[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:612":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":15,"elements":16,"sigelements":21,"key_elements":22,"impurities":11,"cim":23,"ima_status":24,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":27,"discovery_year":28,"strunz10ed1":29,"strunz10ed2":30,"strunz10ed3":31,"strunz10ed4":32,"dana8ed1":33,"dana8ed2":34,"dana8ed3":35,"dana8ed4":34,"csystem":36,"cclass":37,"spacegroup":37,"spacegroupset":38,"a":39,"b":40,"c":41,"alpha":42,"beta":43,"gamma":44,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":11,"csmetamict":13,"commentcrystal":11,"twinning":45,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":46,"tlform":47,"hmin":48,"hmax":48,"hardtype":11,"vhnmin":38,"vhnmax":38,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":49,"dmeas2":50,"dcalc":51,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":11,"commentluster":11,"diapheny":11,"streak":52,"colour":53,"commentcolor":54,"colors":55,"streak_colors":59,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":11,"fracturetype":60,"tenacity":61,"commentbreak":11,"opticaltype":62,"opticalsign":63,"opticalalpha":64,"opticalalpha2":38,"opticalalphaerror":11,"opticalbeta":65,"opticalbeta2":38,"opticalbetaerror":11,"opticalgamma":66,"opticalgamma2":38,"opticalgammaerror":11,"opticalomega":38,"opticalomega2":38,"opticalomegaerror":11,"opticalepsilon":38,"opticalepsilon2":38,"opticalepsilonerror":11,"opticaln":38,"opticaln2":38,"opticalnerror":11,"optical2vcalc":67,"optical2vcalc2":38,"optical2vcalcerror":11,"optical2vmeasured":68,"optical2vmeasured2":38,"optical2vmeasurederror":11,"rimin":69,"rimax":70,"opticaldispersion":71,"opticalpleochroism":72,"opticalpleochorismdesc":73,"opticalbirefringence":74,"opticalcomments":75,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":76,"opticalr":11,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":77,"industrial":11,"occurrence":11,"otheroccurrence":11,"type_specimen_store":78,"description_short":11,"aboutname":79,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":80,"reviewed_at":11,"variety_of":11,"varieties":81,"group_members":82,"associates":83,"confused_with":84,"type_localities":85,"occurrence_total":92,"citations":93,"images":113,"structures":152,"synonyms":159,"language_names":161,"wikidata_qid":184,"texts":185},612,"1:1:612:5","671a60cd-93fb-419f-b82e-39a9324515cf","Bellingerite","Blg",0,"mineral",null,144,false,"Cu\u003Csub>3\u003C\u002Fsub>(IO\u003Csub>3\u003C\u002Fsub>)\u003Csub>6\u003C\u002Fsub>·2H\u003Csub>2\u003C\u002Fsub>O","Cu\u003Csub>3\u003C\u002Fsub>(IO\u003Csub>3\u003C\u002Fsub>)\u003Csub>6\u003C\u002Fsub> · 2H\u003Csub>2\u003C\u002Fsub>O",[17,18,19,20],"Cu","O","H","I",[17,18,19,20],[17,20],"29.2",[25,26],"APPROVED","GRANDFATHERED",1940,"1940","4","K","C","05","21","1","3","Triclinic",2,"0","7.22","7.82","7.94","105","96.98","92.94","On \u003Cmi>{_101}\u003C\u002Fmi>. Reentrant angles may, or may not, be present.","Crystals prismatic [001] and rather tabular {100}. {100} striated parallel to [001].","Veinlets in altered granitic rock; tiny isolated crystals.",4,"4.88","4.9","4.932","Very light green","Green, light green; light bluish green in transmitted light","Photographs of bellingerite are frequently bluer than the natural material, similar to how the green colors of dioptase and emerald may appear in photographs.",[56,57,58],"green","blue","colorless",[56],"Sub-Conchoidal","brittle","Biaxial","+","1.89","1.900","1.99","40","50",1.89,1.99,"r > v strong","Visible","X = Light bluish green; Y = Light bluish green; Z = Blue-green","0.10","Absorption: Z > X = Y.","X (70°,–70°); Y (38°,175°); Z (59°,34°) [with c (0°,0°) and b∗ (0°,90°) using (φ,ρ)].","Slightly soluble in hot water. Readily soluble in dilute HCl.","Harvard University, Cambridge, Massachusetts, USA, number 95026.","Named in 1940 by Harry Berman and Caleb Wroe Wolfe for Herman Carl Bellinger [April 23, 1867 Caub, Nassau, Germany - July 27, 1941 Spokane, Washington, USA], metallurgist and general manager of the Chile Exploration Company, Chuquicamata, Chile, who submitted the first specimens to the eventual describers of the species. Bellinger was the 1941 recipient of the William Lawrence Saunders Gold Medal awarded by the Society of Mining Engineers for his innovations in mining methods. Herman Bellinger's father, Emil Hugo Bellinger, was a mining engineer and his family emigrated to Nevada, USA in 1873. In the mid-1880's, Herman Bellinger worked with, the then young, Fritz Augustus Heinze, who was a founder of the Anaconda Mining Company in Butte, Montana, USA. In 1897, Bellinger established a summer residence in Spokane, Washington, USA where he was a metallugist with the Trail Smelter which processed the Le Roi Mining Company's ores from Rossland, British Columbia. In 1906, Bellinger was still working at Crofton, British Columbia, Canada. By 1913, Bellinger was manager of the Great Cobar Limited in Australia. Beginning in 1916, Bellinger worked with the Chile Exploration Company. His professional assignments were far reaching including Utah, Europe, and Africa mining areas. Herman and Bertha Mae Bellinger also maintained a home in New York City. (In 1924, Bertha Mae Atherton Bellinger inherited a home in Moran Prairie, Washington and the house is now an historical museum.)","2025-08-11 12:14:18",[],[],[],[],[86],{"id":87,"txt":88,"latitude":89,"longitude":90,"country":91},641,"Chuquicamata Mine, Chuquicamata District, Calama, El Loa Province, Antofagasta, Chile",-22.2894444,-68.9011111,"Chile",1,[94,97,101,105,109],{"id":95,"year":27,"html":96,"doi":11},521039,"Berman, Harry, Wolfe, C. W. (1940) Bellingerite, a new mineral from Chuquicamata, Chile. \u003Ci>American Mineralogist\u003C\u002Fi>,  25 (8) 505-512 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM25\u002FAM25_505.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":98,"year":99,"html":100,"doi":11},16102691,1941,"Motter, W.D.B. Jr. (1941) Herman Carl Bellinger. Bolitin Minero de la Sociadad Nacional de la Mineria: 53: 392-393.",{"id":102,"year":103,"html":104,"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":106,"year":107,"html":108,"doi":11},16102693,1974,"Ghose, S., Wan, C. (1974) Structural chemistry of copper and zinc minerals. II. Stereochemistry of copper(II) and iodine(V) in bellingerite, 3Cu(IO3)2·2H2O. Acta Crystallographica: B30: 965-974.",{"id":110,"year":111,"html":112,"doi":11},16963172,2005,"(2005) Bellingerite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fbellingerite.pdf' class='refpdflink'>\u003C\u002Fa>",[114,124,130,140,146],{"id":115,"source_url":116,"license_code":117,"credit_html":118,"title":119,"description":120,"author":121,"original_width":122,"original_height":123},2987,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=8863951","CC BY 3.0","Maurizio Dini, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=8863951\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Bellingerite - Chuquicamata District, Calama, El Loa Province, Antofagasta Region, Chile.jpg","A single tabular almost perfect light green \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBellingerite\" class=\"extiw\" title=\"en:Bellingerite\">Bellingerite\u003C\u002Fa> (nearly 2 mm.) with a diminute \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGypsum\" class=\"extiw\" title=\"en:Gypsum\">Gypsum\u003C\u002Fa> xtl beside, gently perched on matrix. The typical striations of this species may be seen along the xtl. From Chuquicamata pit, Chuquicamata District, El Loa Province, Antofagasta Region, Chile. Fov: 3x3 mm. aprox","Maurizio Dini",640,480,{"id":125,"source_url":126,"license_code":117,"credit_html":127,"title":128,"description":129,"author":121,"original_width":122,"original_height":123},2988,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=45114876","Maurizio Dini, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=45114876\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Bellingerite-245071.jpg","A single tabular almost perfect light green Bellingerite (nearly 2 mm.) with a diminute Gypsum xx beside, gently poached on matrix. The typical striations of this specie may be seen along the xx, and according to the reflections of bulb lightening. From Chuquicamata pit, Chuquicamata District, El Loa Province, Antofagasta Region, Chile.",{"id":131,"source_url":132,"license_code":133,"credit_html":134,"title":135,"description":136,"author":137,"original_width":138,"original_height":139},2989,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=46091308","CC BY-SA 3.0","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=46091308\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Bellingerite, Leightonite-662308.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBellingerite\" class=\"extiw\" title=\"en:Bellingerite\">Bellingerite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FLeightonite\" class=\"extiw\" title=\"en:Leightonite\">Leightonite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Chuquicamata Mine, Chuquicamata District, Calama, El Loa Province, Antofagasta Region, Chile\u003C\u002Fdd>\n\u003Cdd>Size: 13.8 cm x 6.9 cm x 4.8 cm\u003C\u002Fdd>\n\u003Cdd>Bellingerite is a very rare hydrated Cu-iodate, unique to the world's largest copper mine. Clusters of translucent, light and dark, turquoise-blue lathes cover the matrix on this exceptional and rich large specimen. The crystals reach about 6 mm. The larger light bluish-green crystals are leightonite and the smaller darker green crystals appear to be bellingerite. Very rare in this richness, size and quality. Probably older material, but no proof. It was discovered in 1940. Ex. Carl Davis Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Robert M. Lavinsky",465,281,{"id":141,"source_url":142,"license_code":133,"credit_html":143,"title":144,"description":136,"author":137,"original_width":138,"original_height":145},2990,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=46091310","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=46091310\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Bellingerite, Leightonite-662309.jpg",426,{"id":147,"source_url":148,"license_code":133,"credit_html":149,"title":150,"description":136,"author":137,"original_width":138,"original_height":151},2991,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=46091313","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=46091313\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Bellingerite, Leightonite-662310.jpg",306,[153],{"id":154,"url":155,"label":156,"formula":157,"spacegroup":158,"year":107},1366,"\u002Fcif\u002F1366.cif","Ghose 1974","Cu3 I6 O20 H4","P -1",[160],"Bellingeriet",[162,166,170,174,178,181],{"lang":163,"names":164},"ca",[165],"bel·lingerita",{"lang":167,"names":168},"de",[169],"Bellingerit",{"lang":171,"names":172},"eu",[173],"Bellingerita",{"lang":175,"names":176},"fr",[177],"bellingerite",{"lang":179,"names":180},"it",[7],{"lang":182,"names":183},"pt",[177],"Q3637798",{"history":11,"applications":11}]