[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:31726":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":11,"impurities":11,"cim":11,"ima_status":22,"ima_notes":11,"ima_history":11,"approval_year":24,"publication_year":24,"discovery_year":25,"strunz10ed1":26,"strunz10ed2":27,"strunz10ed3":28,"strunz10ed4":29,"dana8ed1":30,"dana8ed2":31,"dana8ed3":31,"dana8ed4":32,"csystem":33,"cclass":34,"spacegroup":34,"spacegroupset":35,"a":36,"b":37,"c":38,"alpha":39,"beta":40,"gamma":41,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":11,"csmetamict":13,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":11,"tlform":42,"hmin":11,"hmax":11,"hardtype":11,"vhnmin":35,"vhnmax":35,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":35,"dmeas2":35,"dcalc":43,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":11,"commentluster":11,"diapheny":44,"streak":45,"colour":46,"commentcolor":11,"colors":47,"streak_colors":50,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":11,"fracturetype":11,"tenacity":11,"commentbreak":11,"opticaltype":11,"opticalsign":11,"opticalalpha":35,"opticalalpha2":35,"opticalalphaerror":11,"opticalbeta":35,"opticalbeta2":35,"opticalbetaerror":11,"opticalgamma":35,"opticalgamma2":35,"opticalgammaerror":11,"opticalomega":35,"opticalomega2":35,"opticalomegaerror":11,"opticalepsilon":35,"opticalepsilon2":35,"opticalepsilonerror":11,"opticaln":35,"opticaln2":35,"opticalnerror":11,"optical2vcalc":35,"optical2vcalc2":35,"optical2vcalcerror":11,"optical2vmeasured":35,"optical2vmeasured2":35,"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":51,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":52,"other":11,"industrial":11,"occurrence":53,"otheroccurrence":11,"type_specimen_store":54,"description_short":55,"aboutname":56,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":57,"reviewed_at":11,"variety_of":11,"varieties":58,"group_members":59,"associates":60,"confused_with":70,"type_localities":71,"occurrence_total":34,"citations":78,"images":126,"structures":127,"synonyms":144,"language_names":146,"wikidata_qid":168,"texts":169},31726,"1:1:31726:1","e6804acf-4207-4c5d-ae3b-503f88465e58","Meridianiite","Mdn",0,"mineral",null,8,false,"MgSO\u003Csub>4\u003C\u002Fsub>·11H\u003Csub>2\u003C\u002Fsub>O","Mg(SO\u003Csub>4\u003C\u002Fsub>) · 11H\u003Csub>2\u003C\u002Fsub>O",[17,18,19,20],"Mg","O","S","H",[17,18,19,20],[23],"APPROVED",2007,"2007","7","C","B","90","29","6","8","Triclinic",2,"0","6.7459","6.8173","17.299","88.137","89.481","62.719","White granular.","1.512","Transparent","White","Colorless, white",[48,49],"colorless","white",[49],"Must be stored below 2° C.","Stable only below 2° C. Above that temperature it melts incongruently to a slurry of \u003CM>epsomite\u003C\u002FM> and water.","Ponds at an abandoned MgSO4 mine, in winter.","Canadian Museum of Nature","A phase that is stable with a saturated brine or with ice and which melts above 2°C into a slurry of Epsomite and water. It has now been found occurring naturally on Earth (on the surface of a frozen pond, and in ice cores) and is suspected of existing...","The compound was originally synthesized in 1837 and is known as Fritzsche's salt. The mineral was named by Peterson, R.C., Nelson, W.,Madu, B., Shurvell, H.F. in 2007 for Meridiani Planum, the locality on Mars where the MER rover Opportunity observed crystal molds in sedimentary rock that are thought to be caused by minerals that have since dehydrated or dissolved.","2026-05-09 16:12:28",[],[],[61],{"id":62,"name":63,"entrytype":9,"csystem":64,"ima_formula":65,"mindat_formula":65,"hmin":66,"hmax":66,"dmeas":67,"dcalc":68,"primary_image_id":69},2001,"Ice","Hexagonal","H\u003Csub>2\u003C\u002Fsub>O",1.5,"0.9167","0.93",12083,[],[72],{"id":73,"txt":74,"latitude":75,"longitude":76,"country":77},145920,"Basque claims (Basque No. 1), Venables Valley, Ashcroft, Kamloops Mining Division, British Columbia, Canada",50.6002778,-121.3583333,"Canada",[79,83,88,93,96,99,103,108,113,118,122],{"id":80,"year":81,"html":82,"doi":11},16136599,1837,"Fritzsche, C.J. (1837) Ueber eine neue Verbindung der schwefelsauren Talkerde mit wasser.  Annalen der Physik und Chemie (Peggendorff's Annalen): 42: 577-580. Bulletin scientifique publié par l'Académie Impériale des Science de St. Pétersbourg: 2: 193-196. (synthetic)",{"id":84,"year":85,"html":86,"doi":87},378871,2005,"Ohno, Hiroshi, Igarashi, Makoto, Hondoh, Takeo (2005) Salt inclusions in polar ice core: Location and chemical form of water-soluble impurities. \u003Ci>Earth and Planetary Science Letters\u003C\u002Fi>,  232 (1) 171-178 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.epsl.2005.01.001'>doi:10.1016\u002Fj.epsl.2005.01.001\u003C\u002Fa>","10.1016\u002Fj.epsl.2005.01.001",{"id":89,"year":90,"html":91,"doi":92},139676,2006,"Peterson, Ronald C.; Wang, Ruiyao (2006) Crystal molds on Mars: Melting of a possible new mineral species to create Martian chaotic terrain. \u003Ci>Geology\u003C\u002Fi>,  34 (11). p.957-960. \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1130\u002Fg22678a.1'>doi:10.1130\u002Fg22678a.1\u003C\u002Fa>","10.1130\u002Fg22678a.1",{"id":94,"year":24,"html":95,"doi":11},16136603,"Genceli, F.E., Lutz, M., Spek, A.L., Witkamp, G.-J. (2007) Crystallization and Characterization of a New Magnesium Sulfate Hydrate MgSO4 · 11H2O. Crystal Growth & Design: 7: 2460-2466.",{"id":97,"year":24,"html":98,"doi":11},16136775,"Peterson, R.C., Nelson, W., Madu, B., Shurvell, H. F. (2007) Meridianiite (MgSO4·11H2O): A New Mineral Species Observed on Earth and Predicted to Exist on Mars. \u003Ci>Seventh International Conference on Mars\u003C\u002Fi>.  \u003Ca target='_blank' href='http:\u002F\u002Fwww.lpi.usra.edu\u002Fmeetings\u002F7thmars2007\u002Fpdf\u002F3124.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":100,"year":24,"html":101,"doi":102},395670,"Peterson, R.C., Nelson, W., Madu, B., Shurvell, H.F. (2007) Meridianiite: A new mineral species observed on Earth and predicted to exist on Mars. \u003Ci>American Mineralogist\u003C\u002Fi>,  92 (10) 1756-1759 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam.2007.2668'>doi:10.2138\u002Fam.2007.2668\u003C\u002Fa>","10.2138\u002Fam.2007.2668",{"id":104,"year":105,"html":106,"doi":107},153420,2008,"Fortes, A. D.; Wood, I. G.; Knight, K. S. (2008) The crystal structure and thermal expansion tensor of MgSO4–11D2O (meridianiite) determined by neutron powder diffraction. \u003Ci>Physics and Chemistry of Minerals\u003C\u002Fi>,  35 (4). p.207-221. \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs00269-008-0214-x'>doi:10.1007\u002Fs00269-008-0214-x\u003C\u002Fa>","10.1007\u002Fs00269-008-0214-x",{"id":109,"year":110,"html":111,"doi":112},5932686,2009,"Elif Genceli, F., Horikawa, Shinichirou, Iizuka, Yoshinori, Sakurai, Toshimitsu, Hondoh, Takeo, Kawamura, Toshiyuki, Witkamp, Geert-Jan (2009) Meridianiite detected in ice. \u003Ci>Journal of Glaciology\u003C\u002Fi>, 55 (189). 117-122 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3189\u002F002214309788608921'>doi:10.3189\u002F002214309788608921\u003C\u002Fa>","10.3189\u002F002214309788608921",{"id":114,"year":115,"html":116,"doi":117},153747,2012,"Fortes, A. Dominic, Browning, Frank, Wood, Ian G. (2012) Cation substitution in synthetic meridianiite (MgSO4·11H2O) I: X-ray powder diffraction analysis of quenched polycrystalline aggregates. \u003Ci>Physics and Chemistry of Minerals\u003C\u002Fi>,  39 (5) 419-441 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs00269-012-0497-9'>doi:10.1007\u002Fs00269-012-0497-9\u003C\u002Fa>","10.1007\u002Fs00269-012-0497-9",{"id":119,"year":115,"html":120,"doi":121},153749,"Fortes, A. Dominic, Browning, Frank, Wood, Ian G. (2012) Cation substitution in synthetic meridianiite (MgSO4·11H2O) II: variation in unit-cell parameters determined from X-ray powder diffraction data. \u003Ci>Physics and Chemistry of Minerals\u003C\u002Fi>,  39 (6) 443-454 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs00269-012-0498-8'>doi:10.1007\u002Fs00269-012-0498-8\u003C\u002Fa>","10.1007\u002Fs00269-012-0498-8",{"id":123,"year":124,"html":125,"doi":11},16965958,2021,"(2021) Meridianiite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002FMeridianiite.pdf' class='refpdflink'>\u003C\u002Fa>",[],[128,135,140],{"id":129,"url":130,"label":131,"formula":132,"spacegroup":133,"year":134},8681,"\u002Fcif\u002F8681.cif","Fortes 2013","Mg S O15 H22","P -1",2013,{"id":136,"url":137,"label":138,"formula":139,"spacegroup":133,"year":105},8682,"\u002Fcif\u002F8682.cif","Fortes 2008","Mg S O15 D22",{"id":141,"url":142,"label":143,"formula":132,"spacegroup":133,"year":24},8684,"\u002Fcif\u002F8684.cif","Genceli 2007",[145],"IMA2007-011",[147,151,156,160,164],{"lang":148,"names":149},"ca",[150],"meridianiita",{"lang":152,"names":153},"de",[154,155],"IMA 2007-011","Meridianiit",{"lang":157,"names":158},"eu",[159],"Meridianiita",{"lang":161,"names":162},"fr",[163],"Méridianiite",{"lang":165,"names":166},"nl",[167],"Meridianiiet","Q2547694",{"history":11,"applications":11}]