[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:4163":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":23,"key_elements":24,"impurities":11,"cim":25,"ima_status":26,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":29,"discovery_year":30,"strunz10ed1":31,"strunz10ed2":32,"strunz10ed3":33,"strunz10ed4":34,"dana8ed1":35,"dana8ed2":36,"dana8ed3":37,"dana8ed4":38,"csystem":39,"cclass":40,"spacegroup":11,"spacegroupset":41,"a":42,"b":43,"c":44,"alpha":41,"beta":45,"gamma":41,"aerror":40,"berror":46,"cerror":47,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":48,"csmetamict":13,"commentcrystal":49,"twinning":50,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":51,"tlform":11,"hmin":52,"hmax":47,"hardtype":11,"vhnmin":41,"vhnmax":41,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":53,"dmeas2":53,"dcalc":53,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":54,"lustretype":55,"commentluster":11,"diapheny":56,"streak":57,"colour":58,"commentcolor":11,"colors":59,"streak_colors":63,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":11,"fracturetype":64,"tenacity":65,"commentbreak":11,"opticaltype":66,"opticalsign":67,"opticalalpha":68,"opticalalpha2":41,"opticalalphaerror":69,"opticalbeta":70,"opticalbeta2":41,"opticalbetaerror":69,"opticalgamma":70,"opticalgamma2":41,"opticalgammaerror":69,"opticalomega":41,"opticalomega2":41,"opticalomegaerror":11,"opticalepsilon":41,"opticalepsilon2":41,"opticalepsilonerror":11,"opticaln":41,"opticaln2":41,"opticalnerror":11,"optical2vcalc":41,"optical2vcalc2":41,"optical2vcalcerror":11,"optical2vmeasured":41,"optical2vmeasured2":41,"optical2vmeasurederror":11,"rimin":71,"rimax":72,"opticaldispersion":73,"opticalpleochroism":74,"opticalpleochorismdesc":75,"opticalbirefringence":11,"opticalcomments":76,"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":77,"industrial":11,"occurrence":11,"otheroccurrence":78,"type_specimen_store":79,"description_short":80,"aboutname":81,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":82,"reviewed_at":11,"variety_of":11,"varieties":83,"group_members":84,"associates":85,"confused_with":95,"type_localities":112,"occurrence_total":117,"citations":118,"images":246,"structures":397,"synonyms":404,"language_names":415,"wikidata_qid":460,"texts":461},4163,"1:1:4163:4","8d218390-2875-4f31-b76c-5004b7234e38","Vauquelinite","Vql",0,"mineral",null,2199,false,"Pb\u003Csub>2\u003C\u002Fsub>Cu(CrO\u003Csub>4\u003C\u002Fsub>)(PO\u003Csub>4\u003C\u002Fsub>)(OH)","CuPb\u003Csub>2\u003C\u002Fsub>(CrO\u003Csub>4\u003C\u002Fsub>)(PO\u003Csub>4\u003C\u002Fsub>)(OH)",[17,18,19,20,21,22],"Cr","Cu","Pb","O","P","H",[17,18,19,20,21,22],[17,18,19],"22.5.1",[27,28],"APPROVED","GRANDFATHERED",1818,"1818","7","F","C","05","43","4","3","1","Monoclinic",5,"0","13.754","5.806","9.563","94.55",6,3,4,"Space Group: P21\u002Fn.","On {102}.","Crystals commonly minute and frequently wedge-shaped; irregularly aggregated; and mammillary fibrous forms; reniform; botryoidal; granular, compact.",2.5,"6.16","Adamantine-Resinous","Adamantine,Resinous","Transparent,Translucent","Greenish or brownish","Olive-green, apple-green, brown to nearly black",[60,61,62],"green","brown","black",[60,61],"Irregular\u002FUneven","brittle","Biaxial","-","2.11",2,"2.22",2.11,2.22,"strong","Visible","X = Light green\r\nY = Light brown\r\nZ = Light brown","2V = near zero.","Partially soluble in HNO3.\r\n\r\nReported as an alteration product of pyromorphite and as incrustation pseudomorphs after dolomite.","Oxidation zone of some hydrothermal deposits.","No designated type material.","Fornacite-Vauquelinite Series. The phosphate analogue of fornacite.\r\n\r\nRelated to the Brackebuschite Supergroup.","Named after Louis Nicolas Vauquelin (16 May 1763, Saint-André-d'Hébertot, Normandy, France - 14 November 1829,  Saint-André-d'Hébertot, Normandy, France), Professor of Chemistry, University of Paris (France) and discoverer of chromium.  He also discovered beryllium, the first amino acid (asparagine), pectin and malic acid.","2025-08-11 12:14:24",[],[],[86],{"id":87,"name":88,"entrytype":9,"csystem":39,"ima_formula":89,"mindat_formula":90,"hmin":52,"hmax":91,"dmeas":92,"dcalc":93,"primary_image_id":94},3194,"Phoenicochroite","Pb\u003Csub>2\u003C\u002Fsub>O(CrO\u003Csub>4\u003C\u002Fsub>)","Pb\u003Csub>2\u003C\u002Fsub>(CrO\u003Csub>4\u003C\u002Fsub>)O",3.5,"7.01","7.075",19318,[96,104],{"id":97,"name":98,"entrytype":9,"csystem":39,"ima_formula":99,"mindat_formula":100,"hmin":69,"hmax":47,"dmeas":101,"dcalc":102,"primary_image_id":103},1583,"Fornacite","CuPb\u003Csub>2\u003C\u002Fsub>(CrO\u003Csub>4\u003C\u002Fsub>)(AsO\u003Csub>4\u003C\u002Fsub>)(OH)","Pb\u003Csub>2\u003C\u002Fsub>Cu(CrO\u003Csub>4\u003C\u002Fsub>)(AsO\u003Csub>4\u003C\u002Fsub>)(OH)","6.27","6.30",9296,{"id":105,"name":106,"entrytype":9,"csystem":39,"ima_formula":107,"mindat_formula":108,"hmin":47,"hmax":48,"dmeas":109,"dcalc":110,"primary_image_id":111},2734,"Molybdofornacite","CuPb\u003Csub>2\u003C\u002Fsub>(MoO\u003Csub>4\u003C\u002Fsub>)(AsO\u003Csub>4\u003C\u002Fsub>)(OH)","Pb\u003Csub>2\u003C\u002Fsub>Cu(MoO\u003Csub>4\u003C\u002Fsub>,CrO\u003Csub>4\u003C\u002Fsub>)(AsO\u003Csub>4\u003C\u002Fsub>,PO\u003Csub>4\u003C\u002Fsub>)(OH)","6.57","6.6",16515,[113],{"id":114,"txt":115,"latitude":11,"longitude":11,"country":116},19472,"Tsvetnoi Mine, Uspenskaya Hill, Berezovsk deposit, Beryozovsky, Sverdlovsk Oblast, Russia","Russia",65,[119,122,126,130,134,138,142,146,150,154,158,163,167,171,175,179,183,186,191,195,199,203,206,211,216,220,225,230,234,237,242],{"id":120,"year":29,"html":121,"doi":11},16127139,"Berzelius, J. (1818) Afhandlingar I Fysik, Kemi och Mineralogi, Stockholm: 6: 246 (as Vauqueline).",{"id":123,"year":124,"html":125,"doi":11},17556069,1819,"Berzelius, J. J. (1819) \u003Ci>Nouveau Système de minéralogie\u003C\u002Fi>. Méquignon-Marvis.",{"id":127,"year":128,"html":129,"doi":11},12960856,1822,"Haüy, René Just (1822) \u003Ci>Traité de Minéralogie\u003C\u002Fi> (2nd ed.) Vol. 3. Bachelier, Paris. \u003Ca target='_blank' href='https:\u002F\u002Farchive.org\u002Fdownload\u002Ftraitdeminralog05goog\u002Ftraitdeminralog05goog.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":131,"year":132,"html":133,"doi":11},16127142,1827,"Haidinger, W. (1827) Account of a French locality of vauquelinite. Edinburgh Journal of Science: 7: 213-214.",{"id":135,"year":136,"html":137,"doi":11},16127143,1837,"Phillips, Wm., augmented by Allan, R. (1837) Mineralogy, Fourth edition London: 369 (as Chromate of Lead and Copper).",{"id":139,"year":140,"html":141,"doi":11},16127144,1845,"John, J. (1845) Untersuchungen über einige merkwurdige Mineralien. Neues Jahrbuch für Mineralogie, Geologie und Paleontologie, Heidelberg, Stuttgart: 66-72 (67-69). (as Chrom-phosphokupferbleispath).",{"id":143,"year":144,"html":145,"doi":11},16127145,1863,"Blum, J.R. (1863) Die Pseudomorphosen des Mineralreichs. Stuttgart, nachträge 3, Erlangen: 197.",{"id":147,"year":148,"html":149,"doi":11},16127146,1867,"Nordenskiöld (1867) Ak. Stockholm, Őfv.: 24: 655 (as Laxmannite).",{"id":151,"year":152,"html":153,"doi":11},16127147,1869,"Nordenskiöld (1869) Annalen der Physik, Halle, Leipzig: 137: 299 (as Laxmannite).",{"id":155,"year":156,"html":157,"doi":11},16127148,1870,"Hermann (1870) Journal für praktische Chemie, Leipzig: 1: 196, 447 (as Phosphorchromit).",{"id":159,"year":160,"html":161,"doi":162},5082,1877,"Davies, Thos. (1877) VI.—Notes on Vauquelinite from Scotland, and Cantonite from Cornwall. \u003Ci>Mineralogical Magazine and Journal of the Mineralogical Society\u003C\u002Fi>,  1 (4) 112-114 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1877.001.4.07'>doi:10.1180\u002Fminmag.1877.001.4.07\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_1\u002F1-4-112.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1877.001.4.07",{"id":164,"year":165,"html":166,"doi":11},17606816,1878,"Koksharov, Nikolai (1878) \u003Ci>Materialien zur Mineralogie Russlands\u003C\u002Fi> Vol. 8. Carl Kray.",{"id":168,"year":169,"html":170,"doi":11},16127151,1880,"Pisani, F. (1880) Chrome-phosphate de plomb et de cuivre. Bulletin de la Société française de Minéralogie: 3: 196-196.",{"id":172,"year":173,"html":174,"doi":11},16127152,1882,"Des Cloizeaux, A. (1882) Bulletin de la Société française de Minéralogie: 5: 53.",{"id":176,"year":177,"html":178,"doi":11},1118647,1892,"Dana, Edward Salisbury; Dana, James Dwight (1892) \u003Ci>A System of Mineralogy\u003C\u002Fi> (6th ed.). John Wiley & Sons, Inc.",{"id":180,"year":181,"html":182,"doi":11},7367189,1910,"Lacroix, A. (1910) \u003Ci>Minéralogie de la France et de ses colonies\u003C\u002Fi> Vol. 4. Library Polytechnique, Paris. \u003Ca target='_blank' href='https:\u002F\u002Fwww.biodiversitylibrary.org\u002Fitempdf\u002F225322' class='refpdflink'>\u003C\u002Fa>",{"id":184,"year":181,"html":185,"doi":11},16127155,"Petterd, W.F. (1910) Catalogue of the Minerals of Tasmania. 221pp., Hobart: 196.",{"id":187,"year":188,"html":189,"doi":190},647767,1921,"Larsen, Esper S. (1921) The microscopic determination of the nonopaque minerals. \u003Ci>Bulletin\u003C\u002Fi> 679. US Geological Survey \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3133\u002Fb679'>doi:10.3133\u002Fb679\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fpubs.usgs.gov\u002Fbul\u002F0679\u002Freport.pdf' class='refpdflink'>\u003C\u002Fa>","10.3133\u002Fb679",{"id":192,"year":193,"html":194,"doi":11},4468631,1923,"(1923) \u003Ci>Atlas Der Krystallformen\u003C\u002Fi> Vol. 9 - Text - Band IX - Trechmannit-Zoisit und Nachträge. Carl Winters Universitätsbuchhandlung, Heidelberg.",{"id":196,"year":197,"html":198,"doi":11},16127157,1935,"Chirva (1935) Annals Leningrad State University, Series Geology: 1: 19 [Min. Abs.: 7: 460].",{"id":200,"year":201,"html":202,"doi":11},1118652,1951,"Palache, Charles; Berman, Harry; Frondel, Clifford (1951) \u003Ci>The System of Mineralogy\u003C\u002Fi> (7th ed.) Vol. 2 - Halides, Nitrates, Borates, Carbonates, Sulfates, Phosphates, Arsenates, Tungstates, Molybdates, Etc. John Wiley and Sons.",{"id":204,"year":201,"html":205,"doi":11},16127159,"Guillemin, C., Prouvost, J. (1951) Étude de la série: fornacite˗vauquelinite. Bulletin de Minéralogie, 74(7), 432-438.",{"id":207,"year":208,"html":209,"doi":210},6114,1967,"Fanfani, L., Zanazzi, P. F. (1967) Structural similarities of some secondary lead minerals. \u003Ci>Mineralogical Magazine and Journal of the Mineralogical Society\u003C\u002Fi>,  36 (280) 522-529 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1967.036.280.06'>doi:10.1180\u002Fminmag.1967.036.280.06\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_36\u002F36-280-522.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1967.036.280.06",{"id":212,"year":213,"html":214,"doi":215},107632,1968,"Fanfani, L., Zanazzi, P. F. (1968) The crystal structure of vauquelinite and the relationships to fornacite. \u003Ci>Zeitschrift für Kristallographie - Crystalline Materials\u003C\u002Fi>,  126 (5) 433-443 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1968.126.5-6.433'>doi:10.1524\u002Fzkri.1968.126.5-6.433\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fzk\u002Fvol126\u002FZK126_433.pdf' class='refpdflink'>\u003C\u002Fa>","10.1524\u002Fzkri.1968.126.5-6.433",{"id":217,"year":218,"html":219,"doi":11},16127161,1978,"Deliens, M. (1978) La chenevixite, la vauquelinite, la sterrettite et la boltwoodite, mineraux nouveaux pour les gisements du Shaba (Zaire) et du Rwanda. Annales de la Société géologique de Belgique, 101, 111–119.",{"id":221,"year":222,"html":223,"doi":224},402808,1980,"Cesbron, Fabien, Williams, Sydney A. (1980) Iranite˗hémihédrite, bellite, phoenicochroite, vauquelinite et fornacite : synthèse et nouvelles données. \u003Ci>Bulletin de Minéralogie\u003C\u002Fi>,  103 (5) 469-477 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3406\u002Fbulmi.1980.7409'>doi:10.3406\u002Fbulmi.1980.7409\u003C\u002Fa>","10.3406\u002Fbulmi.1980.7409",{"id":226,"year":227,"html":228,"doi":229},2423543,2004,"Frost, Ray L. (2004) Raman microscopy of selected chromate minerals. \u003Ci>Journal of Raman Spectroscopy\u003C\u002Fi>, 35 (2). 153-158 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1002\u002Fjrs.1121'>doi:10.1002\u002Fjrs.1121\u003C\u002Fa>","10.1002\u002Fjrs.1121",{"id":231,"year":232,"html":233,"doi":11},16127162,2005,"Yamada, T., Oohama, T. (2005) Vauquelinite from the Akenobe Mine, Yabu City, Hyogo Prefecture, Japan. Abstracts for Annual Meeting of the Mineralogical Society of Japan, 2005 Annual Meeting of the Mineralogical Society of Japan, 125-125.",{"id":235,"year":232,"html":236,"doi":11},16967957,"(2005) Vauquelinite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fvauquelinite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":238,"year":239,"html":240,"doi":241},16987738,2006,"Reddy, K. Nagamuni, Reddy, G. Siva, Reddy, S. Lakshmi, Rao, P. S. (2006) Optical absorption and EPR spectral studies of vauquelinite. \u003Ci>Crystal Research and Technology\u003C\u002Fi>,  41 (8) 818-821 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1002\u002Fcrat.200510676'>doi:10.1002\u002Fcrat.200510676\u003C\u002Fa>","10.1002\u002Fcrat.200510676",{"id":243,"year":244,"html":245,"doi":11},16127164,2014,"Pauliš, Petr; Kopecký, Stanislav; Kopecký, Stanislav; Sejkora, Jiří; Malíkovám Radana (2014) Vauquelinit z ložiska polymetalických rud Suchovršice u Trutnova (Česká republika) [Vauquelinite from the base-metal deposit Suchovršice near Trutnov (Czech Republic)]. Bull. mineral.-petrolog. Odd. Nár. Muz. (Praha), 22(1), 82-86.",[247,257,266,276,285,292,300,308,315,322,329,336,342,352,361,369,375,381,387],{"id":248,"source_url":249,"license_code":250,"credit_html":251,"title":252,"description":253,"author":254,"original_width":255,"original_height":256},27332,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14866890","CC BY-SA 3.0","Leon Hupperichs, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14866890\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Vauquelinite-120513.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FVauquelinite\" class=\"extiw\" title=\"en:Vauquelinite\">Vauquelinite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Point 14.0, Hohenstein, Reichenbach, Bensheim, Odenwald, Hesse, Germany\u003C\u002Fdd>\n\u003Cdd>Field of view 5 mm. Ex Klaus Petitjean collection. Specimen and photo Leon Hupperichs.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Leon Hupperichs",774,581,{"id":258,"source_url":259,"license_code":250,"credit_html":260,"title":261,"description":262,"author":263,"original_width":264,"original_height":265},27333,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=32615429","Christian Rewitzer, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=32615429\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Vauquelinite-544001.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FVauquelinite\" class=\"extiw\" title=\"en:Vauquelinite\">Vauquelinite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Berezovskoe Au Deposit (Berezovsk Mines), Berezovskii (Berezovskii Zavod), Ekaterinburg (Sverdlovsk), Sverdlovskaya Oblast', Middle Urals, Urals Region, Russia\u003C\u002Fdd>\n\u003Cdd>Picture width 2 mm. PXRD confirmed. Collection and photograph Christian Rewitzer\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Christian Rewitzer",1000,961,{"id":267,"source_url":268,"license_code":269,"credit_html":270,"title":271,"description":272,"author":273,"original_width":274,"original_height":275},84943,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=51315682","CC BY-SA 4.0","Weirdmeister, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=51315682\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Vauquelinite Naturkundemuseum Berlin.jpg","Vauquelinit der Mineraliensammlung im Naturkundemuseum Berlin","Weirdmeister",2617,2093,{"id":277,"source_url":278,"license_code":250,"credit_html":279,"title":280,"description":281,"author":282,"original_width":283,"original_height":284},27330,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10136817","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10136817\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Crocoite-Vauquelinite-65716.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCrocoite\" class=\"extiw\" title=\"en:Crocoite\">Crocoite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FVauquelinite\" class=\"extiw\" title=\"en:Vauquelinite\">Vauquelinite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Berezovskoe Au Deposit (Berezovsk Mines), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBerezovsky\" class=\"extiw\" title=\"en:Berezovsky\">Berezovskii (Berezovskii Zavod)\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FYekaterinburg\" class=\"extiw\" title=\"en:Yekaterinburg\">Ekaterinburg (Sverdlovsk)\u003C\u002Fa>, Ekaterinburgskaya (Sverdlovskaya) Oblast', Middle Urals, Urals Region, Russia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2728.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>This matrix is heavily invested with massive crocoite, but a protected vug in the center has several prismatic, lustrous and gemmy, reddish- orange, crystals to 1.5 cm in length. Surrounding the vug and then running in veins throughout are rich veins and surface carpets of olive green vauqelinite, a rare lead-copper species. Over two hundred years ago, crocoite was first described from this locality. At that time, Vauquelinite was found in some quantity but it has not, to my knowledge, been found in any recent reworkings of the locality. 8.8 x 5.8 x 3.8 cm\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Robert M. Lavinsky",800,623,{"id":286,"source_url":287,"license_code":288,"credit_html":289,"title":290,"description":11,"author":11,"original_width":264,"original_height":291},30919,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F108759","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\u002F108759\" rel=\"noopener\">Department of Geology, TalTech\u003C\u002Fa> via Europeana","Crocoite",666,{"id":293,"source_url":294,"license_code":250,"credit_html":295,"title":296,"description":297,"author":282,"original_width":298,"original_height":299},53250,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10122669","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10122669\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Crocoite-Vauquelinite-Embreyite-27531.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCrocoite\" class=\"extiw\" title=\"en:Crocoite\">Crocoite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FVauquelinite\" class=\"extiw\" title=\"en:Vauquelinite\">Vauquelinite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FEmbreyite\" class=\"extiw\" title=\"en:Embreyite\">Embreyite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Berezovskoe Au Deposit (Berezovsk Mines), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBerezovsky\" class=\"extiw\" title=\"en:Berezovsky\">Berezovskii (Berezovskii Zavod)\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FYekaterinburg\" class=\"extiw\" title=\"en:Yekaterinburg\">Ekaterinburg (Sverdlovsk)\u003C\u002Fa>, Ekaterinburgskaya (Sverdlovskaya) Oblast', Middle Urals, Urals Region, Russia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2728.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>A very important specimen with several identified patches of microcrystallized but eye-visible EMBREYITE present. This is an extremely rare mineral and I am told it was identified on old specimens from this locality in museum collections, and is very rarely seen for sale. This specimen is extremely rich. Aside from the two small vugs there are isolated spots of embreyite elsewhere as well. MOREOEVER, the Vauquelinite on this specimen, in the form of spherical green balls atop the crocoite vug, is also quite exceptional and is the richest example of this mineral I have yet seen from the location (it is usually just greenish splotches on broken crocoite!). So, we have TWO significant rarities on what is, overall, a fairly attractive specimen of crocoite from the TYPE LOCALITY for ALL THREE SPECIES 6.5 x 3.4 x 2.9 cm\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",700,530,{"id":301,"source_url":302,"license_code":250,"credit_html":303,"title":304,"description":305,"author":282,"original_width":306,"original_height":307},4824,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10455044","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10455044\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Embreyite-Vauquelinite-oldeuro-54c.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FEmbreyite\" class=\"extiw\" title=\"en:Embreyite\">Embreyite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FVauquelinite\" class=\"extiw\" title=\"en:Vauquelinite\">Vauquelinite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Berezovskoe Au Deposit (Berezovsk Mines), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBerezovsky\" class=\"extiw\" title=\"en:Berezovsky\">Berezovskii (Berezovskii Zavod)\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FYekaterinburg\" class=\"extiw\" title=\"en:Yekaterinburg\">Ekaterinburg (Sverdlovsk)\u003C\u002Fa>, Ekaterinburgskaya (Sverdlovskaya) Oblast', Middle Urals, Urals Region, Russia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2728.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: small cabinet, 7.7 x 4.9 x 4.0 cm\n\u003Cdl>\u003Cdt>Vauquelinite with Embreyite\u003C\u002Fdt>\u003C\u002Fdl>\u003C\u002Fdd>\n\u003Cdd>A very rich specimen from this famous lead deposit, with rich postachio-green Vauquelinite microxls all over the piece, and minute druses of embreyite microxls as well (they are orange, and seem intermixed quite liberally on the righthand side) . The even rarer cassedanneite is red and although I have not analysed the red micros here, it is possible they are that species. Type Locality for both species!\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",328,400,{"id":309,"source_url":310,"license_code":250,"credit_html":311,"title":312,"description":313,"author":282,"original_width":314,"original_height":283},7786,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10154898","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10154898\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Vauquelinite-Embreyite-189272.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FVauquelinite\" class=\"extiw\" title=\"en:Vauquelinite\">Vauquelinite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FEmbreyite\" class=\"extiw\" title=\"en:Embreyite\">Embreyite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Berezovskoe Au Deposit (Berezovsk Mines), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBerezovsky\" class=\"extiw\" title=\"en:Berezovsky\">Berezovskii (Berezovskii Zavod)\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FYekaterinburg\" class=\"extiw\" title=\"en:Yekaterinburg\">Ekaterinburg (Sverdlovsk)\u003C\u002Fa>, Ekaterinburgskaya (Sverdlovskaya) Oblast', Middle Urals, Urals Region, Russia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2728.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 7.7 x 4.9 x 4.0 cm.\u003C\u002Fdd>\n\u003Cdd>A very rich specimen, with rich pistachio-green Vauquelinite microcrystals all over the piece, and minute druses of embreyite microcrystals as well (they are orange, and seem intermixed quite liberally on the righthand side). This is the type locality for both species.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",591,{"id":316,"source_url":317,"license_code":250,"credit_html":318,"title":319,"description":320,"author":282,"original_width":321,"original_height":298},27331,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10160169","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10160169\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Crocoite-Vauquelinite-207506.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCrocoite\" class=\"extiw\" title=\"en:Crocoite\">Crocoite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FVauquelinite\" class=\"extiw\" title=\"en:Vauquelinite\">Vauquelinite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Berezovskoe Au Deposit (Berezovsk Mines), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBerezovsky\" class=\"extiw\" title=\"en:Berezovsky\">Berezovskii (Berezovskii Zavod)\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FYekaterinburg\" class=\"extiw\" title=\"en:Yekaterinburg\">Ekaterinburg (Sverdlovsk)\u003C\u002Fa>, Ekaterinburgskaya (Sverdlovskaya) Oblast', Middle Urals, Urals Region, Russia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2728.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 5.2 x 5.1 x 3.8 cm.\u003C\u002Fdd>\n\u003Cdd>An old-time, very rich and fine chromium species combination specimen from the Type Locality - Berezovsk, Urals Region, Russia. This classic may contain 3 chromium species, 2 of which are very rare. Gemmy and lustrous red to orange crocoite crystals cover part of the specimen. This specimen has a very rich section of pistachio-green vauquelinite, a rare lead, copper, phosphate, chromate. The specimen may also contain embreyite, a very rare lead, phosphate, chromate: although not analyzed, we believe that it may be the black microcrystals on the matrix. The specimen would have to be X-rayed for confirmation of course, it’s just a likelihood given the age and overall appearance of the material.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",660,{"id":323,"source_url":324,"license_code":250,"credit_html":325,"title":326,"description":327,"author":282,"original_width":298,"original_height":328},53251,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10148025","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10148025\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Crocoite-Vauquelinite-162821.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCrocoite\" class=\"extiw\" title=\"en:Crocoite\">Crocoite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FVauquelinite\" class=\"extiw\" title=\"en:Vauquelinite\">Vauquelinite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Berezovskoe Au Deposit (Berezovsk Mines), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBerezovsky\" class=\"extiw\" title=\"en:Berezovsky\">Berezovskii (Berezovskii Zavod)\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FYekaterinburg\" class=\"extiw\" title=\"en:Yekaterinburg\">Ekaterinburg (Sverdlovsk)\u003C\u002Fa>, Ekaterinburgskaya (Sverdlovskaya) Oblast', Middle Urals, Urals Region, Russia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2728.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 9.0 x 7.0 x 4.8 cm.\u003C\u002Fdd>\n\u003Cdd>An OLD-TIME, VERY RICH and showy chrome species combination specimen from the Type Locality - Berezovsk, Urals Region, Russia. This classic may contain 3 chrome species, 2 of which, are VERY RARE. One half of the specimen is covered with red to orange crocoite crystals. This specimen has a VERY RICH section of pistachio-green vauquelinite, a RARE lead, copper, phosphate, chromate. The specimen may also contain embreyite, an ULTRA RARE lead, phosphate, chromate: although not analyzed, we believe that it may be either the tan or black microcrystals on the matrix. The specimen would have to be X-rayed for confirmation of course, its just a likelihood given the age and overall appearance of the material. CHOICE, old material for the species and locality. This rich and showy old-timer comes from an old European collection, where everything dates to the 1800s. This whole collection had myriad old materials, though I cannot name the owner, and was well known in Europe. Accompanied by an old, handwritten German label.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",537,{"id":330,"source_url":331,"license_code":250,"credit_html":332,"title":333,"description":334,"author":282,"original_width":335,"original_height":283},7784,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10151842","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10151842\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Embreyite-Vauquelinite-Crocoite-177809.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FEmbreyite\" class=\"extiw\" title=\"en:Embreyite\">Embreyite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FVauquelinite\" class=\"extiw\" title=\"en:Vauquelinite\">Vauquelinite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCrocoite\" class=\"extiw\" title=\"en:Crocoite\">Crocoite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Berezovskoe Au Deposit (Berezovsk Mines), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBerezovsky\" class=\"extiw\" title=\"en:Berezovsky\">Berezovskii (Berezovskii Zavod)\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FYekaterinburg\" class=\"extiw\" title=\"en:Yekaterinburg\">Ekaterinburg (Sverdlovsk)\u003C\u002Fa>, Ekaterinburgskaya (Sverdlovskaya) Oblast', Middle Urals, Urals Region, Russia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2728.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 6.0 x 5.4 x 4.6 cm.\u003C\u002Fdd>\n\u003Cdd>This specimen is from the type locality for all three species here, and features rich zones of all three as well. It has prismatic orange crocoite crystals to 2 cm in length. Olive green vauquelinite occurs as chalky, green growths on crocoite. Nestled in a vug are minute orange embreyite crystals. Ex. Harvard University and Phil Scalisi Collections.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",672,{"id":337,"source_url":338,"license_code":250,"credit_html":339,"title":340,"description":334,"author":282,"original_width":341,"original_height":307},7785,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10151847","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10151847\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Embreyite-Vauquelinite-Crocoite-177810.jpg",366,{"id":343,"source_url":344,"license_code":345,"credit_html":346,"title":347,"description":348,"author":349,"original_width":350,"original_height":351},27334,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=32615615","CC BY 3.0","John Hagstrom, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=32615615\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Vauquelinite, Dioptase-439000.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAntigorite\" class=\"extiw\" title=\"en:Antigorite\">Antigorite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDioptase\" class=\"extiw\" title=\"en:Dioptase\">Dioptase\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Blue Bell Mine (Blue Bell claims; Hard Luck Mine; Hard Luck claims; Atkinson), Baker, Soda Lake Mts, San Bernardino Co., California, USA\u003C\u002Fdd>\n\u003Cdd>\u003Ci>Original description:\u003C\u002Fi> Vauquelinite and Dioptase. specimen dimension is 21CM X9CM, field of view is 5mm. taken with a Variscope using Helicon Focus.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","John Hagstrom",1024,768,{"id":353,"source_url":354,"license_code":269,"credit_html":355,"title":356,"description":357,"author":358,"original_width":359,"original_height":360},6460,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=129540021","Kaethe17, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=129540021\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Krokoit-Vauquelinit.jpg","\u003Ca href=\"https:\u002F\u002Fde.wikipedia.org\u002Fwiki\u002FKrokoit\" class=\"extiw\" title=\"de:Krokoit\">Krokoit\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fde.wikipedia.org\u002Fwiki\u002FVauquelinit\" class=\"extiw\" title=\"de:Vauquelinit\">Vauquelinit\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fde.wikipedia.org\u002Fwiki\u002FPh%C3%B6nikochroit\" class=\"extiw\" title=\"de:Phönikochroit\">Phönikochroit\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fde.wikipedia.org\u002Fwiki\u002FQuarz\" class=\"extiw\" title=\"de:Quarz\">Quarz\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fde.wikipedia.org\u002Fwiki\u002FMuskovit\" class=\"extiw\" title=\"de:Muskovit\">Muskovit\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Fundort: Grube Beresowsk bei Jekaterinburg, Ural, ca. 1846\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Kaethe17",5013,3342,{"id":362,"source_url":363,"license_code":250,"credit_html":364,"title":365,"description":366,"author":282,"original_width":367,"original_height":368},84941,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10162647","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10162647\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Crocoite-Vauquelinite-224156.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCrocoite\" class=\"extiw\" title=\"en:Crocoite\">Crocoite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FVauquelinite\" class=\"extiw\" title=\"en:Vauquelinite\">Vauquelinite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Berezovskoe Au Deposit (Berezovsk Mines), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBerezovsky\" class=\"extiw\" title=\"en:Berezovsky\">Berezovskii (Berezovskii Zavod)\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FYekaterinburg\" class=\"extiw\" title=\"en:Yekaterinburg\">Ekaterinburg (Sverdlovsk)\u003C\u002Fa>, Ekaterinburgskaya (Sverdlovskaya) Oblast', Middle Urals, Urals Region, Russia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2728.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 11.5 x 7.1 x 6.0 cm.\u003C\u002Fdd>\n\u003Cdd>This large specimen is an excellent, important example of crocoite from the type locality for the species. Note the robust, sharp, stereotypic crystal habit so different from that which we normally see in the far more common Australian material. These stand out, dramatically, from most crocoite you will see from Australian localities. The crystals are to 1.4 cm, on matrix. Also, you have rich pistachio-green druse of the very rare phosphate-chromate Vauquelinite all over the specimen. Discovered in the early 1800s, these are some of the oldest well-studied lead mineral species and both are lead chromates. Ex. Ed N. Harrison Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",600,397,{"id":370,"source_url":371,"license_code":250,"credit_html":372,"title":373,"description":366,"author":282,"original_width":307,"original_height":374},84942,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10162648","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10162648\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Crocoite-Vauquelinite-224157.jpg",318,{"id":376,"source_url":377,"license_code":250,"credit_html":378,"title":379,"description":305,"author":282,"original_width":380,"original_height":283},4823,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10455043","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10455043\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Embreyite-Vauquelinite-oldeuro-54b.jpg",592,{"id":382,"source_url":383,"license_code":250,"credit_html":384,"title":385,"description":305,"author":282,"original_width":307,"original_height":386},4825,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10455045","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10455045\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Embreyite-Vauquelinite-oldeuro-54d.jpg",382,{"id":388,"source_url":389,"license_code":390,"credit_html":391,"title":392,"description":393,"author":394,"original_width":395,"original_height":396},84948,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118200635","CC BY-SA 2.0","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118200635\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Crocoite with Vauquelinite and Quarts (48140158842).jpg","Beresovsk, USSR","Pacific Museum of Earth from Canada",4000,6000,[398],{"id":399,"url":400,"label":401,"formula":402,"spacegroup":403,"year":213},14161,"\u002Fcif\u002F14161.cif","Fanfani 1968","Pb2 Cu Cr P O9 H","P 1 21\u002Fn 1",[405,406,407,408,409,410,411,412,413,414],"Chromate of Lead and Copper","Chromphosphorkupferbleispath","Hemiprismatischer Olivenmalachit","Laxmannit","Laxmannita","Laxmannite","Melnochlor-Malachit","Phosphorchromit","Plomb chromé","Vauqueline",[416,420,424,428,431,435,438,442,445,449,453,456],{"lang":417,"names":418},"ca",[419],"vauquelinita",{"lang":421,"names":422},"de",[423],"Vauquelinit",{"lang":425,"names":426},"es",[427],"Vauquelinita",{"lang":429,"names":430},"eu",[427],{"lang":432,"names":433},"he",[434],"ווקלניט",{"lang":436,"names":437},"it",[7],{"lang":439,"names":440},"nl",[441],"Vauqueliniet",{"lang":443,"names":444},"pl",[423],{"lang":446,"names":447},"ta",[448],"வோக்வெலிணைட்டு",{"lang":450,"names":451},"uk",[452],"Вокеленіт",{"lang":454,"names":455},"vi",[7],{"lang":457,"names":458},"zh",[459],"磷铬铜铅矿","Q2252069",{"history":11,"applications":11}]