgsecongeo.33.7.749\u003C\u002Fa>","10.2113\u002Fgsecongeo.33.7.749",{"id":294,"year":295,"html":296,"doi":297},5700401,1940,"Ness, Ilse (1940) Zum Gitterbau des monoklinen FeSO4 · 7H2O (Eisenvitriol, Melanterit). \u003Ci>Die Naturwissenschaften\u003C\u002Fi>,  28 (5). 78 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fbf01493998'>doi:10.1007\u002Fbf01493998\u003C\u002Fa>","10.1007\u002Fbf01493998",{"id":299,"year":300,"html":301,"doi":11},16116721,1944,"Mélon (1944) Ann. soc. géol. Belgique: 67: B56.",{"id":303,"year":304,"html":305,"doi":11},1118652,1951,"Palache, Charles; Berman, Harry; Frondel, Clifford (1951) \u003Ci>The System of Mineralogy\u003C\u002Fi> (7th ed.) Vol. 2 - Halides, Nitrates, Borates, Carbonates, Sulfates, Phosphates, Arsenates, Tungstates, Molybdates, Etc. John Wiley and Sons.",{"id":307,"year":308,"html":309,"doi":310},5719264,1962,"Baur, Werner H. (1962) Die Kristallstrukturbestimmung des Melanterits, FeSO4·7 H2O. \u003Ci>Die Naturwissenschaften\u003C\u002Fi>,  49 (20). 464 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fbf00631886'>doi:10.1007\u002Fbf00631886\u003C\u002Fa>","10.1007\u002Fbf00631886",{"id":312,"year":313,"html":314,"doi":11},16085972,1963,"Pel, J., Bourguignon, P. (1963) Cristallisation de mélantérite dans des schistes houillers et leurs effets. Annales de la Société géologique de Belgique, 86, B569.",{"id":316,"year":317,"html":318,"doi":319},16591697,1964,"Kohler, K.; Zäske, P. (1964) Beiträge zur Thermochemie der Hydrate. III. Der thermische Abbau von CoSO\u003Csub>4\u003C\u002Fsub> · 7 H\u003Csub>2\u003C\u002Fsub>O, FeSO\u003Csub>4\u003C\u002Fsub> · 7 H\u003Csub>2\u003C\u002Fsub>O, CuSO\u003Csub>4\u003C\u002Fsub> · 5 H\u003Csub>2\u003C\u002Fsub>O und die Isotypiebeziehungen der Abbauprodukte der Epsomit‐ und Melanteritreihe. \u003Ci>Zeitschrift für anorganische und allgemeine Chemie\u003C\u002Fi>,  331 (1-2). p.7-16. \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1002\u002Fzaac.19643310103'>doi:10.1002\u002Fzaac.19643310103\u003C\u002Fa>","10.1002\u002Fzaac.19643310103",{"id":321,"year":317,"html":322,"doi":323},619915,"Baur, W. H. (1964) On the crystal chemistry of salt hydrates. III. The determination of the crystal structure of FeSO4.7H2O (melanterite) \u003Ci>Acta Crystallographica\u003C\u002Fi>,  17 (9) 1167-1174 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1107\u002Fs0365110x64003000'>doi:10.1107\u002Fs0365110x64003000\u003C\u002Fa>","10.1107\u002Fs0365110x64003000",{"id":325,"year":326,"html":327,"doi":11},524345,1965,"Ehlers, Ernest G., Stiles, David V. (1965) Melanterite-rozenite equilibrium. \u003Ci>American Mineralogist\u003C\u002Fi>,  50 (9) 1457-1460 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM50\u002FAM50_1457.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":329,"year":330,"html":331,"doi":332},217724,1969,"El Saffar, Z. M. (1969) On the water molecules in FeSO4.7H2O. A nuclear magnetic resonance study. \u003Ci>Acta Crystallographica Section B Structural Crystallography and Crystal Chemistry\u003C\u002Fi>,  25 (9) 1784-1786 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1107\u002Fs0567740869004730'>doi:10.1107\u002Fs0567740869004730\u003C\u002Fa>","10.1107\u002Fs0567740869004730",{"id":334,"year":335,"html":336,"doi":11},16116725,1970,"U.S. Department of Commerce (1970) National Bureau of Standards Monograph 25: Standard X-ray Diffraction Powder Patterns, section 8. (http:\u002F\u002Fdigicoll.manoa.hawaii.edu\u002Ftechreports\u002FPDF\u002FNBS25-8.pdf)",{"id":338,"year":339,"html":340,"doi":11},1118654,1997,"Gaines, Richard V.; Skinner, H. Catherine W.; Foord, Eugene E.; Mason, Brian; Rosenzweig, Abraham; King, Vandall T. (1997) \u003Ci>Dana's New Mineralogy\u003C\u002Fi> (8th ed.). Wiley-Interscience. 1872 pp.",{"id":342,"year":343,"html":344,"doi":11},16116727,2003,"Peterson, R.C. (2003) Dehydration of mine waste. The relationship among melanterite FeSO4·7H2O, siderotile FeSO4·5H2O and rozenite FeSO4·4H2O. Geological Association of Canada-Mineralogical Association of Canada-Society of Economic Geologists Abstracts Volume 28: 134-135.",{"id":346,"year":347,"html":348,"doi":11},16965927,2005,"(2005) Melanterite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fmelanterite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":350,"year":347,"html":351,"doi":352},293857,"Hammarstrom, J.M., Seal, R.R., Meier, A.L., Kornfeld, J.M. (2005) Secondary sulfate minerals associated with acid drainage in the eastern US: recycling of metals and acidity in surficial environments. \u003Ci>Chemical Geology\u003C\u002Fi>,  215 (1) 407-431 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.chemgeo.2004.06.053'>doi:10.1016\u002Fj.chemgeo.2004.06.053\u003C\u002Fa>","10.1016\u002Fj.chemgeo.2004.06.053",{"id":354,"year":355,"html":356,"doi":11},16116729,2018,"Mauro, D., Biagioni, C., Pasero, M. (2018) Crystal-chemistry of sulfates from Apuan Alps (Tuscany, Italy). I. Crystal structure and hydrogen bond system of melanterite, Fe(H2O)6(SO4)•H2O. Periodico di Mineralogia: 87: 89-96.",{"id":358,"year":359,"html":360,"doi":361},13422272,2021,"Lacalamita, Maria, Ventruti, Gennaro, Della Ventura, Giancarlo, Radica, Francesco, Mauro, Daniela, Schingaro, Emanuela (2021) In Situ High-Temperature X-ray Powder Diffraction and Infrared Spectroscopic Study of Melanterite, FeSO\u003Csub>4\u003C\u002Fsub>·7H\u003Csub>2\u003C\u002Fsub>O. \u003Ci>Minerals\u003C\u002Fi>,  11 (4) 392 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3390\u002Fmin11040392'>doi:10.3390\u002Fmin11040392\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fwww.mdpi.com\u002F2075-163X\u002F11\u002F4\u002F392\u002Fpdf?version=1617963666' class='refpdflink'>\u003C\u002Fa>","10.3390\u002Fmin11040392",[363,373,380,388,398,404,412,418,427,433,439,445,453,460],{"id":364,"source_url":365,"license_code":366,"credit_html":367,"title":368,"description":369,"author":370,"original_width":371,"original_height":372},15794,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=12682540","Public domain","John Krygier, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=12682540\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Melanterite-322401.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMelanterite\" class=\"extiw\" title=\"en:Melanterite\">Melanterite\u003C\u002Fa> (size: 2\" across)\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Copperas Mountain, Paxton Township, Ross County, Ohio, USA\u003C\u002Fdd>\n\u003Cdd>\u003Ci>original description:\u003C\u002Fi> Melanterite efflorescence, from the breakdown of pyrite in the Ohio Shale. Almost a year after I collected the specimen (shown in the other image) the shale fell apart; the melanterite maintained its color and did not fall apart, so I removed what I could from the shale (July 2010).\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","John Krygier",1024,768,{"id":374,"source_url":375,"license_code":376,"credit_html":377,"title":7,"description":11,"author":11,"original_width":378,"original_height":379},30178,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F115205","CC BY 4.0","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F115205\" rel=\"noopener\">Department of Geology, TalTech\u003C\u002Fa> via Europeana",1000,666,{"id":381,"source_url":382,"license_code":366,"credit_html":383,"title":384,"description":385,"author":370,"original_width":386,"original_height":387},15796,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=68179099","John Krygier, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=68179099\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Melanterite-253611.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMelanterite\" class=\"extiw\" title=\"en:Melanterite\">Melanterite\u003C\u002Fa> (size: 2\" across)\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Copperas Mountain, Paxton Township, Ross County, Ohio, USA\u003C\u002Fdd>\n\u003Cdd>\u003Ci>original description:\u003C\u002Fi> Sample of Melanterite efflorescence on shale. The shale is crumbly and the Melanterite fibrous, fragile, and water soluble. This sample is pale green in color. Collected September 2009.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",2400,1800,{"id":389,"source_url":390,"license_code":391,"credit_html":392,"title":393,"description":394,"author":395,"original_width":396,"original_height":397},15797,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=68180183","CC BY-SA 3.0","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=68180183\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Melanterite-657241.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMelanterite\" class=\"extiw\" title=\"en:Melanterite\">Melanterite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGypsum\" class=\"extiw\" title=\"en:Gypsum\">Gypsum\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Buena Vista Mine (Goodview Mine), Providencia Canyon, Patagonia District, Patagonia Mts, Santa Cruz County, Arizona, USA\u003C\u002Fdd>\n\u003Cdd>Size: 6.7cm x 5.3cm x 3.2cm\u003C\u002Fdd>\n\u003Cdd>An interesting and attractive combination specimen from Arizona. The majority of the specimen is composed of microcrystalline melanterite (cuprian), turquoise blue in color. Melanterite is a hydrated iron sulphate, formed after the decomposition of pyrite or other iron minerals due to the action of surface waters. It is often found in mines as a post-mining formation on mine walls. On the melanterite is a forest of dozens upon dozens 3-4 mm white curvaceous gypsum (var. selenite) fishtail twins. Ex. Hoppel Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Robert M. Lavinsky",465,281,{"id":399,"source_url":400,"license_code":391,"credit_html":401,"title":402,"description":394,"author":395,"original_width":396,"original_height":403},15798,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=68180187","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=68180187\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Melanterite-657239.jpg",344,{"id":405,"source_url":406,"license_code":391,"credit_html":407,"title":408,"description":409,"author":395,"original_width":410,"original_height":411},15799,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=68180821","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=68180821\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Melanterite-784855.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMelanterite\" class=\"extiw\" title=\"en:Melanterite\">Melanterite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGypsum\" class=\"extiw\" title=\"en:Gypsum\">Gypsum\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Sherwood Mine, Mineral Hills, Menominee iron range, Iron County, Michigan, USA\u003C\u002Fdd>\n\u003Cdd>Size: 10.4cm x 7.9cm x 6.1cm\u003C\u002Fdd>\n\u003Cdd>Melanterite is a hydrated iron sulphate formed after the decomposition of pyrite or other iron minerals due to the action of surface waters. It is often found in mines as a post-mining formation on mine walls (MINDAT). It is very rare from any of the iron mines in Iron County of the Menominee iron range. This sculptural, large, very light weight (119 grams), post-mining crust is from the extinct underground Sherwood Mine, a deep 1625' mine. The rounded light brown masses consist of intergrown sprays of needle-like crystals. It looks like coral on the surface. Rare and desirable older material from the Mark & Lynn Langenfeld and Robert Nowakowski Collections. Melanterite is not listed for this locality on Mindat.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",1500,1252,{"id":413,"source_url":414,"license_code":391,"credit_html":415,"title":416,"description":409,"author":395,"original_width":417,"original_height":378},15800,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=68180824","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=68180824\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Melanterite-784856.jpg",1853,{"id":419,"source_url":420,"license_code":376,"credit_html":421,"title":422,"description":423,"author":424,"original_width":425,"original_height":426},15801,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=168135790","Animalculum, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=168135790\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Melanterite, Musee de Mineralogie, Paris, 2025.jpg","Melanterite from Salsigne, Aude, France in Musee de Mineralogie, Paris","Animalculum",1824,2425,{"id":428,"source_url":429,"license_code":391,"credit_html":430,"title":431,"description":394,"author":395,"original_width":396,"original_height":432},50639,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=68180186","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=68180186\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Melanterite-657240.jpg",337,{"id":434,"source_url":435,"license_code":391,"credit_html":436,"title":437,"description":394,"author":395,"original_width":396,"original_height":438},50640,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=68180189","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=68180189\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Melanterite-657238.jpg",319,{"id":440,"source_url":441,"license_code":391,"credit_html":442,"title":443,"description":409,"author":395,"original_width":410,"original_height":444},50641,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=68180819","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=68180819\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Melanterite-784854.jpg",1212,{"id":446,"source_url":447,"license_code":391,"credit_html":448,"title":449,"description":450,"author":395,"original_width":451,"original_height":452},21091,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10159473","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10159473\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Chalcanthite-Melanterite-Romerite-202117.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FChalcanthite\" class=\"extiw\" title=\"en:Chalcanthite\">Chalcanthite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMelanterite\" class=\"extiw\" title=\"en:Melanterite\">Melanterite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FR%C3%B6merite\" class=\"extiw\" title=\"en:Römerite\">Römerite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCerro_de_Pasco\" class=\"extiw\" title=\"en:Cerro de Pasco\">Cerro de Pasco\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDaniel_Alcides_Carri%C3%B3n_Province\" class=\"extiw\" title=\"en:Daniel Alcides Carrión Province\">Daniel Alcides Carrión Province\u003C\u002Fa>, Pasco Department, Peru (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-12249.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 20.8 x 9.5 x 8.0 cm.\u003C\u002Fdd>\n\u003Cdd>This is a bizarre columnar Chalcanthite specimen that is coated by a thin layer of the iron sulfate romerite, through which nests of sharp, bladed melanterite crystals to 6mm in size poke out every which way on all sides. According to museum records and the number on the back of the piece (19977), this dates to the time period as the Vaux expeditions of the 1920s and thus was most likely collected by Sam Gordon, then-curator, on one of the early Vaux expeditions (1st or 2nd). Sam Gordon collected the specimen in 1921 (then on the Vaux expeditions). Ex. Academy of Natural Sciences Philadelphia Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",288,400,{"id":454,"source_url":455,"license_code":391,"credit_html":456,"title":457,"description":450,"author":395,"original_width":458,"original_height":459},21090,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10159472","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10159472\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Chalcanthite-Melanterite-Romerite-202116.jpg",372,800,{"id":461,"source_url":462,"license_code":463,"credit_html":464,"title":465,"description":466,"author":467,"original_width":468,"original_height":469},73599,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=85925228","CC BY 2.0","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=85925228\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Melanterite-rich mine effluent (Mollie Kathleen Gold Mine, Cripple Creek Mining District, Colorado, USA) 5.jpg","The Cripple Creek Gold District of central Colorado is famous for its unusual gold and silver mineralization.  Precious metal mineralization occurs in the Cripple Creek Diatreme, the root zone of a deeply eroded volcano dating to the Early Oligocene (32 Ma).  The dominant lithology at Cripple Creek is phonolite, a scarce, alkaline, intermediate, extrusive igneous rock.  Cripple Creek gold can be found in its native state (Au), but it typically occurs in the form of gold telluride minerals: for example, calaverite - AuTe2, sylvanite - (Au,Ag)2Te4, petzite - Ag3AuTe2, krennerite - (Au,Ag)Te2, and nagyagite - Pb5Au(Sb,Bi)Te2S6).  Silver also occurs in some Cripple Creek minerals, including sylvanite, petzite, krennerite, hessite - Ag2Te, tennantite - (Cu,Ag,Fe,Zn)12As4S13, acanthite - Ag2S, and argentian tetrahedrite - (Cu,Fe,Ag,Zn)12Sb4S13.\n\u003Cp>The greenish material seen in the photo is melanterite-rich mine effluent, which refers to crystals forming on the walls and ceiling of mines.  This is on the ceiling of a deep subsurface gold mine in Colorado.  Mine effluent is not technically composed of minerals, because it is not natural - mines and mine tunnels are manmade constructs.  Melanterite is a greenish-colored hydrous iron sulfate, FeSO4·7H2O.  It can be naturally-occurring if it forms on weathered, natural rock surfaces.  Iron and sulfur are needed to make melanterite.  In the case seen here, the host rocks for the gold-bearing veins are pyritic phonolites.  Pyrite is iron sulfide (fool's gold), FeS2.  Oxidation in the presence of water readily breaks down pyrite.  The oxidation-hydration products include melanterite.  The brownish material in the picture is iron oxide.\n\u003C\u002Fp>\u003Cp>Geologic unit: Cripple Creek Diatreme, Early Oligocene, ~32 Ma\n\u003C\u002Fp>\u003Cp>Locality: ceiling of the 1000' Level of the Mollie Kathleen Gold Mine, east of the town of Cripple Creek, Cripple Creek Mining District, southern Teller County, central Colorado, USA (38° 45' 11.02\" North latitude, 105° 09' 37.96\" West longitude)\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>See info. at:\n\u003C\u002Fp>\nen.wikipedia.org\u002Fwiki\u002FMelanterite","James St. John",3008,2000,[471,477,483,488,493],{"id":472,"url":473,"label":474,"formula":475,"spacegroup":476,"year":355},8634,"\u002Fcif\u002F8634.cif","Mauro 2018","(Fe.925 Mg.075) S O11 H14","P 1 21\u002Fc 1",{"id":478,"url":479,"label":480,"formula":481,"spacegroup":476,"year":482},8635,"\u002Fcif\u002F8635.cif","Anderson 2007","Fe S O11 (D13.16 H.84)",2007,{"id":484,"url":485,"label":486,"formula":487,"spacegroup":476,"year":343},8636,"\u002Fcif\u002F8636.cif","Peterson 2003 · Fe S O11 H14","Fe S O11 H14",{"id":489,"url":490,"label":491,"formula":492,"spacegroup":476,"year":343},8637,"\u002Fcif\u002F8637.cif","Peterson 2003 · Fe1.8 Cu.2 S2 O22 H28","Fe1.8 Cu.2 S2 O22 H28",{"id":494,"url":495,"label":496,"formula":497,"spacegroup":476,"year":343},8638,"\u002Fcif\u002F8638.cif","Peterson 2003 · Fe1.535 Cu.415 Zn.05 S2 O22 H28","Fe1.535 Cu.415 Zn.05 S2 O22 H28",[499,500,501,502,503,504,505,506,507,508,509,510,511,512,513,514,515,516],"Alcaparossa Verde","Atramentum","Atramentum sutorium viride","Atramentum viride","Copperas","Copperasin","Eisenvitriol","Fer sulfaté","Green Vitriol","Iron Vitriol","Kupferwasser","Melanteria","Mélantérie","Melantherite","Sulphate of Iron","Vitriolum","Vitriolum viride","Vitrolo verde",[518,525,529,533,537,541,545,549,552,556,560,578,581,585,589,593,598,602,606,609,612,616,620],{"lang":519,"names":520},"ar",[521,522,523,524],"الزاج القبرصي","زاج قبرصي","كبريتات الحديدوز","ميلانتريت",{"lang":526,"names":527},"az",[528],"Melanterit",{"lang":530,"names":531},"ca",[532],"melanterita",{"lang":534,"names":535},"cs",[536],"melanterit",{"lang":538,"names":539},"de",[528,540],"Pisanit",{"lang":542,"names":543},"el",[544],"Μελαντερίτης",{"lang":546,"names":547},"es",[548],"Melanterita",{"lang":550,"names":551},"eu",[548],{"lang":553,"names":554},"fa",[555],"ملان تریت",{"lang":557,"names":558},"fi",[559],"Melanteriitti",{"lang":561,"names":562},"fr",[563,564,565,566,567,568,506,569,570,571,511,572,573,574,575,576,577],"7782-63-0","Chalcite","Chalcitris","Couperose verte","Cuprojarosite","Cuprokirovite","FeSO4,7H2O","Luckite","Luckyite","Mélantérite","Mélantérite cuprifère","Pisanite","Sommairite","Vitriol vert","Yarroshite",{"lang":579,"names":580},"hu",[536],{"lang":582,"names":583},"it",[7,584],"Vetriolo di ferro",{"lang":586,"names":587},"ja",[588],"緑礬",{"lang":590,"names":591},"nb",[592],"melanteritt",{"lang":594,"names":595},"nl",[596,597],"IJzervitriool","melanteriet",{"lang":599,"names":600},"nn",[601],"Melanteritt",{"lang":603,"names":604},"pl",[605],"Melanteryt",{"lang":607,"names":608},"sl",[528],{"lang":610,"names":611},"sv",[528],{"lang":613,"names":614},"ta",[615],"மெலண்டரைட்டு",{"lang":617,"names":618},"uk",[619],"Мелантерит",{"lang":621,"names":622},"zh",[623],"水绿矾","Q410267",{"history":11,"applications":11}]