[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:46033":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":22,"key_elements":23,"impurities":11,"cim":11,"ima_status":24,"ima_notes":11,"ima_history":11,"approval_year":26,"publication_year":27,"discovery_year":11,"strunz10ed1":28,"strunz10ed2":29,"strunz10ed3":30,"strunz10ed4":11,"dana8ed1":11,"dana8ed2":11,"dana8ed3":11,"dana8ed4":11,"csystem":31,"cclass":32,"spacegroup":33,"spacegroupset":34,"a":35,"b":11,"c":36,"alpha":11,"beta":11,"gamma":11,"aerror":37,"berror":11,"cerror":38,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":39,"z":40,"csmetamict":13,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":41,"tlform":42,"hmin":11,"hmax":11,"hardtype":11,"vhnmin":11,"vhnmax":11,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":11,"dmeas2":11,"dcalc":11,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":11,"commentluster":11,"diapheny":11,"streak":11,"colour":43,"commentcolor":11,"colors":44,"streak_colors":11,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":11,"fracturetype":11,"tenacity":11,"commentbreak":11,"opticaltype":11,"opticalsign":11,"opticalalpha":11,"opticalalpha2":11,"opticalalphaerror":11,"opticalbeta":11,"opticalbeta2":11,"opticalbetaerror":11,"opticalgamma":11,"opticalgamma2":11,"opticalgammaerror":11,"opticalomega":11,"opticalomega2":11,"opticalomegaerror":11,"opticalepsilon":11,"opticalepsilon2":11,"opticalepsilonerror":11,"opticaln":11,"opticaln2":11,"opticalnerror":11,"optical2vcalc":11,"optical2vcalc2":11,"optical2vcalcerror":11,"optical2vmeasured":11,"optical2vmeasured2":11,"optical2vmeasurederror":11,"rimin":11,"rimax":11,"opticaldispersion":11,"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":46,"thermalbehaviour":11,"other":47,"industrial":11,"occurrence":48,"otheroccurrence":11,"type_specimen_store":49,"description_short":50,"aboutname":51,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":52,"reviewed_at":11,"variety_of":11,"varieties":53,"group_members":54,"associates":55,"confused_with":56,"type_localities":57,"occurrence_total":40,"citations":64,"images":86,"structures":97,"synonyms":98,"language_names":101,"wikidata_qid":119,"texts":120},46033,"1:1:46033:2","677e6f37-8489-41a2-afe8-98456239ac0e","Centennialite","Cte",0,"mineral",null,21,false,"CaCu\u003Csub>3\u003C\u002Fsub>Cl\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>6\u003C\u002Fsub>&middot;nH\u003Csub>2\u003C\u002Fsub>O (n ~ 0.7)","CaCu\u003Csub>3\u003C\u002Fsub>Cl\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>6\u003C\u002Fsub> &middot; nH\u003Csub>2\u003C\u002Fsub>O (n ~ 0.7)",[17,18,19,20,21],"Ca","Cl","Cu","O","H",[17,18,19,20,21],[18,19],[25],"APPROVED",2013,2017,"3","D","A","Trigonal",13,97,"0","6.6606","5.8004",9,8,222.85,1,"Botryoidal encrustations.","Encrustations (often botryoidal)","Pale to azure blue",[45],"blue","Antiferromagnetic","Indivisible from the other associated Cu-bearing minerals","A secondary alteration phase, formed due to interaction of  supergene Cu mineralization with acid water","Type material is deposited in the collections of the Musée de Mineralogie, Paris, France, collection number 83080 and 14073, and the Mineral Museum of the University of Arizona, Tucson, Arizona, USA, catalogue number 19588 and 8789","Related to kapellasite, haydeeite and misakiite, but also to calumetite.\r\n\r\nProbably identical to (1) \"unidentified Cu-Ca-Cl mineral\" of Heinrich’s Mineralogy of Michigan, and (2) hexagonal basic calcium-copper hydroxychloride monohydrate of Erdös et a...","For the type locality, the Centennial mine, Calumet, Houghton County, Michigan, USA.","2025-10-29 12:29:19",[],[],[],[],[58],{"id":59,"txt":60,"latitude":61,"longitude":62,"country":63},3844,"Centennial Mine, Centennial Heights, Calumet Township, Houghton County, Michigan, USA",47.2583351,-88.4286118,"USA",[65,69,74,78,82],{"id":66,"year":67,"html":68,"doi":11},16104573,2002,"Brandes, P.T., Robinson, G.W. (2002) A Preliminary Study of Calumetite and Other Copper Chloride Mineralization on the Keweenaw Peninsula, Michigan. Unpublished MSc thesis, Michigan Technological University, USA.",{"id":70,"year":71,"html":72,"doi":73},244491,2014,"Williams, P. A., Hatert, F., Pasero, M., Mills, S. J. (2014) New minerals and nomenclature modifications approved in 2014, CNMNC Newsletter No 19. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  78 (1) 165-170 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.2014.078.1.12'>doi:10.1180\u002Fminmag.2014.078.1.12\u003C\u002Fa>","10.1180\u002Fminmag.2014.078.1.12",{"id":75,"year":76,"html":77,"doi":11},16139955,2016,"Sun, W., Huang, Y.X., Pan, Y., Mi, J.X. (2016) Synthesis and magnetic properties of centennialite: a new S= ½ Kagomé antiferromagnet and comparison with herbertsmithite and kapellasite. Physics and Chemistry of Minerals: 43: 127-136.",{"id":79,"year":27,"html":80,"doi":81},244939,"Crichton, Wilson A., Müller, Harald (2017) Centennialite, CaCu\u003Csub>3\u003C\u002Fsub>(OH)\u003Csub>6\u003C\u002Fsub>Cl\u003Csub>2\u003C\u002Fsub>.\u003Ci>n\u003C\u002Fi>H\u003Csub>2\u003C\u002Fsub>O, \u003Ci>n\u003C\u002Fi> ≈ 0.7, a new kapellasite-like species, and a reassessment of calumetite. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  81 (5) 1105-1124 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.2016.080.157'>doi:10.1180\u002Fminmag.2016.080.157\u003C\u002Fa>","10.1180\u002Fminmag.2016.080.157",{"id":83,"year":84,"html":85,"doi":11},16963571,2020,"(2020) Centennialite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fcentennialite.pdf' class='refpdflink'>\u003C\u002Fa>",[87],{"id":88,"source_url":89,"license_code":90,"credit_html":91,"title":92,"description":93,"author":94,"original_width":95,"original_height":96},4485,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=84421250","CC BY-SA 4.0","David Hospital, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=84421250\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Centennialite.jpg","Blue crystals of centennialite (IMA 2013-110) associated to minoritary green calumetite both associated to perfect halite cubes. Rudna Mine, Lubin District, Lower Silesia, Poland.","David Hospital",798,667,[],[99,100],"Centennialiet","IMA2013-110",[102,106,111,115],{"lang":103,"names":104},"ca",[105],"centennialita",{"lang":107,"names":108},"de",[109,110],"Centennialit","IMA 2013-110",{"lang":112,"names":113},"eu",[114],"Centennialita",{"lang":116,"names":117},"it",[118],"centennialite","Q19833308",{"history":11,"applications":11}]