[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:40566":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":11,"ima_formula":16,"elements":17,"sigelements":23,"key_elements":24,"impurities":11,"cim":11,"ima_status":25,"ima_notes":11,"ima_history":11,"approval_year":27,"publication_year":28,"discovery_year":11,"strunz10ed1":29,"strunz10ed2":30,"strunz10ed3":30,"strunz10ed4":11,"dana8ed1":11,"dana8ed2":11,"dana8ed3":11,"dana8ed4":11,"csystem":31,"cclass":32,"spacegroup":33,"spacegroupset":34,"a":35,"b":36,"c":37,"alpha":11,"beta":38,"gamma":11,"aerror":39,"berror":40,"cerror":41,"alphaerror":11,"betaerror":42,"gammaerror":11,"va3":11,"z":11,"csmetamict":14,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":43,"tlform":44,"hmin":45,"hmax":45,"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":46,"lustre":11,"lustretype":47,"commentluster":11,"diapheny":48,"streak":49,"colour":50,"commentcolor":11,"colors":51,"streak_colors":54,"luminescence":11,"uv":11,"cleavage":55,"cleavagetype":11,"fracturetype":11,"tenacity":56,"commentbreak":11,"opticaltype":57,"opticalsign":58,"opticalalpha":59,"opticalalpha2":11,"opticalalphaerror":40,"opticalbeta":60,"opticalbeta2":11,"opticalbetaerror":40,"opticalgamma":61,"opticalgamma2":11,"opticalgammaerror":62,"opticalomega":11,"opticalomega2":11,"opticalomegaerror":11,"opticalepsilon":11,"opticalepsilon2":11,"opticalepsilonerror":11,"opticaln":11,"opticaln2":11,"opticalnerror":11,"optical2vcalc":63,"optical2vcalc2":11,"optical2vcalcerror":11,"optical2vmeasured":64,"optical2vmeasured2":11,"optical2vmeasurederror":65,"rimin":66,"rimax":67,"opticaldispersion":68,"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":11,"industrial":11,"occurrence":69,"otheroccurrence":11,"type_specimen_store":70,"description_short":71,"aboutname":72,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":73,"reviewed_at":11,"variety_of":11,"varieties":74,"group_members":75,"associates":89,"confused_with":90,"type_localities":91,"occurrence_total":41,"citations":102,"images":120,"structures":121,"synonyms":128,"language_names":131,"wikidata_qid":149,"texts":150},40566,"1:1:40566:3","64740783-e6f8-41e9-9047-9c76801e3f02","Ferroericssonite","Fers",0,"mineral",null,40565,59,false,"BaFe\u003Csup>2+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub> Fe\u003Csup>3+\u003C\u002Fsup>(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>)O(OH) ","BaFe\u003Csup>2+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>)O(OH)",[18,19,20,21,22],"Ba","Fe","Si","O","H",[18,19,20,21,22],[18],[26],"APPROVED",2010,2011,"9","0","Monoclinic",5,11,"C2\u002Fm ","20.3459","7.0119","5.3879","94.874",10,3,4,7,"Flattened on {100} and elongate and striated parallel to [001]. ","Crystals occur in dark reddish brown foliated masses of irregular, undulating striated blades up to several mm in length. ",4.5,"Calculated densities : 4.445 and 4.413 g\u002Fcm3 on the basis of the empirical formulas for Esquire #7 and Esquire #8 material, respectively","Vitreous","Transparent","Brown","Dark reddish brown",[52,53],"brown","red",[52],"Two cleavages: {100} perfect and {011} good","brittle","Biaxial","+","1.827","1.845","1.920",6,"63.0","63",2,1.827,1.92,"Parallel, r \u003C v","As late stage mineral in a sequence of minerals resulting from fluids interacting with a quartz–sanbornite vein along its margin with the country rock.","Natural History Museum of Los Angeles County, Los Angeles, California, USA, (63206 - Esquire 7 and 63207 - Esquire 8).","Fe2+ analogue to ericssonite.","Named for being the Fe2+ analogue of \u003Cm>ericssonite\u003C\u002Fm>. The root name is for John Ericsson (31 July 1803, Långbanshyttan, Värmland, Sweden – 8 March 1889, New York, USA), an inventor and mechanical engineer.","2025-08-11 12:15:07",[],[76,83],{"id":77,"name":78,"entrytype":9,"csystem":31,"ima_formula":79,"mindat_formula":79,"hmin":45,"hmax":45,"dmeas":80,"dcalc":81,"primary_image_id":82},1397,"Ericssonite","BaMn\u003Csup>2+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>)O(OH)","4.21","4.38",7952,{"id":84,"name":85,"entrytype":9,"csystem":86,"ima_formula":87,"mindat_formula":87,"hmin":45,"hmax":45,"dmeas":11,"dcalc":11,"primary_image_id":88},55043,"Zinkgruvanite","Triclinic","Ba\u003Csub>4\u003C\u002Fsub>Mn\u003Csup>2+\u003C\u002Fsup>\u003Csub>4\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>O\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>",28826,[],[],[92,98],{"id":93,"txt":94,"latitude":95,"longitude":96,"country":97},8237,"Esquire No. 7 claim, Big Creek, Big Creek-Rush Creek Mining District, Fresno County, California, USA",36.9166667,-119.245,"USA",{"id":99,"txt":100,"latitude":95,"longitude":101,"country":97},25573,"Esquire No. 8 claim, Big Creek, Big Creek-Rush Creek Mining District, Fresno County, California, USA",-119.2455556,[103,107,111,116],{"id":104,"year":27,"html":105,"doi":106},4564703,"Williams, P. A., Hatert, F., Pasero, M., Mills, S. J. (2010) IMA Commission on New Minerals, Nomenclature and Classification (CNMNC) CNMNC Newsletter No 4. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  74 (4) 797-800 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fs0026461x00038925'>doi:10.1180\u002Fs0026461x00038925\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Forbi.uliege.be\u002Fbitstream\u002F2268\u002F77812\u002F1\u002FCNMNC%20NEWSLETTER%204.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fs0026461x00038925",{"id":108,"year":28,"html":109,"doi":110},64879,"Kampf, A. R., Roberts, A. C., Venance, K. E., Dunning, G. E., Walstrom, R. E. (2011) Ferroericssonite, the Fe\u003Csup>2+\u003C\u002Fsup> analogue of ericssonite, from eastern Fresno County, California, USA. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  49 (2). 587-594 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3749\u002Fcanmin.49.2.587'>doi:10.3749\u002Fcanmin.49.2.587\u003C\u002Fa>","10.3749\u002Fcanmin.49.2.587",{"id":112,"year":113,"html":114,"doi":115},65198,2014,"Sokolova, Elena, Cámara, Fernando (2014) From structure topology to chemical composition. XVII. Fe\u003Csup>3+\u003C\u002Fsup> versus Ti\u003Csup>4+\u003C\u002Fsup>: The topology of the HOH layer in ericssonite-2O, Ba\u003Csub>2\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>Mn\u003Csub>4\u003C\u002Fsub>(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>O\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>, ferroericssonite, Ba\u003Csub>2\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>Fe\u003Csup>2+\u003C\u002Fsup>\u003Csub>4\u003C\u002Fsub>(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>O\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>, and yoshimuraite, Ba\u003Csub>4\u003C\u002Fsub>Ti\u003Csup>4+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>Mn\u003Csub>4\u003C\u002Fsub>(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>O\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  52 (3) 569-576 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3749\u002Fcanmin.52.3.569'>doi:10.3749\u002Fcanmin.52.3.569\u003C\u002Fa>","10.3749\u002Fcanmin.52.3.569",{"id":117,"year":118,"html":119,"doi":11},16964288,2017,"(2017) Ferroericssonite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fferroericssonite.pdf' class='refpdflink'>\u003C\u002Fa>",[],[122],{"id":123,"url":124,"label":125,"formula":126,"spacegroup":127,"year":28},4557,"\u002Fcif\u002F4557.cif","Kampf 2011","Ba Fe3 Si2 O8.77 (Cl.23 H.77)","C 1 2\u002Fm 1",[129,130],"Ferroericssoniet","IMA2010-025",[132,136,141,145],{"lang":133,"names":134},"ca",[135],"ferroericssonita",{"lang":137,"names":138},"de",[139,140],"Ferroericssonit","IMA 2010-025",{"lang":142,"names":143},"eu",[144],"Ferroericssonita",{"lang":146,"names":147},"it",[148],"ferroericssonite","Q19833636",{"history":11,"applications":11}]