[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:46440":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":24,"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":31,"strunz10ed4":32,"dana8ed1":33,"dana8ed2":33,"dana8ed3":33,"dana8ed4":33,"csystem":34,"cclass":35,"spacegroup":36,"spacegroupset":37,"a":38,"b":39,"c":40,"alpha":11,"beta":41,"gamma":41,"aerror":42,"berror":42,"cerror":43,"alphaerror":11,"betaerror":35,"gammaerror":35,"va3":44,"z":45,"csmetamict":13,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":46,"epitaxidescription":11,"morphology":11,"tlform":47,"hmin":48,"hmax":48,"hardtype":11,"vhnmin":11,"vhnmax":11,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":49,"dmeas2":11,"dcalc":50,"dmeaserror":48,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":51,"commentluster":11,"diapheny":52,"streak":53,"colour":54,"commentcolor":11,"colors":55,"streak_colors":58,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":59,"fracturetype":60,"tenacity":61,"commentbreak":11,"opticaltype":62,"opticalsign":63,"opticalalpha":64,"opticalalpha2":11,"opticalalphaerror":48,"opticalbeta":65,"opticalbeta2":11,"opticalbetaerror":48,"opticalgamma":66,"opticalgamma2":11,"opticalgammaerror":42,"opticalomega":11,"opticalomega2":11,"opticalomegaerror":11,"opticalepsilon":11,"opticalepsilon2":11,"opticalepsilonerror":11,"opticaln":11,"opticaln2":11,"opticalnerror":11,"optical2vcalc":67,"optical2vcalc2":11,"optical2vcalcerror":11,"optical2vmeasured":68,"optical2vmeasured2":11,"optical2vmeasurederror":69,"rimin":70,"rimax":71,"opticaldispersion":72,"opticalpleochroism":73,"opticalpleochorismdesc":11,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":74,"opticalr":11,"specdispm":11,"ir":75,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":76,"industrial":11,"occurrence":77,"otheroccurrence":11,"type_specimen_store":78,"description_short":79,"aboutname":80,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":81,"reviewed_at":11,"variety_of":11,"varieties":82,"group_members":83,"associates":84,"confused_with":85,"type_localities":86,"occurrence_total":93,"citations":94,"images":112,"structures":113,"synonyms":114,"language_names":117,"wikidata_qid":135,"texts":136},46440,"1:1:46440:8","17e0b95f-7d19-415e-bc5b-9bd13a93452d","Cryobostryxite","Cbx",0,"mineral",null,29,false,"KZnCl\u003Csub>3\u003C\u002Fsub>&middot;2H\u003Csub>2\u003C\u002Fsub>O","KZnCl\u003Csub>3\u003C\u002Fsub> &middot; 2H\u003Csub>2\u003C\u002Fsub>O",[17,18,19,20,21],"Cl","Zn","O","K","H",[17,18,19,20,21],[17,18],"Tl",[26],"APPROVED",2014,2015,"3","B","A","20","0","Monoclinic",5,14,"P21\u002Fc ","6.2795","10.1397","12.0829","107.732",3,7,732.79,4,"None obeserved.","Anthodites (up to 0.5 × 2 mm), their aggregates (up to 4 × 5 mm), granular crusts (up to 2 × 2 mm) and, rarely, coarse prismatic to acicular crystals (up to 0.2 × 1 mm).",2,"2.30","2.300","Vitreous","Transparent","White","Colorless",[56,57],"colorless","white",[57],"None Observed","Irregular\u002FUneven","brittle","Biaxial","+","1.522","1.530","1.576","46","30",15,1.522,1.576,"None.","Non-pleochroic","Plane of optical axes is (010); Z ∧ c = 26°.","O–H stretching (3200–3600 cm-1) and H–O–H bending (1607 cm-1), vibrations of H2O molecules as a whole (508 cm-1). A band at 3590 cm-1 and a doublet 3533 + 3520 cm-1 conform with weak hydrogen bonds formed by the atoms H3 and H4. Bands at 3372 and 3210 cm-1 conform with strong hydrogen bonds formed by the atoms H1 and H2. Weak bands in the range 600–1200 cm-1 correspond to overtones and combination modes. Absorptions corresponding to B–O, C–O, N–O and N–H bonds are absent.","Readily dissolves in H2O at room temperature.","Secondary mineral formed in the upper, moderately hot (30–80 °C) zone of active fumaroles, probably as a product of the interactions between high-temperature volcanic sublimates and meteoric water. Formed on the surface of basalt scoria.","Type material is deposited in the collections of the Fersman Mineralogical Museum of the Russian Academy of Sciences, Moscow, Russia, registration number 4576\u002F1.","Chemically related to flinteite and mellizinkalite (both anhydrous).\r\n\r\nIn the structure there are isolated Zn-centered ZnCl3(H2O) tetrahedra connected with KCl7(H2O) polyhedra to constitute a framework. Water in the above polyhedra contains O(1) atoms...","The mineral name is based on two Greek words, κρύος, cold or ice, and βóστρυξ, curl, reflecting the typical appearance: visually, \u003Cg>anthodites\u003C\u002Fg> of the mineral are very similar to ice curls.","2026-01-31 12:50:18",[],[],[],[],[87],{"id":88,"txt":89,"latitude":90,"longitude":91,"country":92},259832,"Northern fumarole field, First scoria cone, Northern Breakthrough (North Breach), Great Fissure eruption (Main Fracture), Tolbachik Volcanic field, Milkovsky District, Kamchatka Krai, Russia",55.6833333,160.2333333,"Russia",1,[95,100,104,108],{"id":96,"year":97,"html":98,"doi":99},7745769,1964,"Süsse, Peter; Brehler, Bruno (1964) Die Kristallstruktur des KZnCl3·2H2O. \u003Ci>Beiträge zur Mineralogie und Petrographie\u003C\u002Fi>,  10 (1). 132-140 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fbf01192542'>doi:10.1007\u002Fbf01192542\u003C\u002Fa>","10.1007\u002Fbf01192542",{"id":101,"year":27,"html":102,"doi":103},244562,"Williams, P. A., Hatert, F., Pasero, M., Mills, S. J. (2014) IMA Commission on New Minerals, Nomenclature and Classification (CNMNC), CNMNC Newsletter No. 22. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  78 (5) 1241-1248 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.2014.078.5.10'>doi:10.1180\u002Fminmag.2014.078.5.10\u003C\u002Fa>","10.1180\u002Fminmag.2014.078.5.10",{"id":105,"year":28,"html":106,"doi":107},129441,"Pekov, Igor V., Zubkova, Natalia V., Britvin, Sergey N., Yapaskurt, Vasiliy O., Chukanov, Nikita V., Lykova, Inna S., Sidorov, Evgeny G., Pushcharovsky, Dmitry Yu. (2015) New zinc and potassium chlorides from fumaroles of the Tolbachik volcano, Kamchatka, Russia: mineral data and crystal chemistry. III. Cryobostryxite, KZnCl\u003Csub>3\u003C\u002Fsub>·2H\u003Csub>2\u003C\u002Fsub>O. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  27 (6) 805-812 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1127\u002Fejm\u002F2015\u002F0027-2482'>doi:10.1127\u002Fejm\u002F2015\u002F0027-2482\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FEJM27_805.pdf' class='refpdflink'>\u003C\u002Fa>","10.1127\u002Fejm\u002F2015\u002F0027-2482",{"id":109,"year":110,"html":111,"doi":11},16963839,2016,"(2016) Cryobostryxite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fcryobostryxite.pdf' class='refpdflink'>\u003C\u002Fa>",[],[],[115,116],"Cryobostryxiet","IMA2014-058",[118,122,127,131],{"lang":119,"names":120},"ca",[121],"criobostrixita",{"lang":123,"names":124},"de",[125,126],"Cryobostryxit","IMA 2014-058",{"lang":128,"names":129},"eu",[130],"Kriobostrixita",{"lang":132,"names":133},"it",[134],"cryobostryxite","Q19833357",{"history":11,"applications":11}]