[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:10860":3},{"id":4,"longid":5,"guid":6,"name":7,"shortcode_ima":8,"entrytype":9,"entrytype_text":10,"varietyof":11,"synid":8,"polytypeof":8,"groupid":8,"weighting":12,"nolocadd":13,"blacklisted":13,"mindat_formula":8,"mindat_formula_note":8,"ima_formula":8,"elements":8,"sigelements":8,"key_elements":8,"impurities":8,"cim":8,"ima_status":8,"ima_notes":8,"ima_history":8,"approval_year":8,"publication_year":8,"discovery_year":14,"strunz10ed1":15,"strunz10ed2":15,"strunz10ed3":15,"strunz10ed4":8,"dana8ed1":8,"dana8ed2":8,"dana8ed3":8,"dana8ed4":8,"csystem":8,"cclass":8,"spacegroup":8,"spacegroupset":15,"a":8,"b":8,"c":8,"alpha":8,"beta":8,"gamma":8,"aerror":8,"berror":8,"cerror":8,"alphaerror":8,"betaerror":8,"gammaerror":8,"va3":8,"z":8,"csmetamict":13,"commentcrystal":8,"twinning":8,"tranglide":8,"parting":8,"epitaxidescription":8,"morphology":8,"tlform":8,"hmin":8,"hmax":8,"hardtype":8,"vhnmin":15,"vhnmax":15,"vhnerror":8,"vhng":8,"vhns":8,"commenthard":8,"dmeas":15,"dmeas2":15,"dcalc":15,"dmeaserror":8,"dcalcerror":8,"commentdense":8,"lustre":8,"lustretype":8,"commentluster":8,"diapheny":8,"streak":8,"colour":8,"commentcolor":8,"colors":8,"streak_colors":8,"luminescence":8,"uv":8,"cleavage":8,"cleavagetype":8,"fracturetype":8,"tenacity":8,"commentbreak":8,"opticaltype":8,"opticalsign":8,"opticalalpha":8,"opticalalpha2":8,"opticalalphaerror":8,"opticalbeta":8,"opticalbeta2":8,"opticalbetaerror":8,"opticalgamma":8,"opticalgamma2":8,"opticalgammaerror":8,"opticalomega":8,"opticalomega2":8,"opticalomegaerror":8,"opticalepsilon":8,"opticalepsilon2":8,"opticalepsilonerror":8,"opticaln":8,"opticaln2":8,"opticalnerror":8,"optical2vcalc":8,"optical2vcalc2":8,"optical2vcalcerror":8,"optical2vmeasured":8,"optical2vmeasured2":8,"optical2vmeasurederror":8,"rimin":8,"rimax":8,"opticaldispersion":8,"opticalpleochroism":8,"opticalpleochorismdesc":8,"opticalbirefringence":8,"opticalcomments":8,"opticalcolour":8,"opticalinternal":8,"opticaltropic":8,"opticalanisotropism":8,"opticalbireflectance":8,"opticalextinction":8,"opticalr":8,"specdispm":8,"ir":8,"electrical":8,"magnetism":8,"thermalbehaviour":8,"other":8,"industrial":8,"occurrence":8,"otheroccurrence":8,"type_specimen_store":8,"description_short":8,"aboutname":16,"rock_parent":8,"rock_parent2":8,"rock_root":17,"rock_bgs_code":8,"meteoritical_code":8,"updttime":18,"reviewed_at":8,"variety_of":8,"varieties":19,"group_members":20,"associates":21,"confused_with":22,"type_localities":23,"occurrence_total":28,"citations":29,"images":110,"structures":277,"synonyms":278,"language_names":286,"wikidata_qid":8,"texts":287},10860,"1:1:10860:9","530000c8-80f2-4c81-9f3a-557b5274df4a","Moldavite",null,2,"variety",10859,2438,false,"1788","0","Name first introduced by Zippe (1836) after the main occurrence at the Vltava River (Moldau River) in Southern Bohemia.\r\nFirst described by Joseph Mayer in 1788 after being found within a radius of some 50km from Ceské Budëjovice.",0,"2025-09-19 11:35:21",[],[],[],[],[24],{"id":25,"txt":26,"latitude":8,"longitude":8,"country":27},265433,"Moldavite occurrence, Týn nad Vltavou, České Budějovice District, South Bohemian Region, Czech Republic","Czech Republic",41,[30,33,36,40,44,49,53,57,60,64,68,72,76,80,85,89,93,97,101,106],{"id":31,"year":8,"html":32,"doi":8},16132764,"[https:\u002F\u002Fwww.gia.edu\u002Fgems-gemology\u002Fspring-2015-gemnews-moldavites-natural-fake]",{"id":34,"year":8,"html":35,"doi":8},16384113,"www.vltaviny.cz (n.d.) \u003Ca target='_blank' rel='nofollow' href='https%3A%2F%2Fwww.vltaviny.cz%2Fen%2Ffake-moldavites%2F%3Fcurrency%3DEUR+%28on+fake+moldavites%29'>https:\u002F\u002Fwww.vltaviny.cz\u002Fen\u002Ffake-moldavites\u002F?currency=EUR (on fake moldavites)\u003C\u002Fa>",{"id":37,"year":38,"html":39,"doi":8},16060027,1889,"John, C. v. (1889): Ueber den Moldavit oder Bouteillenstein von Radomilic in Böhmen. Jahrbuch der Geologischen Bundesanstalt 39, 473-476 (in German). [https:\u002F\u002Fopac.geologie.ac.at\u002Fwwwopacx\u002Fwwwopac.ashx?command=getcontent&server=images&value=JB0393_473_A.pdf]",{"id":41,"year":42,"html":43,"doi":8},16132757,1971,"Gentner, W. (1971) Cogenesis of the Ries crater and moldavites and the origin of tektites. Meteoritics: 6: 274-275.",{"id":45,"year":46,"html":47,"doi":48},1080064,1974,"Zook, T. F. (1974) A Moldavite Some Typical Inclusions and Theories. \u003Ci>The Journal of Gemmology\u003C\u002Fi>,  14 (2). 60-68 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.15506\u002Fjog.1974.14.2.60'>doi:10.15506\u002Fjog.1974.14.2.60\u003C\u002Fa>","10.15506\u002Fjog.1974.14.2.60",{"id":50,"year":51,"html":52,"doi":8},16132758,1994,"Vladimir Bouska (1994) Moldavites, The Czech Tektites. Stylizace, Prague, 69 pp. [in English]",{"id":54,"year":55,"html":56,"doi":8},16132759,2002,"Stöffler, D., Artemieva, N.A., Pierazzo, E. (2002): Modeling the Ries‐Steinheim impact event and the formation of the moldavite strewn field. Meteoritics & Planetary Science, 37(12), 1893-1907.",{"id":58,"year":55,"html":59,"doi":8},16132760,"Trnka, Milan; Houzar, Stansilav (2002) \u003Ci>Bulletin of the Czech Geological Survey\u003C\u002Fi>,  77 (4). 283-302",{"id":61,"year":62,"html":63,"doi":8},16132767,2005,"en.wikipedia.org (n.d.) \u003Ca target='_blank' rel='nofollow' href='https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMoldavite'>https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMoldavite\u003C\u002Fa>",{"id":65,"year":66,"html":67,"doi":8},16132761,2009,"Baier, J. (2009) Zur Herkunft und Bedeutung der Ries-Auswurfprodukte für den Impakt-Mechanismus. Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins Band: 91: 9-29 (in German).",{"id":69,"year":70,"html":71,"doi":8},16132762,2012,"ŽÁK, K., SkáLA, R., ŘANDA, Z., MIZERA, J. (2012): A review of volatile compounds in tektites, and carbon content and isotopic composition of moldavite glass. Meteoritics & Planetary Science, 47(6), 1010-1028.",{"id":73,"year":74,"html":75,"doi":8},16046217,2013,"lausitzer-moldavite.de (n.d.) \u003Ca target='_blank' rel='nofollow' href='http:\u002F\u002Flausitzer-moldavite.de\u002F'>http:\u002F\u002Flausitzer-moldavite.de\u002F\u003C\u002Fa>",{"id":77,"year":74,"html":78,"doi":79},129256,"Rantzsch, Ulrike, Franz, Alexandra, Kloess, Gert (2013) Moldavite porosity: a 3-D X-ray micro-tomography study. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  25 (4) 705-710 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1127\u002F0935-1221\u002F2013\u002F0025-2328'>doi:10.1127\u002F0935-1221\u002F2013\u002F0025-2328\u003C\u002Fa>","10.1127\u002F0935-1221\u002F2013\u002F0025-2328",{"id":81,"year":82,"html":83,"doi":84},334135,2014,"Brachaniec, Tomasz, Szopa, Krzysztof, Karwowski, Łukasz (2014) Discovery of the most distal Ries tektites found in Lower Silesia, southwestern Poland. \u003Ci>Meteoritics & Planetary Science\u003C\u002Fi>,  49 (8) 1315-1322 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1111\u002Fmaps.12311'>doi:10.1111\u002Fmaps.12311\u003C\u002Fa>","10.1111\u002Fmaps.12311",{"id":86,"year":87,"html":88,"doi":8},16132763,2015,"Hyršl, J. (2015): Moldavites: Natural Or Fake? Gems & Gemology, 51, 103-104.",{"id":90,"year":87,"html":91,"doi":92},334187,"Brachaniec, Tomasz, Szopa, Krzysztof, Karwowski, Łukasz (2015) A new discovery of parautochthonous moldavites in southwestern Poland, Central Europe. \u003Ci>Meteoritics & Planetary Science\u003C\u002Fi>,  50 (10) 1697-1702 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1111\u002Fmaps.12504'>doi:10.1111\u002Fmaps.12504\u003C\u002Fa>","10.1111\u002Fmaps.12504",{"id":94,"year":95,"html":96,"doi":8},16693429,2016,"Skála, R., Jonášová, Š., Žák, K., Ďurišová, J., Brachaniec, T., Magna, T. (2016) New constraints on the Polish moldavite finds: a separate sub-strewn field of the central European tektite field or re-deposited materials? \u003Ci>Journal of GEOsciences\u003C\u002Fi>,  61 (2). 171-191 \u003Ca target='_blank' href='http:\u002F\u002Fwww.jgeosci.org\u002Fcontent\u002Fjgeosci.214_skala.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":98,"year":95,"html":99,"doi":100},7697056,"Brachaniec, Tomasz, Szopa, Krzysztof, Karwowski, Łukasz (2016) New moldavites from SW Poland. \u003Ci>Acta Geologica Polonica\u003C\u002Fi>, 66 (1). 99-105 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1515\u002Fagp-2016-0005'>doi:10.1515\u002Fagp-2016-0005\u003C\u002Fa>","10.1515\u002Fagp-2016-0005",{"id":102,"year":103,"html":104,"doi":105},334698,2017,"Fritzke, B., Götze, J., Lange, J.-M. (2017) Cathodoluminescence of moldavites. \u003Ci>Meteoritics & Planetary Science\u003C\u002Fi>,  52 (7) 1428-1436 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1111\u002Fmaps.12852'>doi:10.1111\u002Fmaps.12852\u003C\u002Fa>","10.1111\u002Fmaps.12852",{"id":107,"year":108,"html":109,"doi":8},17550604,2020,"Rejl, Ladislav David (2020) \u003Ci>Moldavite\u003C\u002Fi> - The Gemstone that fell to the Earth. Green Snowflake LLC. 300 pp.",[111,121,129,136,141,150,160,169,178,187,196,203,210,218,225,235,243,252,260,269],{"id":112,"source_url":113,"license_code":114,"credit_html":115,"title":116,"description":117,"author":118,"original_width":119,"original_height":120},14241,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=488611","CC BY-SA 3.0","H. Raab (User:Vesta), via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=488611\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Moldavite Besednice.jpg","Moldavite from Besednice, Bohemia, Czech Republic. The specimen weighs 11g and is about 46 mm wide.","H. Raab (User:Vesta)",1024,717,{"id":122,"source_url":123,"license_code":124,"credit_html":125,"title":126,"description":8,"author":8,"original_width":127,"original_height":128},88768,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F50559","CC BY 4.0","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F50559\" rel=\"noopener\">Department of Geology, TalTech\u003C\u002Fa> via Europeana","igneous- and metamorphic rocks",1000,662,{"id":130,"source_url":131,"license_code":114,"credit_html":132,"title":133,"description":134,"author":118,"original_width":119,"original_height":135},68179,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=513299","H. Raab (User:Vesta), via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=513299\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Moldavite Moravia.jpg","Moldavite from Slavice, Moravia, Czech Republic. The specimen weights 17g and is about 40 mm wide. The color of Moravian Moldavites is olive green to brown, they are darker than the bottle-green Moldavites from Bohemia.",768,{"id":137,"source_url":138,"license_code":124,"credit_html":139,"title":126,"description":8,"author":8,"original_width":127,"original_height":140},88769,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F50560","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F50560\" rel=\"noopener\">Department of Geology, TalTech\u003C\u002Fa> via Europeana",667,{"id":142,"source_url":143,"license_code":114,"credit_html":144,"title":145,"description":146,"author":147,"original_width":148,"original_height":149},68181,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=1877839","Chmee2, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=1877839\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Moldavite3.jpg","Moldavite from South Bohemia","Chmee2",2816,2112,{"id":151,"source_url":152,"license_code":153,"credit_html":154,"title":155,"description":156,"author":157,"original_width":158,"original_height":159},68183,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10386963","CC BY-SA 2.0","Claire H., via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10386963\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Moldavite AMNH.jpg","\u003Cp>15 million years old\nFound in Czech Republic.\n\u003C\u002Fp>\nAMNH.","Claire H.",1600,1200,{"id":161,"source_url":162,"license_code":163,"credit_html":164,"title":165,"description":166,"author":167,"original_width":168,"original_height":168},68184,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=39388164","CC BY-SA 4.0","Merinmotapaco, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=39388164\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Moldavita.jpg","Moldavita","Merinmotapaco",403,{"id":170,"source_url":171,"license_code":172,"credit_html":173,"title":174,"description":7,"author":175,"original_width":176,"original_height":177},68185,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=52719238","CC BY 3.0","Johannes Baier, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=52719238\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Moldavit.JPG","Johannes Baier",1515,719,{"id":179,"source_url":180,"license_code":114,"credit_html":181,"title":182,"description":183,"author":184,"original_width":185,"original_height":186},68186,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=61932790","Tiia Monto, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=61932790\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Moldavite 2.jpg","Moldavite in Naturmuseum Augsburg.","Tiia Monto",1122,1092,{"id":188,"source_url":189,"license_code":163,"credit_html":190,"title":191,"description":192,"author":193,"original_width":194,"original_height":195},68187,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=63534844","Onohej zlatove, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=63534844\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Moldavite No.2.jpg","Photo taken by Moldavite Association team 2017\nwww.starstones.com, www.moldavitassociation.com","Onohej zlatove",512,753,{"id":197,"source_url":198,"license_code":163,"credit_html":199,"title":200,"description":201,"author":193,"original_width":194,"original_height":202},68188,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=63580358","Onohej zlatove, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=63580358\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Moldavite No.4.jpg","Moldavite Besednice\nPhoto: Onohej Zlatove, Moldavite Association",671,{"id":204,"source_url":205,"license_code":163,"credit_html":206,"title":207,"description":208,"author":193,"original_width":194,"original_height":209},68190,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=63581009","Onohej zlatove, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=63581009\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Moldavite No.9.jpg","Moldavite Czech Republic - Chlum\nPhoto: Onohej Zlatove - Moldavite Association",666,{"id":211,"source_url":212,"license_code":163,"credit_html":213,"title":214,"description":215,"author":193,"original_width":216,"original_height":217},68191,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=63581015","Onohej zlatove, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=63581015\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Moldavite No.11.jpg","Moldavite Czech Republic - Besednice\nPhoto: Onohej Zlatove - Moldavite Association",1827,2508,{"id":219,"source_url":220,"license_code":163,"credit_html":221,"title":222,"description":215,"author":193,"original_width":223,"original_height":224},68192,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=63581016","Onohej zlatove, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=63581016\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Moldavite No.13.jpg",494,665,{"id":226,"source_url":227,"license_code":228,"credit_html":229,"title":230,"description":231,"author":232,"original_width":233,"original_height":234},68194,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=83657438","CC BY 2.0","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=83657438\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Moldavite (Miocene, 14.5-14.8 Ma; Besednice, Bohemia) (14609742880).jpg","\u003Cp>Moldavite from the Miocene of Bohemia. (2.5 centimeters tall)\n\u003C\u002Fp>\u003Cp>Large & small impacts have affected Earth since its formation 4.55 billion years ago.  Compared with the intensely pitted and cratered Moon, Earth has relatively few preserved impact craters, because they have been destroyed by water & glacial erosion.  Impact events are accompanied by tremendous amounts of heat, resulting in melting of much of the ejected pulverized bedrock at ground zero.  The melted material cools quickly, and falls back to Earth in the form of impact splash glasses (a.k.a. tektites).  Tektites are principally composed of amorphous silica (SiO2).  Broken surfaces show a conchoidal fracture.  Tektites from different impact events are given different names.\n\u003C\u002Fp>\u003Cp>Moldavite is probably the most distinctive impact splash glass in the world, due to its pleasant green color.  Like other impact splash glasses, moldavite is amorphous SiO2 with minor Al, Ca, Fe, K, and Na.  Moldavite formed ~14.5-14.8 million years ago, during the mid-Miocene, in association with the Ries Impact Crater, located in Bavaria, Germany.\n\u003C\u002Fp>\u003Cp>The specimen shown above is derived from >4 meters below the land surface, below the water table, which accounts for the pitting and the surficial dissolution network.\n\u003C\u002Fp>\nLocality: pit near the town of Besednice, in the Moldau (Vltava) River Valley area, southern Jihocesky Region (far-southern Bohemia), far-southern Czech Republic","James St. John",602,772,{"id":236,"source_url":237,"license_code":228,"credit_html":238,"title":239,"description":240,"author":232,"original_width":241,"original_height":242},68195,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=96360068","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=96360068\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Moldavite (Miocene, 14.5-14.8 Ma; Ries Impact Crater's tektite strewn field, Bohemia) 2.jpg","Moldavites from the Miocene of Bohemia. (the elongated specimen at right is ~2.4 centimeters tall)\n\u003Cp>Large & small impacts have affected Earth since its formation 4.55 billion years ago.  Compared with the intensely pitted and cratered Moon, Earth has relatively few preserved impact craters, because they have been destroyed by water & glacial erosion.  Impact events are accompanied by tremendous amounts of heat, resulting in melting of much of the ejected pulverized bedrock at ground zero.  The melted material cools quickly, and falls back to Earth in the form of impact splash glasses (= tektites).  Tektites are principally composed of amorphous silica (SiO2).  Broken surfaces show a conchoidal fracture.  Tektites from different impact events are given different names.\n\u003C\u002Fp>\u003Cp>Moldavite is probably the most distinctive impact splash glass in the world, due to its pleasant green color.  Like other impact splash glasses, moldavite is amorphous SiO2 with minor Al, Ca, Fe, K, and Na.  Moldavite formed ~14.5-14.8 million years ago, during the mid-Miocene, in association with the Ries Impact Crater, located in Bavaria, Germany.\n\u003C\u002Fp>\u003Cp>The specimens seen here have surficial pitting and fine-scale dissolution networks.  This results from being below the water table for long periods of time.\n\u003C\u002Fp>\nLocality: unrecorded\u002Fundisclosed site in the Ries Impact Crater's tektite strewn field, Moldau (Vltava) River Valley area, southern Jihocesky Region (far-southern Bohemia), far-southern Czech Republic",2066,1656,{"id":244,"source_url":245,"license_code":163,"credit_html":246,"title":247,"description":248,"author":249,"original_width":250,"original_height":251},68196,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=138620125","Geolina163, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=138620125\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Joanneum Naturkundemuseum Moldavit in Matrix Tschechien.jpg","Universalmuseum Joanneum Naturkundemuseum: Moldavit in Matrix, Chlum nad Malsi \u002F Tschechische Republik","Geolina163",2304,3162,{"id":253,"source_url":254,"license_code":163,"credit_html":255,"title":256,"description":257,"author":249,"original_width":258,"original_height":259},68197,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=138620131","Geolina163, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=138620131\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Joanneum Naturkundemuseum Moldavit in Matrix Tschechien 1.jpg","Universalmuseum Joanneum Naturkundemuseum:  Moldavit in Matrix, Chlum nad Malsi \u002F Tschechische Republik",4864,3648,{"id":261,"source_url":262,"license_code":124,"credit_html":263,"title":264,"description":265,"author":266,"original_width":267,"original_height":268},68200,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=181778419","AdamStejskal, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=181778419\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Faceted natural Moldavite - Moldavite gemstones.jpg","beautifull Faceted natural Moldavite - Moldavite gemstones","AdamStejskal",6960,4640,{"id":270,"source_url":271,"license_code":124,"credit_html":272,"title":273,"description":274,"author":266,"original_width":275,"original_height":276},68202,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=181778430","AdamStejskal, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=181778430\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Moldavite gemstone - vltavín.jpg","natural faceted Moldavite gemstone - vltavín",3641,2325,[],[279,280,281,282,166,283,284,285],"Bouteillenstein","False Chrysolite","Glass meteorite","Moldavit","Moldawit","Pseudochrysolite","Water Chrysolite",[],{"history":8,"applications":8}]