[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:53168":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":15,"elements":16,"sigelements":21,"key_elements":11,"impurities":11,"cim":11,"ima_status":22,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":24,"discovery_year":11,"strunz10ed1":25,"strunz10ed2":26,"strunz10ed3":27,"strunz10ed4":28,"dana8ed1":11,"dana8ed2":11,"dana8ed3":11,"dana8ed4":11,"csystem":29,"cclass":30,"spacegroup":11,"spacegroupset":31,"a":32,"b":33,"c":34,"alpha":11,"beta":11,"gamma":11,"aerror":35,"berror":35,"cerror":36,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":37,"csmetamict":14,"commentcrystal":38,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":39,"tlform":40,"hmin":11,"hmax":11,"hardtype":11,"vhnmin":11,"vhnmax":11,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":41,"dmeas2":41,"dcalc":42,"dmeaserror":11,"dcalcerror":11,"commentdense":43,"lustre":11,"lustretype":11,"commentluster":11,"diapheny":11,"streak":11,"colour":44,"commentcolor":11,"colors":45,"streak_colors":11,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":11,"fracturetype":11,"tenacity":11,"commentbreak":11,"opticaltype":50,"opticalsign":51,"opticalalpha":52,"opticalalpha2":11,"opticalalphaerror":36,"opticalbeta":53,"opticalbeta2":11,"opticalbetaerror":11,"opticalgamma":54,"opticalgamma2":11,"opticalgammaerror":36,"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":55,"optical2vmeasured2":11,"optical2vmeasurederror":35,"rimin":56,"rimax":57,"opticaldispersion":58,"opticalpleochroism":59,"opticalpleochorismdesc":60,"opticalbirefringence":11,"opticalcomments":61,"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":62,"otheroccurrence":11,"type_specimen_store":63,"description_short":64,"aboutname":65,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":66,"reviewed_at":11,"variety_of":11,"varieties":67,"group_members":68,"associates":107,"confused_with":108,"type_localities":109,"occurrence_total":116,"citations":117,"images":127,"structures":128,"synonyms":129,"language_names":132,"wikidata_qid":146,"texts":147},53168,"1:1:53168:5","d4ad1bb5-2d6b-49c0-b50f-c877b5b68453","Ferrirockbridgeite","Frck",0,"mineral",null,39395,17,false,"(Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>0.67\u003C\u002Fsub>◻\u003Csub>0.33\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(Fe\u003Csup>3+\u003C\u002Fsup>)\u003Csub>3\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>3\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub>(H\u003Csub>2\u003C\u002Fsub>O)",[17,18,19,20],"Fe","O","P","H",[17,18,19,20],[23],"APPROVED",2019,"8","B","C","10","Orthorhombic",8,"0","13.853","16.928","5.1917",1,5,4,"space group is Bbmm","Blade-like crystals, flattened on {010} and elongated on [001].","Radial fibrous crusts and masses.  Compact intergrowths of reddish-brown blade-like crystals.","3.33","3.42","Measured using Berman balance with toluene.  The low measured value is due to sub-micron porosity.","Reddish-brown",[46,47,48,49],"brown","red","yellow","green","Biaxial","-","1.875","1.890","1.900","78",1.875,1.9,"Strong, with r > v","Visible","X = yellow brown, Y = olive brown, Z = dark olive green","β calculated.\r\nOrientation: X = c, Y = a, Z = b.\r\nAbsorption: Z > Y > X.","Oxidized zone of a granitic pegmatite.  Highly oxidized alteration of triphylite.","Collections of the Mineralogical and Geological Museum, Harvard University, 20 Oxford Street, Cambridge, MA 02138, USA, catalogue number 95086.","Fe3+-vacancy-analogue of ferrorockbridgeite. One of few known fully ferric-iron hydrous hydrated phosphate minerals, chemically comparable to allanpringite, beraunite, ferristrunzite, santabarbaraite, and tinticite.","For the root name of rockbridgeite and the ferric iron content.","2025-08-11 12:15:21",[],[69,76,84,91,100],{"id":70,"name":71,"entrytype":9,"csystem":29,"ima_formula":72,"mindat_formula":73,"hmin":11,"hmax":11,"dmeas":74,"dcalc":75,"primary_image_id":11},52914,"Ferrorockbridgeite","(Fe\u003Csup>2+\u003C\u002Fsup>,Mn\u003Csup>2+\u003C\u002Fsup>)\u003Csub>2\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>3\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub>(H\u003Csub>2\u003C\u002Fsub>O)","(Fe\u003Csup>2+\u003C\u002Fsup>,Mn\u003Csup>2+\u003C\u002Fsup>)\u003Csub>2\u003C\u002Fsub>(Fe\u003Csup>3+\u003C\u002Fsup>)\u003Csub>3\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>3\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub>(H\u003Csub>2\u003C\u002Fsub>O)","3.21","3.51",{"id":77,"name":78,"entrytype":9,"csystem":29,"ima_formula":79,"mindat_formula":79,"hmin":80,"hmax":80,"dmeas":81,"dcalc":82,"primary_image_id":83},1614,"Frondelite","(Mn\u003Csup>2+\u003C\u002Fsup>\u003Csub>0.5\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>0.5\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>3\u003C\u002Fsub>(OH)\u003Csub>5\u003C\u002Fsub>",4.5,"3.453","3.35",9448,{"id":85,"name":86,"entrytype":9,"csystem":87,"ima_formula":88,"mindat_formula":88,"hmin":11,"hmax":11,"dmeas":11,"dcalc":89,"primary_image_id":90},470690,"Manganrockbridgeite","Monoclinic","Mn\u003Csup>2+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>3\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub>(H\u003Csub>2\u003C\u002Fsub>O)","3.40",15382,{"id":92,"name":93,"entrytype":9,"csystem":29,"ima_formula":94,"mindat_formula":95,"hmin":96,"hmax":37,"dmeas":97,"dcalc":98,"primary_image_id":99},36041,"Plimerite","Zn\u003Csub>2\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>3\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub>(H\u003Csub>2\u003C\u002Fsub>O)","ZnFe\u003Csup>3+\u003C\u002Fsup>\u003Csub>4\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>3\u003C\u002Fsub>(OH)\u003Csub>5\u003C\u002Fsub>",3.5,"3.67","3.62",19605,{"id":101,"name":102,"entrytype":9,"csystem":29,"ima_formula":103,"mindat_formula":103,"hmin":96,"hmax":80,"dmeas":104,"dcalc":105,"primary_image_id":106},3433,"Rockbridgeite","(Fe\u003Csup>2+\u003C\u002Fsup>\u003Csub>0.5\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>0.5\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>3\u003C\u002Fsub>(OH)\u003Csub>5\u003C\u002Fsub>","3.45","3.60",77132,[],[],[110],{"id":111,"txt":112,"latitude":113,"longitude":114,"country":115},3942,"Palermo No. 1 Mine, Groton, Grafton County, New Hampshire, USA",43.7512952,-71.889562,"USA",2,[118,123],{"id":119,"year":120,"html":121,"doi":122},16080084,2018,"Hålenius, U., Hatert, F., Pasero, M., Mills, S. J. (2018) CNMNC Newsletter 45, New minerals and nomenclature modifications approved in 2018. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  82 (5) 1225-1232 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fmgm.2018.160'>doi:10.1180\u002Fmgm.2018.160\u003C\u002Fa>","10.1180\u002Fmgm.2018.160",{"id":124,"year":24,"html":125,"doi":126},129839,"Grey, Ian Edward, Kampf, Anthony R., Keck, Erich, Cashion, John D., MacRae, Colin M., Gozukara, Yesim, Shanks, Finlay L. (2019) Ferrirockbridgeite, (Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>0.67\u003C\u002Fsub>□\u003Csub>0.33\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(Fe\u003Csup>3+\u003C\u002Fsup>)\u003Csub>3\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>3\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub>(H\u003Csub>2\u003C\u002Fsub>O), and the oxidation mechanism for rockbridgeite-group minerals. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  31 (3) 585-594 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1127\u002Fejm\u002F2019\u002F0031-2846'>doi:10.1127\u002Fejm\u002F2019\u002F0031-2846\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FEJM31_585.pdf' class='refpdflink'>\u003C\u002Fa>","10.1127\u002Fejm\u002F2019\u002F0031-2846",[],[],[130,131],"Ferrirockbridgeiet","IMA2018-065",[133,137,142],{"lang":134,"names":135},"ca",[136],"ferrirockbridgeïta",{"lang":138,"names":139},"de",[140,141],"Ferrirockbridgeit","IMA 2018-065",{"lang":143,"names":144},"eu",[145],"Ferrirockbridgeita","Q57812616",{"history":11,"applications":11}]