[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:3509":3},{"id":4,"longid":5,"guid":6,"name":7,"shortcode_ima":8,"entrytype":9,"entrytype_text":10,"varietyof":11,"synid":11,"polytypeof":11,"groupid":11,"weighting":12,"nolocadd":13,"blacklisted":13,"mindat_formula":14,"mindat_formula_note":11,"ima_formula":14,"elements":15,"sigelements":20,"key_elements":21,"impurities":11,"cim":22,"ima_status":23,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":26,"discovery_year":27,"strunz10ed1":28,"strunz10ed2":29,"strunz10ed3":30,"strunz10ed4":31,"dana8ed1":32,"dana8ed2":33,"dana8ed3":33,"dana8ed4":33,"csystem":34,"cclass":35,"spacegroup":36,"spacegroupset":37,"a":38,"b":39,"c":40,"alpha":37,"beta":37,"gamma":37,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":41,"csmetamict":13,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":42,"tlform":43,"hmin":44,"hmax":44,"hardtype":11,"vhnmin":37,"vhnmax":37,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":45,"dmeas2":46,"dcalc":47,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":48,"lustretype":48,"commentluster":11,"diapheny":49,"streak":11,"colour":50,"commentcolor":11,"colors":51,"streak_colors":11,"luminescence":11,"uv":55,"cleavage":56,"cleavagetype":57,"fracturetype":11,"tenacity":11,"commentbreak":11,"opticaltype":58,"opticalsign":59,"opticalalpha":60,"opticalalpha2":37,"opticalalphaerror":11,"opticalbeta":61,"opticalbeta2":37,"opticalbetaerror":11,"opticalgamma":62,"opticalgamma2":37,"opticalgammaerror":11,"opticalomega":37,"opticalomega2":37,"opticalomegaerror":11,"opticalepsilon":37,"opticalepsilon2":37,"opticalepsilonerror":11,"opticaln":37,"opticaln2":37,"opticalnerror":11,"optical2vcalc":63,"optical2vcalc2":37,"optical2vcalcerror":11,"optical2vmeasured":37,"optical2vmeasured2":64,"optical2vmeasurederror":11,"rimin":65,"rimax":66,"opticaldispersion":67,"opticalpleochroism":68,"opticalpleochorismdesc":69,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":70,"opticalr":11,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":71,"industrial":11,"occurrence":72,"otheroccurrence":11,"type_specimen_store":73,"description_short":74,"aboutname":75,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":76,"reviewed_at":11,"variety_of":11,"varieties":77,"group_members":78,"associates":79,"confused_with":80,"type_localities":81,"occurrence_total":91,"citations":92,"images":113,"structures":173,"synonyms":180,"language_names":182,"wikidata_qid":205,"texts":206},3509,"1:1:3509:1","d1869cb4-726f-4a69-931c-e2c9b28bfcfe","Salesite","Sls",0,"mineral",null,405,false,"Cu(IO\u003Csub>3\u003C\u002Fsub>)(OH)",[16,17,18,19],"Cu","O","H","I",[16,17,18,19],[16,19],"29.1",[24,25],"APPROVED","GRANDFATHERED",1939,"1939","4","K","B","05","22","1","Orthorhombic",8,71,"0","10.794","6.708","4.781",4,"Crystals stout prismatic [001] with pyramidal terminations.  Forms include {001}, {010}, {130}, {110}, {023}, {011}, {111}.","Stout, prismatic crystals with a pyramidal termination.",3,"4.72","4.82","4.888","Vitreous","Transparent","Bluish-green; bluish green in transmitted light",[52,53,54],"blue","green","colorless","None","on {101}","Perfect","Biaxial","-","1.786","2.070","2.075","12","5",1.786,2.075,"r > v, extreme.","Visible","X = Colourless\r\nY = Light bluish green\r\nZ = Bluish green","X = c; Y = b; Z = a.","Insoluble in water. Readily soluble in HNO3.\r\n\r\nIn a closed tube, when first heated, it snaps into small splinters and almost at once gives copious purple fumes of iodine that crystallize on the wall of the tube. A small amount of water is also given off.\r\n\r\nIn forceps, heated gradually, it darkens and yields a clear green flame of copper iodide without fusing. The residue left after heating on charcoal is readily reduced to metallic copper.","Oxidized zone of copper deposit in an arid climate.","Harvard University, Cambridge, Massachusetts, USA, number 95027.","Attempts at synthesis gave an orthorhombic dimorph, differing in cleavage and optical properties with respect to salesite (Palache and Jarrell, 1939).","Named after Reno Haber Sales (10 September 1876, Storm Lake, Iowa, USA - 9 May 1969, Bozeman, Montana, USA), chief geologist, Anaconda Copper Company, Chile. He was awarded the Penrose Award of the Society of Economic Geologists in 1939.","2025-08-11 12:14:23",[],[],[],[],[82,88],{"id":83,"txt":84,"latitude":85,"longitude":86,"country":87},641,"Chuquicamata Mine, Chuquicamata District, Calama, El Loa Province, Antofagasta, Chile",-22.2894444,-68.9011111,"Chile",{"id":89,"txt":90,"latitude":11,"longitude":11,"country":87},646,"Cachinal, Antofagasta Province, Antofagasta, Chile",2,[93,96,100,105,109],{"id":94,"year":26,"html":95,"doi":11},520898,"Palache, Charles, Jarrell, O. W. (1939) Salesite, a new mineral from Chuquicamata, Chile. \u003Ci>American Mineralogist\u003C\u002Fi>,  24 (6) 388-392 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM24\u002FAM24_388.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":97,"year":98,"html":99,"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":101,"year":102,"html":103,"doi":104},614034,1962,"Ghose, S. (1962) The crystal structure of salesite, CuIO)3(OH). \u003Ci>Acta Crystallographica\u003C\u002Fi>,  15 (11). 1105-1109 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1107\u002Fs0365110x62002959'>doi:10.1107\u002Fs0365110x62002959\u003C\u002Fa>","10.1107\u002Fs0365110x62002959",{"id":106,"year":107,"html":108,"doi":11},526995,1978,"Ghose, Subrata, Wan, Che'ng (1978) Salesite, CuIO3(OH), and Cu(IO3)2·2H2O: a comparison of the crystal structures and their magnetic behavior. \u003Ci>American Mineralogist\u003C\u002Fi>,  63 (1-2). 172-179 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM63\u002FAM63_172.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":110,"year":111,"html":112,"doi":11},16967125,2005,"(2005) Salesite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fsalesite.pdf' class='refpdflink'>\u003C\u002Fa>",[114,124,131,138,144,154,164],{"id":115,"source_url":116,"license_code":117,"credit_html":118,"title":119,"description":120,"author":121,"original_width":122,"original_height":123},21451,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10138994","CC BY-SA 3.0","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10138994\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Salesite-118013.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSalesite\" class=\"extiw\" title=\"en:Salesite\">Salesite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Chuquicamata Mine, Chuquicamata District, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCalama\" class=\"extiw\" title=\"en:Calama\">Calama\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FEl_Loa_Province\" class=\"extiw\" title=\"en:El Loa Province\">El Loa Province\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAntofagasta_Region\" class=\"extiw\" title=\"en:Antofagasta Region\">Antofagasta Region\u003C\u002Fa>, Chile (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-641.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 6.6 x 6.4 x 5.0 cm.\u003C\u002Fdd>\n\u003Cdd>Salesite is an ULTRA RARE copper iodate found worldwide at only two mines in Chile. This impressive specimen, from the Type Locality, has RICH coverage of large for the species, lustrous, prismatic crystals to 3 mm. The striking bluish-green color is impressive.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Robert M. Lavinsky",600,465,{"id":125,"source_url":126,"license_code":117,"credit_html":127,"title":128,"description":120,"author":121,"original_width":129,"original_height":130},21452,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10138995","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10138995\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Salesite-118014.jpg",500,420,{"id":132,"source_url":133,"license_code":117,"credit_html":134,"title":135,"description":136,"author":121,"original_width":122,"original_height":137},21453,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10171853","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10171853\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Salesite-278377.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSalesite\" class=\"extiw\" title=\"en:Salesite\">Salesite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Chuquicamata Mine, Chuquicamata District, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCalama\" class=\"extiw\" title=\"en:Calama\">Calama\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FEl_Loa_Province\" class=\"extiw\" title=\"en:El Loa Province\">El Loa Province\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAntofagasta_Region\" class=\"extiw\" title=\"en:Antofagasta Region\">Antofagasta Region\u003C\u002Fa>, Chile (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-641.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 5.4 x 3.4 x 1.8 cm.\u003C\u002Fdd>\n\u003Cdd>Salesite is a very rare copper iodate found worldwide at only two mines in Chile. This impressive specimen, from the famous Co-Type Locality, has rich coverage on both sides of large for the species, lustrous, prismatic crystals to 3 mm. The striking bluish-green color is impressive against the porphry matrix.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",459,{"id":139,"source_url":140,"license_code":117,"credit_html":141,"title":142,"description":136,"author":121,"original_width":122,"original_height":143},21454,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10171855","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10171855\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Salesite-278378.jpg",508,{"id":145,"source_url":146,"license_code":147,"credit_html":148,"title":149,"description":150,"author":151,"original_width":152,"original_height":153},21455,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118193103","CC BY-SA 2.0","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118193103\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Salesite (49055214263).jpg","\u003Cp>Chuquicamata Mine\n\u003C\u002Fp>\nChile","Pacific Museum of Earth from Canada",4000,6000,{"id":155,"source_url":156,"license_code":157,"credit_html":158,"title":159,"description":160,"author":161,"original_width":162,"original_height":163},21456,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=138522038","CC0 1.0","Luigi Chiappino, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=138522038\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cristal de salesitaa.jpg","Cristal de salesita","Luigi Chiappino",634,507,{"id":165,"source_url":166,"license_code":157,"credit_html":167,"title":168,"description":169,"author":170,"original_width":171,"original_height":172},21457,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163475173","Darla Sondrol, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163475173\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Salesite (GeoDIL number - 155).jpg","Salesite, a rare mineral containing iodine, has the formula Cu(IO3)(OH). Here we see salesite (the greenish mineral on the surface of an altered carbonate rich rock). The source of this sample is uncertain, but it comes from Chile, perhaps from the Chuquicamata mining district (one of the few places where salesite is found). This sample is about 8 cm across.","Darla Sondrol",2590,1256,[174],{"id":175,"url":176,"label":177,"formula":178,"spacegroup":179,"year":107},12349,"\u002Fcif\u002F12349.cif","Ghose 1978","Cu I O4 H","P n m a",[181],"Salesiet",[183,187,191,195,198,201],{"lang":184,"names":185},"ca",[186],"salesita",{"lang":188,"names":189},"de",[190],"Salesit",{"lang":192,"names":193},"es",[194],"Salesita",{"lang":196,"names":197},"eu",[194],{"lang":199,"names":200},"it",[7],{"lang":202,"names":203},"uk",[204],"Сейлзит","Q3945473",{"history":11,"applications":11}]