[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:1157":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":16,"elements":17,"sigelements":21,"key_elements":22,"impurities":23,"cim":24,"ima_status":25,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":11,"discovery_year":11,"strunz10ed1":28,"strunz10ed2":29,"strunz10ed3":30,"strunz10ed4":31,"dana8ed1":32,"dana8ed2":33,"dana8ed3":34,"dana8ed4":34,"csystem":35,"cclass":36,"spacegroup":11,"spacegroupset":37,"a":38,"b":39,"c":40,"alpha":37,"beta":41,"gamma":37,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":42,"csmetamict":14,"commentcrystal":43,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":44,"tlform":11,"hmin":45,"hmax":46,"hardtype":11,"vhnmin":37,"vhnmax":37,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":47,"dmeas2":48,"dcalc":47,"dmeaserror":11,"dcalcerror":11,"commentdense":49,"lustre":50,"lustretype":51,"commentluster":11,"diapheny":52,"streak":53,"colour":54,"commentcolor":11,"colors":55,"streak_colors":59,"luminescence":11,"uv":60,"cleavage":61,"cleavagetype":62,"fracturetype":63,"tenacity":64,"commentbreak":11,"opticaltype":65,"opticalsign":66,"opticalalpha":67,"opticalalpha2":37,"opticalalphaerror":68,"opticalbeta":69,"opticalbeta2":37,"opticalbetaerror":68,"opticalgamma":70,"opticalgamma2":37,"opticalgammaerror":68,"opticalomega":37,"opticalomega2":37,"opticalomegaerror":11,"opticalepsilon":37,"opticalepsilon2":37,"opticalepsilonerror":11,"opticaln":37,"opticaln2":37,"opticalnerror":11,"optical2vcalc":71,"optical2vcalc2":37,"optical2vcalcerror":11,"optical2vmeasured":72,"optical2vmeasured2":37,"optical2vmeasurederror":11,"rimin":73,"rimax":74,"opticaldispersion":75,"opticalpleochroism":76,"opticalpleochorismdesc":77,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":78,"opticalr":11,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":11,"otheroccurrence":79,"type_specimen_store":80,"description_short":81,"aboutname":82,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":83,"reviewed_at":11,"variety_of":11,"varieties":84,"group_members":85,"associates":108,"confused_with":118,"type_localities":119,"occurrence_total":124,"citations":125,"images":368,"structures":649,"synonyms":672,"language_names":701,"wikidata_qid":849,"texts":850},1157,"1:1:1157:6","903ad8d4-540d-4b97-bca4-48fff757e371","Crocoite","Crc",0,"mineral",null,29313,13455,false,"PbCr\u003Csup>6+\u003C\u002Fsup>O\u003Csub>4\u003C\u002Fsub>","Pb(CrO\u003Csub>4\u003C\u002Fsub>)",[18,19,20],"Cr","Pb","O",[18,19,20],[18,19],"Zn, S","27.2.5",[26,27],"APPROVED","GRANDFATHERED","7","F","A","20","35","3","1","Monoclinic",5,"0","7.12","7.421","6.80","102.41",4,"Space group P21\u002Fn.","Crystals commonly prismatic [001] to acicular crystals with nearly square outline; elongated parallel to \u003Cmi>[_101]\u003C\u002Fmi>; pseudo-octahedral at times, with {111} \u003Cmi>{_111}\u003C\u002Fmi>, or acute rhombohedral with {110} \u003Cmi>{_h0l}\u003C\u002Fmi>. Faces usually smooth and brilliant; {110} commonly striated [001], and the steep orthodomes rounded or distorted. Crystals are often cavernous or hollow. Massive; imperfectly columnar to granular.\r\n\r\nForms include:\r\n\u003Cmi>a{100}, b{010}, c{001}, α{310}, d{210}, g{320}, m{110}, ζ{350}, f{120}, h{101}, ρ{502}, n{401}, χ{801}, k{_101}, x{_301}, l{_401}, ε{_501}, θ{_601}, w{012}, z{011}, y{021}, t{111}, π{221}, ϑ{331}, s{441}, λ{_112}, γ{_223}, v{_111}, e{11.1.1}, ψ{911}, G{812}, N{711}, η{412}, q{12.4.1}, L{2.1.10}, g{841}, Q{953}, H{435}, δ{11.10.1}, p{_1_3.1.5}, τ{_911}, r{_612}, A{_511}, R{_1_8.4.1}, ξ{_411}, β{_312}, φ{_311}, F{_621}, Y{_931}, B{_521}, u{_211}, E{_328}, o{_8.7.10}, M{6.10.9}, σ{352}, i{123}, μ(154}, D{_265}.  Also an additional couple dozen probable forms.\u003C\u002Fmi>",2.5,3,"5.97","6.02","6.06 (Dundas mat.); 6.12 (artificial mat.)","Adamantine, vitreous","Sub-Adamantine,Sub-Vitreous,Resinous,Waxy","Transparent,Translucent","Yellow-orange","Orange, red, yellow; orange-red in transmitted light.",[56,57,58],"red","orange","yellow",[58,57],"Not fluorescent in UV.","Distinct on {110}, indistinct on {001} and {100}.","Poor\u002FIndistinct","Conchoidal","brittle","Biaxial","+","2.29",2,"2.36","2.66","54","57",2.29,2.66,"very strong r > v inclined","Weak","X = Red-orange\r\nY = Red-orange\r\nZ = Blood red","Y = b; Z ∧ c = 5.5°.","Uncommon secondary mineral in lead deposits associated with chromium-bearing rocks.","Natural History Museum, Paris","Crocoite is commonly found as crystals, usually as long prismatic crystals and more rarely as equant crystals, but are most often poorly terminated, and are usually of a bright hyacinth-red color, which are translucent and have an adamantine to vitreou...","Originally recognized by Mikhail Vassil’evich Lomonosov in 1763 as a red lead ore. Johann Gottlob Lehmann in 1766 named it Nova Minera Plumbi. Various authors later gave the mineral a name signifying the presence of lead and the color red: minera plumbi rubra (Wallerius, 1778), Rothes bleierz (Werner, 1774), and Plomb rouge (Macquart, 1789). After the element chromium was announced in 1798, a new series of names was applied to the species: Plomb chromaté (Haüy, 1801), Kallochrom (Hausmann, 1813), etc. Renamed Crocise by François Sulpice Beudant in 1832 and Krokoisite by Franz von Kobell in 1838. Translated to the current pronunciation, Krokoit, by Johann August Breithaupt in 1841. Named Beresofite in 1844 by Charles Upham Shepard. Named Lehmannite by Henry J. Brooke and William H. Miller in 1852. The name crocoite comes from the Greek κρόκος \"crocon\" = saffron, alluding to the saffron-orange color of its powder.","2026-04-18 16:45:51",[],[86,92,100],{"id":87,"name":88,"entrytype":9,"csystem":35,"ima_formula":89,"mindat_formula":89,"hmin":36,"hmax":36,"dmeas":90,"dcalc":91,"primary_image_id":11},6865,"Cheralite","CaTh(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>","4.72","5.26",{"id":93,"name":94,"entrytype":9,"csystem":35,"ima_formula":95,"mindat_formula":96,"hmin":36,"hmax":36,"dmeas":97,"dcalc":98,"primary_image_id":99},1955,"Huttonite","Th(SiO\u003Csub>4\u003C\u002Fsub>)","ThSiO\u003Csub>4\u003C\u002Fsub>","7.1","7.18",11786,{"id":101,"name":102,"entrytype":9,"csystem":35,"ima_formula":103,"mindat_formula":103,"hmin":42,"hmax":104,"dmeas":105,"dcalc":106,"primary_image_id":107},3444,"Rooseveltite","Bi(AsO\u003Csub>4\u003C\u002Fsub>)",4.5,"6.86","7.21",3343,[109],{"id":110,"name":111,"entrytype":9,"csystem":35,"ima_formula":112,"mindat_formula":113,"hmin":45,"hmax":114,"dmeas":115,"dcalc":116,"primary_image_id":117},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,[],[120],{"id":121,"txt":122,"latitude":11,"longitude":11,"country":123},19472,"Tsvetnoi Mine, Uspenskaya Hill, Berezovsk deposit, Beryozovsky, Sverdlovsk Oblast, Russia","Russia",81,[126,130,134,138,142,146,150,154,157,161,165,169,172,175,178,181,184,187,190,194,198,202,206,210,214,218,222,226,229,234,239,243,247,251,256,261,266,271,275,279,284,289,294,298,303,308,312,317,322,326,331,335,340,344,349,353,358,363],{"id":127,"year":128,"html":129,"doi":11},16106806,1763,"Lomonossow, Michail Wassiljewitsch (1763) \u003Ci>Erste Grundlagen Der Metallurgie Oder Des Huttenwesens\u003C\u002Fi>.",{"id":131,"year":132,"html":133,"doi":11},16106807,1766,"Lehmann, Johann G. (1766) De nova mineral plumbi specie crystallina rubra. Novi Commentarii Academiae Petropolitanae, 12, 356. [as Nova minera Plumbi].",{"id":135,"year":136,"html":137,"doi":11},16106808,1767,"Lehmann, Johann G. (1767) Nachricht von einem neu endechten Bleyerze. Neues Hamburg Magazin: 7: 336-348.",{"id":139,"year":140,"html":141,"doi":11},16106809,1771,"Pallas, Peter Simon (1771) Reise durch verschiedene Provinzen des russischen Reichs. St. Petersburg, Imperial Academy of Sciences, 2, 235. [as Minerai de plomb rouge].",{"id":143,"year":144,"html":145,"doi":11},16106810,1774,"Werner, Abraham Gottlieb (1774) Von den äusserlichen Kennzeichen der Fossilien. Leipzig, 296. [as Rotbleierz and Rothes Bleierz].",{"id":147,"year":148,"html":149,"doi":11},16106811,1775,"Wallerius, J. G. (1775) Systema mineralogicum. Holmiae. vol. 2: 309. [as Minera Plumbi rubra].",{"id":151,"year":152,"html":153,"doi":11},16106812,1789,"Macquart, Louis Charles Henri (1789) Sur le Plomb rouge de Sibérie. Journal de Physique de Chimie D'histoire Naturelle et des Arts, 34. 389-396. [as Plombe rouge de Sibérie].",{"id":155,"year":152,"html":156,"doi":11},16106813,"Marquart, Louis Charles Henri (1789) Essais ou Recueil de mémoires sur plusieurs points de minéralogie, Chez Cechet, Paris, pp. 580 + 7 plates.",{"id":158,"year":159,"html":160,"doi":11},16106814,1792,"Bindheim, Johann Jakob (1792) Ueber den Sibirischen rothen Bleyspat. Der Gesellschaft Naturforschender Freunde zu Berlin, 4, 287-318.",{"id":162,"year":163,"html":164,"doi":11},16106815,1794,"Vauquelin, Louis-Nicolas (1794) Sur un nouvel Acide métallique qui existe dans le plomb rouge de Sibérie. Journal de Physique de Chimie D'histoire Naturelle et des Arts, 45, 393-395. [as plombe rouge de Sibérie].",{"id":166,"year":167,"html":168,"doi":11},16106816,1798,"Vauquelin, Louis (1798) Le Journal de physique et le radium, Paris: 46: 152, 311. [as Plombe rouge de Sibérie].",{"id":170,"year":167,"html":171,"doi":11},16106817,"Vauquelin, Louis-Nicolas (1798) Sur le Chrome, ou métal trouvé dans le plomb rouge de Sibérie. Journal de Physique de Chimie D'histoire Naturelle et des Arts, 46, 152-153.",{"id":173,"year":167,"html":174,"doi":11},16106818,"Vauquelin, Louis-Nicolas (1798) Memoire. Sur le Chrome, ou métal trouvé dans le plomb rouge de Sibérie. Journal de Physique de Chimie D'histoire Naturelle et des Arts, 46, 311-315.",{"id":176,"year":167,"html":177,"doi":11},16106819,"Vauquelin, Louis-Nicolas (1798) On a new metallic substance contained in the red lead of Siberia, to which it is proposed to give the name of chrôme on account of the property it possesses of colouring every substance combined with it. The Philosophical Magazine, 1(3), 279-285.",{"id":179,"year":167,"html":180,"doi":11},16106820,"Vauquelin, Louis-Nicolas (1798) Second memoir on the metal contained in the red lead of Siberia. The Philosophical Magazine, 1(4), 361-367.",{"id":182,"year":167,"html":183,"doi":11},16106821,"Vauquelin, Louis-Nicolas (1798) Mémoire: Sur une nouvelle substance métallique contenue dans le plomb rouge de Sibérie et qu’on propose d’appeler Chrôme, à cause de la propriété qu’il a de colorer les combinaisons où il entre. Annales de Chimie, 25, 21-31.",{"id":185,"year":167,"html":186,"doi":11},16106822,"Vauquelin, Louis-Nicolas (1798) Second mémoire: Sur le métal contenu dans le plomb rouge de Sibérie. Annales de Chimie, 25, 194-205.",{"id":188,"year":167,"html":189,"doi":11},16106823,"Klaproth, Martin Heinrich (1798) Nachricht von einem neu entdeckten Metall aus dem rothen Sibirischen Bleyspathe. Crell's Chemische Annalen für die Freunde der Naturlehre, 1, 80-82.",{"id":191,"year":192,"html":193,"doi":11},16106824,1799,"Vauquelin, Louis-Nicolas (1799) Analysis of the Red Lead of Siberia, with Experiments on the new Metal it contains. A Journal of Natural Philosophy, Chemistry and the Arts (Nicholson's Journal), 2, 387-393.",{"id":195,"year":196,"html":197,"doi":11},12960848,1801,"Haüy, René Just (1801) \u003Ci>Traité de Minéralogie\u003C\u002Fi> (1st ed.) Chez Louis, Paris.",{"id":199,"year":200,"html":201,"doi":11},17557205,1813,"Hausmann, Johann Friedrich Ludwig (1813) \u003Ci>Handbuch der Mineralogie\u003C\u002Fi> (1st ed.). Vandenhoeck und Ruprecht. \u003Ca target='_blank' href='https:\u002F\u002Farchive.org\u002Fdownload\u002Fhandbuchdermine01hausgoog\u002Fhandbuchdermine01hausgoog.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":203,"year":204,"html":205,"doi":11},18530121,1832,"Beudant, François-Sulpice (1832) \u003Ci>Traité élémentaire de minéralogie. Deuxiéme Edition [Elementary Treatise on Mineralogy. Second Edition]\u003C\u002Fi> (2nd ed.) Vol. 2 - Tome II [Volume  II]. Chez Verdière. \u003Ca target='_blank' href='https:\u002F\u002Farchive.org\u002Fdownload\u002Fbub_gb_XSRCAAAAcAAJ\u002Fbub_gb_XSRCAAAAcAAJ.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":207,"year":208,"html":209,"doi":11},12962122,1838,"von Kobell, Franz (1838) \u003Ci>Grundzüge der Mineralogie: Grundzüge der Mineralogie: zum Gebrauche bey Vorlesungen, sowie zum Selbststudium Entworfen\u003C\u002Fi>. Johann Leonard Schrag. \u003Ca target='_blank' href='https:\u002F\u002Farchive.org\u002Fdownload\u002Fbub_gb__y8-AAAAcAAJ\u002Fbub_gb__y8-AAAAcAAJ.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":211,"year":212,"html":213,"doi":11},16106829,1841,"Breithaupt, A. (1841) Vollständige Handbuch der Mineralogie. Vol. 2: 262. [as Bleiischer Chromspath].",{"id":215,"year":216,"html":217,"doi":11},16106831,1844,"Shepard, Charles U. (1844) Treatise on Mineralogy. second edition: 121. [as Beresofite].",{"id":219,"year":220,"html":221,"doi":11},12911330,1852,"Brooke, Henry J., Phillips, William (1852) \u003Ci>An Elementary Introduction to Mineralogy\u003C\u002Fi> (6th ed.) \u003Ca target='_blank' href='https:\u002F\u002Farchive.org\u002Fdownload\u002Fbub_gb_mxsIAAAAIAAJ\u002Fbub_gb_mxsIAAAAIAAJ.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":223,"year":224,"html":225,"doi":11},16106832,1860,"Dauber, H. (1860) Ermittelung krystallographischer Constanten und des Grades ihrer Zuverlässigkeit. 22. Rothbleierz. Sitzungsberichte der Kaiserlichen Akademie der Wissenschaften. Mathematisch-Naturwissenschaftliche Classe, 42, 19-54. [as rothbleierz]",{"id":227,"year":224,"html":228,"doi":11},16106833,"Haidinger, W. (1860) Notiz uber das Rothbleierz von den Philippinen. Sitzungsberichte der Kaiserlichen Akademie der Wissenschaften. Mathematisch-Naturwissenschaftliche Classe, 42, 742-743.  [as rothbleierz]",{"id":230,"year":231,"html":232,"doi":233},399196,1882,"Des Cloizeaux, Alfred (1882) Note sur les constantes optiques de la crocoïse. \u003Ci>Bulletin de Minéralogie\u003C\u002Fi>,  5 (4) 103-105 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3406\u002Fbulmi.1882.1718'>doi:10.3406\u002Fbulmi.1882.1718\u003C\u002Fa>","10.3406\u002Fbulmi.1882.1718",{"id":235,"year":236,"html":237,"doi":238},399556,1887,"Bourgeois, Léon (1887) Nouveau procédé de reproduction de la crocoïse. \u003Ci>Bulletin de Minéralogie\u003C\u002Fi>,  10 (5) 187-190 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3406\u002Fbulmi.1887.2064'>doi:10.3406\u002Fbulmi.1887.2064\u003C\u002Fa>","10.3406\u002Fbulmi.1887.2064",{"id":240,"year":241,"html":242,"doi":11},16106835,1896,"Palache, C. (1896) Crocoite from Tasmania. American Journal of Science, s4-1(5), 389-390.",{"id":244,"year":245,"html":246,"doi":11},16106836,1902,"Van Name, R.G. (1902) On crystals of crocoite from Tasmania. American Journal of Science, s4-13(77), 339-342.",{"id":248,"year":249,"html":250,"doi":11},16106837,1904,"de Schulten, A. (1904) Production artificielle par voie humide des chromates anhydres cristallisés de baryum, de plomb, de strontium. Bulletin de la Société française de Minéralogie: 27: 129-137 (135).",{"id":252,"year":253,"html":254,"doi":255},10636321,1906,"Anderson, C. (1906) Mineralogical notes. No. III. Axinite, petterdite, crocoite, and datolite. \u003Ci>Records of the Australian Museum\u003C\u002Fi>, 6. 133-144 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3853\u002Fj.0067-1975.6.1906.998'>doi:10.3853\u002Fj.0067-1975.6.1906.998\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Farchive.org\u002Fdownload\u002Fbiostor-52913\u002Fbiostor-52913.pdf' class='refpdflink'>\u003C\u002Fa>","10.3853\u002Fj.0067-1975.6.1906.998",{"id":257,"year":258,"html":259,"doi":260},14970544,1913,"Hevesy, Georg V., Paneth, Fritz (1913) Die Löslichkeit des Bleisulfids und Bleichromats. \u003Ci>Zeitschrift für anorganische Chemie\u003C\u002Fi>, 82 (1) 323-328 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1002\u002Fzaac.19130820125'>doi:10.1002\u002Fzaac.19130820125\u003C\u002Fa>","10.1002\u002Fzaac.19130820125",{"id":262,"year":263,"html":264,"doi":265},8747187,1919,"Gröger, Max (1919) Über Bleichromat. \u003Ci>Zeitschrift für anorganische und allgemeine Chemie\u003C\u002Fi>, 109. 226-234 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1002\u002Fzaac.19201090117'>doi:10.1002\u002Fzaac.19201090117\u003C\u002Fa>","10.1002\u002Fzaac.19201090117",{"id":267,"year":268,"html":269,"doi":270},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":272,"year":273,"html":274,"doi":11},4468629,1922,"(1922) \u003Ci>Atlas Der Krystallformen\u003C\u002Fi> Vol. 7 - Text - Band VII - Pyroaurit-Rutil. Carl Winters Universitätsbuchhandlung, Heidelberg.",{"id":276,"year":277,"html":278,"doi":11},16106841,1929,"Hintze, C. (1929) Handbuch der Mineralogie. Berlin and Leipzig. 6 volumes: 1 [3B]: 4030.",{"id":280,"year":281,"html":282,"doi":283},104337,1930,"Goßner, B.; Mußgnug, F. (1930) Über Krokoit, Lautarit und Dietzeit und deren kristallographische Beziehungen. \u003Ci>Zeitschrift für Kristallographie\u003C\u002Fi>,  75 (1). 410-420 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1515\u002Fzkri-1930-0131'>doi:10.1515\u002Fzkri-1930-0131\u003C\u002Fa>","10.1515\u002Fzkri-1930-0131",{"id":285,"year":286,"html":287,"doi":288},104432,1931,"Brill, R. (1931) Über das Gitter von Bleichromat. \u003Ci>Zeitschrift für Kristallographie\u003C\u002Fi>,  77 (1-6). 506 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1931.77.1.506'>doi:10.1524\u002Fzkri.1931.77.1.506\u003C\u002Fa>","10.1524\u002Fzkri.1931.77.1.506",{"id":290,"year":291,"html":292,"doi":293},15203009,1932,"Quittner, F.; Sapgir, J.; Rassudowa, N. (1932) Die rhombische Modifikation des Bleichromates. \u003Ci>Zeitschrift für anorganische und allgemeine Chemie\u003C\u002Fi>,  204 (3). 315-317 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1002\u002Fzaac.19322040309'>doi:10.1002\u002Fzaac.19322040309\u003C\u002Fa>","10.1002\u002Fzaac.19322040309",{"id":295,"year":291,"html":296,"doi":297},15202942,"Wagner, Hans; Haug, Robert; Zipfel, Matthias (1932) Die Modifikationen des Bleichromats. \u003Ci>Zeitschrift für anorganische und allgemeine Chemie\u003C\u002Fi>,  208 (3). 249-254 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1002\u002Fzaac.19322080304'>doi:10.1002\u002Fzaac.19322080304\u003C\u002Fa>","10.1002\u002Fzaac.19322080304",{"id":299,"year":300,"html":301,"doi":302},8752742,1933,"Deines, O. V. (1933) Über die zweite monokline und die rhomboedrische Modifikation des Schwefels. \u003Ci>Zeitschrift für anorganische und allgemeine Chemie\u003C\u002Fi>, 214. 330-336 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1002\u002Fzaac.19332140314'>doi:10.1002\u002Fzaac.19332140314\u003C\u002Fa>","10.1002\u002Fzaac.19332140314",{"id":304,"year":305,"html":306,"doi":307},105628,1939,"Gliszçzynski, S. von (1939) Beitrag zur »Isomorphie« von Monazit und Krokoit. \u003Ci>Zeitschrift für Kristallographie, Mineralogie und Petrographie\u003C\u002Fi>,  101 (1-6). 1-16 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1939.101.1.1'>doi:10.1524\u002Fzkri.1939.101.1.1\u003C\u002Fa>","10.1524\u002Fzkri.1939.101.1.1",{"id":309,"year":310,"html":311,"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":313,"year":314,"html":315,"doi":316},621364,1965,"Quareni, S., de Pieri, R. (1965) A three-dimensional refinement of the structure of crocoite, PbCrO4. \u003Ci>Acta Crystallographica\u003C\u002Fi>,  19 (2) 287-289 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1107\u002Fs0365110x65003304'>doi:10.1107\u002Fs0365110x65003304\u003C\u002Fa>","10.1107\u002Fs0365110x65003304",{"id":318,"year":319,"html":320,"doi":321},6466,1971,"Wilkins, R. W. T. (1971) The Raman spectrum of crocoite. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  38 (294) 249-250 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1971.038.294.15'>doi:10.1180\u002Fminmag.1971.038.294.15\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_38\u002F38-294-249.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1971.038.294.15",{"id":323,"year":324,"html":325,"doi":11},12906660,1972,"Chapman, Albert H. (1972) On a Spectacular Find of Crocoite in the Adelaide Mine, Dundas, Tasmania [Australia], in \u003Ci>May - June 1972\u003C\u002Fi>. \u003Ci>The Mineralogical Record\u003C\u002Fi>,  3 (3) Tucson. 111-114",{"id":327,"year":328,"html":329,"doi":330},111168,1986,"Effenberger, H., Pertlik, F. (1986) Four monazite type structures: comparison of SrCrO\u003Csub>4\u003C\u002Fsub>, SrSeO\u003Csub>4\u003C\u002Fsub>, PbCrO\u003Csub>4\u003C\u002Fsub> (crocoite), and PbSeO\u003Csub>4\u003C\u002Fsub>. \u003Ci>Zeitschrift für Kristallographie\u003C\u002Fi>,  176 (1). 75-83 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1986.176.1-2.75'>doi:10.1524\u002Fzkri.1986.176.1-2.75\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fzk\u002Fvol176\u002FZK176_75.pdf' class='refpdflink'>\u003C\u002Fa>","10.1524\u002Fzkri.1986.176.1-2.75",{"id":332,"year":333,"html":334,"doi":11},16106849,1996,"Bushmakin, A.F. (1996) Crocoite from the Berezovsk gold mines. World of Stones, 10, 28–31.",{"id":336,"year":337,"html":338,"doi":339},997722,2001,"Li, Zhongsheng, Moore, T.A, Weaver, S.D, Finkelman, R.B (2001) Crocoite: an unusual mode of occurrence for lead in coal. \u003Ci>International Journal of Coal Geology\u003C\u002Fi>,  45 (4) 289-293 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1016\u002Fs0166-5162(00)00024-0'>doi:10.1016\u002Fs0166-5162(00)00024-0\u003C\u002Fa>","10.1016\u002Fs0166-5162(00)00024-0",{"id":341,"year":342,"html":343,"doi":11},16771791,2003,"Anthony, John Williams, Bideaux, Richard A., Bladh, Kenneth W., Nichols, Monte C. (2003) \u003Ci>Handbook of Mineralogy\u003C\u002Fi> Vol. 5 - Borates, Carbonates, Sulfates. Mineral Data Publishing, Tucson, Arizona.",{"id":345,"year":346,"html":347,"doi":348},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":350,"year":351,"html":352,"doi":11},16963834,2005,"(2005) Crocoite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fcrocoite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":354,"year":355,"html":356,"doi":357},30599,2007,"Cook, Robert B. (2007) Crocoite: Dundas, Tasmania, Australia. \u003Ci>Rocks & Minerals\u003C\u002Fi>,  82 (1) 50-54 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3200\u002Frmin.82.1.50-54'>doi:10.3200\u002Frmin.82.1.50-54\u003C\u002Fa>","10.3200\u002Frmin.82.1.50-54",{"id":359,"year":360,"html":361,"doi":362},31350,2014,"Pohwat, Paul W. (2014) Connoisseur's Choice: Crocoite, Adelaide Mine, Tasmania, Australia. \u003Ci>Rocks & Minerals\u003C\u002Fi>,  89 (2) 158-165 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1080\u002F00357529.2014.865437'>doi:10.1080\u002F00357529.2014.865437\u003C\u002Fa>","10.1080\u002F00357529.2014.865437",{"id":364,"year":365,"html":366,"doi":367},18443653,2025,"Kläger, Sebastian; Zeman, Otto E. O.; Bräuniger, Thomas (2025) Determination of the 207Pb Chemical Shift Tensor in Crocoite, PbCrO4, Using Single-Crystal NMR Spectroscopy. \u003Ci>Crystals\u003C\u002Fi>,  15 (5). 480 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3390\u002Fcryst15050480'>doi:10.3390\u002Fcryst15050480\u003C\u002Fa>","10.3390\u002Fcryst15050480",[369,379,389,395,400,410,415,420,425,432,436,443,452,460,468,477,486,496,501,510,517,523,528,535,542,550,554,561,567,574,582,590,598,606,612,619,626,633,639],{"id":370,"source_url":371,"license_code":372,"credit_html":373,"title":374,"description":375,"author":376,"original_width":377,"original_height":378},6456,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=5848602","CC BY-SA 2.5","JJ Harrison (https:\u002F\u002Fwww.jjharrison.com.au\u002F), via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=5848602\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Crocoite from the Dundas extended mine, Dundas, Tasmania, Australia.jpg","\u003Cp>Crocoite from the Dundas extended mine, Dundas, Tasmania, Australia\n\u003Cbr>\u003Cb>Camera data\u003C\u002Fb>\n\u003C\u002Fp>\n\u003Cul>\u003Cli>\u003Cb>Camera\u003C\u002Fb> Canon EOS 400D\u003C\u002Fli>\n\u003Cli>\u003Cb>Lens\u003C\u002Fb> Canon EF 70-200mm f4L w\u002F 12mm extension tube\u003C\u002Fli>\n\u003Cli>\u003Cspan style=\"font-weight:bold\">Flash\u003C\u002Fspan> Shoot through umbrella\u003C\u002Fli>\n\u003Cli>\u003Cb>Focal length\u003C\u002Fb> 94 mm\u003C\u002Fli>\n\u003Cli>\u003Cb>Aperture\u003C\u002Fb> f\u002F11\u003C\u002Fli>\n\u003Cli>\u003Cb>Exposure time\u003C\u002Fb> 1\u002F160 s\u003C\u002Fli>\n\u003Cli>\u003Cb>Sensivity\u003C\u002Fb> ISO 100\u003C\u002Fli>\u003C\u002Ful>","JJ Harrison (https:\u002F\u002Fwww.jjharrison.com.au\u002F)",1923,1301,{"id":380,"source_url":381,"license_code":382,"credit_html":383,"title":384,"description":385,"author":386,"original_width":387,"original_height":388},6462,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=167211831","CC BY 4.0","Animalculum, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=167211831\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Crocoite, Musee de Mineralogie, Paris, 2025, 2.jpg","Crocoite from Dundas, Tasmania in Musee de Mineralogie, Paris","Animalculum",1998,2663,{"id":390,"source_url":391,"license_code":382,"credit_html":392,"title":7,"description":11,"author":11,"original_width":393,"original_height":394},29548,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F113445","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F113445\" rel=\"noopener\">Department of Geology, TalTech\u003C\u002Fa> via Europeana",1000,666,{"id":396,"source_url":397,"license_code":398,"credit_html":399,"title":7,"description":11,"author":11,"original_width":393,"original_height":394},29549,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F91942","CC BY-SA 4.0","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby-sa\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F91942\" rel=\"noopener\">The Estonian Museum of Natural History\u003C\u002Fa> via Europeana",{"id":401,"source_url":402,"license_code":403,"credit_html":404,"title":405,"description":406,"author":407,"original_width":408,"original_height":409},6458,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=13277461","CC BY-SA 3.0","Didier Descouens, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=13277461\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Crocoïte Dundas2p.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCrocoite\" class=\"extiw\" title=\"en:Crocoite\">Crocoite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Adelaide Mine (Adelaide Pty Mine; Adelaide Proprietary Mine), Dundas mineral field, Zeehan District, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FTasmania\" class=\"extiw\" title=\"en:Tasmania\">Tasmania\u003C\u002Fa>, Australia\u003C\u002Fdd>\n\u003Cdd>Size of view : 3.5 cm\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Didier Descouens",4397,2888,{"id":411,"source_url":412,"license_code":398,"credit_html":413,"title":7,"description":11,"author":11,"original_width":393,"original_height":414},29550,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F92341","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby-sa\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F92341\" rel=\"noopener\">The Estonian Museum of Natural History\u003C\u002Fa> via Europeana",681,{"id":416,"source_url":417,"license_code":398,"credit_html":418,"title":7,"description":11,"author":11,"original_width":393,"original_height":419},29551,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F65239","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby-sa\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F65239\" rel=\"noopener\">The Estonian Museum of Natural History\u003C\u002Fa> via Europeana",782,{"id":421,"source_url":422,"license_code":398,"credit_html":423,"title":7,"description":11,"author":11,"original_width":393,"original_height":424},29552,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F65332","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby-sa\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F65332\" rel=\"noopener\">The Estonian Museum of Natural History\u003C\u002Fa> via Europeana",818,{"id":426,"source_url":427,"license_code":382,"credit_html":428,"title":429,"description":385,"author":386,"original_width":430,"original_height":431},6461,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=167137542","Animalculum, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=167137542\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Crocoite, Musee de Mineralogie, Paris, 2025.jpg",2229,2972,{"id":433,"source_url":434,"license_code":382,"credit_html":435,"title":7,"description":11,"author":11,"original_width":393,"original_height":394},29553,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F116470","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F116470\" rel=\"noopener\">Department of Geology, TalTech\u003C\u002Fa> via Europeana",{"id":437,"source_url":438,"license_code":382,"credit_html":439,"title":440,"description":385,"author":386,"original_width":441,"original_height":442},6463,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=168135643","Animalculum, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=168135643\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Crocoite, Musee de Mineralogie, Paris, 2025, 3.jpg",2911,2183,{"id":444,"source_url":445,"license_code":398,"credit_html":446,"title":447,"description":448,"author":449,"original_width":450,"original_height":451},52801,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=75818244","Géry PARENT, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=75818244\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Crocoite, dunsdasite.jpg","Crocoite, dundasite : Adelaide Mine (Adelaide Pty Mine, Adelaide Proprietary Mine), Dundas Mineral Field, Zeehan District, Tasmanie, Australia","Géry PARENT",1975,1317,{"id":453,"source_url":454,"license_code":382,"credit_html":455,"title":456,"description":457,"author":458,"original_width":459,"original_height":459},6459,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=87372573","Marie-Lan Taÿ Pamart, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=87372573\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Crocoite Red Lead MNHN Minéralogie.jpg","Crocoite from Red Lead, Tasmania. Gallery of Mineralogy and Geology of the French National Museum of Natural History in Paris.","Marie-Lan Taÿ Pamart",4500,{"id":461,"source_url":462,"license_code":403,"credit_html":463,"title":464,"description":465,"author":376,"original_width":466,"original_height":467},6457,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=8080888","JJ Harrison (https:\u002F\u002Fwww.jjharrison.com.au\u002F), via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=8080888\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Dundasite and Crocoite.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDundasite\" class=\"extiw\" title=\"en:Dundasite\">Dundasite\u003C\u002Fa> (white) and \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCrocoite\" class=\"extiw\" title=\"en:Crocoite\">Crocoite\u003C\u002Fa> (red orange) from \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDundas,_Tasmania\" class=\"extiw\" title=\"en:Dundas, Tasmania\">Dundas\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FTasmania\" class=\"extiw\" title=\"en:Tasmania\">Tasmania\u003C\u002Fa>.",2139,1429,{"id":469,"source_url":470,"license_code":398,"credit_html":471,"title":472,"description":473,"author":474,"original_width":475,"original_height":476},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":478,"source_url":479,"license_code":403,"credit_html":480,"title":481,"description":482,"author":483,"original_width":484,"original_height":485},7495,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=61338694","Leon Hupperichs, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=61338694\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Dundasite, Crocoite-507982.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDundasite\" class=\"extiw\" title=\"en:Dundasite\">Dundasite\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: Adelaide Mine (Adelaide Pty Mine; Adelaide Proprietary Mine), Dundas mineral field, Zeehan District, West Coast municipality, Tasmania, Australia\u003C\u002Fdd>\n\u003Cdd>Dimensions: 3 x 2.5 cm\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Leon Hupperichs",842,728,{"id":487,"source_url":488,"license_code":489,"credit_html":490,"title":491,"description":492,"author":493,"original_width":494,"original_height":495},7496,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=61339022","CC BY 3.0","Ralph Bottrill, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=61339022\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Dundasite, Crocoite-583175.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDundasite\" class=\"extiw\" title=\"en:Dundasite\">Dundasite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCrocoite\" class=\"extiw\" title=\"en:Crocoite\">Crocoite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Dimensions: 35 mm x 20 mm ; field of view: 20 mm\u003C\u002Fdd>\n\u003Cdd>Locality: Adelaide Mine (Adelaide Pty Mine; Adelaide Proprietary Mine), Dundas mineral field, Zeehan District, West Coast municipality, Tasmania, Australia\u003C\u002Fdd>\n\u003Cdd>\u003Ci>Original description:\u003C\u002Fi> Botryoidal white dundasite, with a pale blue-green colour on the surface, a some small overgrowing crocoite crystals\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Ralph Bottrill",1121,850,{"id":497,"source_url":498,"license_code":398,"credit_html":499,"title":500,"description":448,"author":449,"original_width":450,"original_height":451},7497,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=75818243","Géry PARENT, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=75818243\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Crocoite, dundasite 1.jpg",{"id":502,"source_url":503,"license_code":403,"credit_html":504,"title":505,"description":506,"author":507,"original_width":508,"original_height":509},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>","Robert M. Lavinsky",672,800,{"id":511,"source_url":512,"license_code":403,"credit_html":513,"title":514,"description":506,"author":507,"original_width":515,"original_height":516},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",366,400,{"id":518,"source_url":519,"license_code":403,"credit_html":520,"title":521,"description":522,"author":507,"original_width":508,"original_height":509},7787,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10446899","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10446899\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Crocoite-Embreyite-d06-244a.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\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: small cabinet, 6.0 x 5.4 x 4.6 cm\n\u003Cdl>\u003Cdt>Embreyite, Vauquelenite, Crocoite\u003C\u002Fdt>\u003C\u002Fdl>\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, mostly broken but nice for the color. Olive green vauquelinite occurs as chalky, green growths on crocoite. More than 200 years after these specimens were discovered, the extremely rare species embreyite was discovered on similar old specimens in the drawers of the BMNH; and then other old specimens in major holdings were re-examined. This piece has a particularly rich cluster of admittedly ugly, but mineralogically important, crystals of this more recently identified species (the minute black crystals, nestled in a vug). It is an eccentric, but very fine specimen!\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",{"id":524,"source_url":525,"license_code":403,"credit_html":526,"title":527,"description":522,"author":507,"original_width":515,"original_height":516},7788,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10446900","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10446900\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Crocoite-Embreyite-d06-244b.jpg",{"id":529,"source_url":530,"license_code":403,"credit_html":531,"title":532,"description":533,"author":507,"original_width":516,"original_height":534},7789,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10446901","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10446901\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Crocoite-Embreyite-d06-244c.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCrocoite\" class=\"extiw\" title=\"en:Crocoite\">Crocoite\u003C\u002Fa>, Embreyite\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, 6.0 x 5.4 x 4.6 cm\n\u003Cdl>\u003Cdt>Embreyite, Vauquelenite, Crocoite\u003C\u002Fdt>\u003C\u002Fdl>\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, mostly broken but nice for the color. Olive green vauquelinite occurs as chalky, green growths on crocoite. More than 200 years after these specimens were discovered, the extremely rare species embreyite was discovered on similar old specimens in the drawers of the BMNH; and then other old specimens in major holdings were re-examined. This piece has a particularly rich cluster of admittedly ugly, but mineralogically important, crystals of this more recently identified species (the minute black crystals, nestled in a vug). It is an eccentric, but very fine specimen!\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",374,{"id":536,"source_url":537,"license_code":403,"credit_html":538,"title":539,"description":540,"author":507,"original_width":509,"original_height":541},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>",623,{"id":543,"source_url":544,"license_code":403,"credit_html":545,"title":546,"description":547,"author":507,"original_width":548,"original_height":549},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>",660,700,{"id":551,"source_url":552,"license_code":382,"credit_html":553,"title":7,"description":11,"author":11,"original_width":393,"original_height":394},30919,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F108759","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",{"id":555,"source_url":556,"license_code":403,"credit_html":557,"title":558,"description":559,"author":507,"original_width":560,"original_height":509},39967,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10151853","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10151853\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cerussite-Crocoite-177812.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCerussite\" class=\"extiw\" title=\"en:Cerussite\">Cerussite\u003C\u002Fa> (Var.: \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCerussite\" class=\"extiw\" title=\"en:Cerussite\">Chrome-Cerussite\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: West Comet Mine, Dundas mineral field, Zeehan district, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FTasmania\" class=\"extiw\" title=\"en:Tasmania\">Tasmania\u003C\u002Fa>, Australia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-7202.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 5.9 x 5.1 x 3.3 cm.\u003C\u002Fdd>\n\u003Cdd>This specimen has an unusual type of cerussite with discrete coloration due to chromium rich content, and the sharp crystals reach .7 cm across. Studded on the cerussite are bright orange prisms of crocoite, to .3 cm across. Ex. Dr. Edward David Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",705,{"id":562,"source_url":563,"license_code":403,"credit_html":564,"title":565,"description":559,"author":507,"original_width":516,"original_height":566},39968,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10151854","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10151854\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cerussite-Crocoite-177814.jpg",278,{"id":568,"source_url":569,"license_code":403,"credit_html":570,"title":571,"description":572,"author":507,"original_width":573,"original_height":516},39979,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10443911","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10443911\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cerussite-Crocoite-51jc.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCerussite\" class=\"extiw\" title=\"en:Cerussite\">Cerussite\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: Comet Mine, Dundas mineral field, Zeehan district, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FTasmania\" class=\"extiw\" title=\"en:Tasmania\">Tasmania\u003C\u002Fa>, Australia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-177.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: small cabinet, 5.9 x 5.1 x 3.3 cm\n\u003Cdl>\u003Cdt>Chrome Cerussite with Crocoite\u003C\u002Fdt>\u003C\u002Fdl>\u003C\u002Fdd>\n\u003Cdd>This specimen has an unusual type of cerussite with discrete coloration due to chromium rich content, and the sharp crystals reach .7 cm across. In person, they are a bit more yellow than appears here. Studded on the cerussite are bright orange prisms of crocoite, to .3 cm across. Rare and unusual material to begin with but in association with crocoite...this I have only but once before seen for sale! For some reason, the cerussite and crocoite zones seem to not overlap often. This is an old piece, though I do not know how old. Ed thought 30-40 years.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",322,{"id":575,"source_url":576,"license_code":403,"credit_html":577,"title":578,"description":579,"author":376,"original_width":580,"original_height":581},52794,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=8166469","JJ Harrison (https:\u002F\u002Fwww.jjharrison.com.au\u002F), via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=8166469\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Dundasite and Crocoite 2.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDundasite\" class=\"extiw\" title=\"en:Dundasite\">Dundasite\u003C\u002Fa> (white) and \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCrocoite\" class=\"extiw\" title=\"en:Crocoite\">Crocoite\u003C\u002Fa> (red orange) from \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDundas,_Tasmania\" class=\"extiw\" title=\"en:Dundas, Tasmania\">Dundas\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FTasmania\" class=\"extiw\" title=\"en:Tasmania\">Tasmania\u003C\u002Fa>",1752,1344,{"id":583,"source_url":584,"license_code":403,"credit_html":585,"title":586,"description":587,"author":507,"original_width":588,"original_height":589},52795,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10135934","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10135934\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Crocoite-Gibbsite-Dundasite-60826.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\u002FGibbsite\" class=\"extiw\" title=\"en:Gibbsite\">Gibbsite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDundasite\" class=\"extiw\" title=\"en:Dundasite\">Dundasite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Dundas mineral field, Zeehan district, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FTasmania\" class=\"extiw\" title=\"en:Tasmania\">Tasmania\u003C\u002Fa>, Australia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-175.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>A STRIKING and beautiful plate covered with orange crocoite, brown gibbsite and cream-colored dundasite from Dundas, Tasmania, Australia. The brown gibbsite is a tentative identification. This is an UNCOMMONLY FINE combination specimen from this locality, especially the dundasite. 7.8 x 4.5 x 1.4 cm\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",394,600,{"id":591,"source_url":592,"license_code":403,"credit_html":593,"title":594,"description":595,"author":507,"original_width":596,"original_height":597},52796,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10138983","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10138983\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Crocoite-Dundasite-118004.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\u002FDundasite\" class=\"extiw\" title=\"en:Dundasite\">Dundasite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Adelaide Mine (Adelaide Pty Mine; Adelaide Proprietary Mine), Dundas mineral field, Zeehan District, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FTasmania\" class=\"extiw\" title=\"en:Tasmania\">Tasmania\u003C\u002Fa>, Australia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-176.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 10.2 x 6.2 x 2.0 cm.\u003C\u002Fdd>\n\u003Cdd>A fine and showy Tasmania rarity of brick-red crocoite crystals on a wing-like CABINET plate nearly covered with tan dundasite, a rare lead carbonate. This excellent piece is from near the Type Locality - the Adelaide Mine.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",625,398,{"id":599,"source_url":600,"license_code":489,"credit_html":601,"title":602,"description":603,"author":493,"original_width":604,"original_height":605},52797,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=61337587","Ralph Bottrill, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=61337587\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Dundasite, Gibbsite, Crocoite, Goethite-583974.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDundasite\" class=\"extiw\" title=\"en:Dundasite\">Dundasite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGibbsite\" class=\"extiw\" title=\"en:Gibbsite\">Gibbsite\u003C\u002Fa>, \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\u002FGoethite\" class=\"extiw\" title=\"en:Goethite\">Goethite\u003C\u002Fa> (Size 30 mm)\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Adelaide Mine (Adelaide Pty Mine; Adelaide Proprietary Mine), Dundas mineral field, Zeehan District, West Coast municipality, Tasmania, Australia\u003C\u002Fdd>\n\u003Cdd>\u003Ci>Original description:\u003C\u002Fi> Botryoidal-fibrous dundasite, white to pale blue-green on the surface, altering to microcrystalline gibbsite (white). Minor crocoite and goethite\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",924,622,{"id":607,"source_url":608,"license_code":489,"credit_html":609,"title":610,"description":603,"author":493,"original_width":611,"original_height":541},52798,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=61337747","Ralph Bottrill, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=61337747\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Dundasite, Gibbsite, Crocoite, Goethite-583975.jpg",935,{"id":613,"source_url":614,"license_code":403,"credit_html":615,"title":616,"description":617,"author":507,"original_width":549,"original_height":618},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>",530,{"id":620,"source_url":621,"license_code":403,"credit_html":622,"title":623,"description":624,"author":507,"original_width":549,"original_height":625},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":627,"source_url":628,"license_code":403,"credit_html":629,"title":630,"description":631,"author":507,"original_width":589,"original_height":632},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>",397,{"id":634,"source_url":635,"license_code":403,"credit_html":636,"title":637,"description":631,"author":507,"original_width":516,"original_height":638},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":640,"source_url":641,"license_code":642,"credit_html":643,"title":644,"description":645,"author":646,"original_width":647,"original_height":648},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,[650,657,664,668],{"id":651,"url":652,"label":653,"formula":654,"spacegroup":655,"year":656},3337,"\u002Fcif\u002F3337.cif","Bandiello 2012","(Pb.997 Fe.003) Cr O4","P 1 21\u002Fn 1",2012,{"id":658,"url":659,"label":660,"formula":661,"spacegroup":662,"year":663},3338,"\u002Fcif\u002F3338.cif","Knight 2000","Pb Cr O4","P n m a",2000,{"id":665,"url":666,"label":667,"formula":661,"spacegroup":655,"year":328},3339,"\u002Fcif\u002F3339.cif","Effenberger 1986",{"id":669,"url":670,"label":671,"formula":661,"spacegroup":655,"year":314},3340,"\u002Fcif\u002F3340.cif","Quareni 1965",[673,674,675,676,677,678,679,680,681,682,683,684,685,686,687,688,689,690,691,692,693,694,695,696,697,698,699,700],"Beresofite (of Shepard)","Beresowite (of Shepard)","Bleichromat","Bleiischer Chromspath","Callochrome","Chromate of lead","Chrombleispath","Chromsaures Blei","Crocoise","Crocoisit","Crocoisita","Crocoisite","Kallochrom","Kollochrom","Krokoisit","Lehmannit (nach Brooke)","Lehmannita","Lehmannite (of Brooke)","Minera plumbi rubra","Minera spathiforma rubra","Minerai de plomb rouge","Nova minera plumbi","Plomb chromaté","Plombe rouge de Sibérie","Red lead ore","Red lead-ore from Beresov","Rotbleierz","Rothes Bleierz",[702,706,710,714,718,722,725,728,732,736,740,744,748,752,758,761,764,768,772,775,778,782,786,790,793,797,800,804,808,811,815,818,822,826,830,833,836,840,843,846],{"lang":703,"names":704},"ar",[705],"كروكوئيت",{"lang":707,"names":708},"az",[709],"Krokoit",{"lang":711,"names":712},"be",[713],"Кракаіт",{"lang":715,"names":716},"bg",[717],"Крокоит",{"lang":719,"names":720},"ca",[721],"crocoïta",{"lang":723,"names":724},"cs",[709],{"lang":726,"names":727},"de",[709,699],{"lang":729,"names":730},"el",[731],"Κροκοΐτης",{"lang":733,"names":734},"es",[735],"crocoíta",{"lang":737,"names":738},"et",[739],"krokoiit",{"lang":741,"names":742},"eu",[743],"krokoita",{"lang":745,"names":746},"fa",[747],"کروکوئیت",{"lang":749,"names":750},"fi",[751],"Krokoiitti",{"lang":753,"names":754},"fr",[755,756,757,690,693,695,696],"Beresofite","Crocoïse","Crocoïte",{"lang":759,"names":760},"hu",[709],{"lang":762,"names":763},"it",[7],{"lang":765,"names":766},"ja",[767],"紅鉛鉱",{"lang":769,"names":770},"ko",[771],"홍연석",{"lang":773,"names":774},"ky",[717],{"lang":776,"names":777},"mk",[717],{"lang":779,"names":780},"nb",[781],"krokoitt",{"lang":783,"names":784},"nds",[709,785],"Rootblieierz",{"lang":787,"names":788},"nl",[789],"crocoiet",{"lang":791,"names":792},"nn",[781],{"lang":794,"names":795},"oc",[796],"Crocoïta",{"lang":798,"names":799},"pl",[709],{"lang":801,"names":802},"pt",[735,803],"Crocoíte",{"lang":805,"names":806},"ru",[807,717],"Красная свинцовая руда",{"lang":809,"names":810},"sk",[709],{"lang":812,"names":813},"sr",[814],"крокојин",{"lang":816,"names":817},"sv",[709],{"lang":819,"names":820},"uk",[821],"Крокоїт",{"lang":823,"names":824},"vi",[825,7],"Crocoit",{"lang":827,"names":828},"zh",[829],"铬铅矿",{"lang":831,"names":832},"zh-cn",[829],{"lang":834,"names":835},"zh-hans",[829],{"lang":837,"names":838},"zh-hant",[839],"鉻鉛礦",{"lang":841,"names":842},"zh-hk",[839],{"lang":844,"names":845},"zh-sg",[829],{"lang":847,"names":848},"zh-tw",[839],"Q422903",{"history":851,"applications":855},{"markdown":852,"model_version":853,"prompt_version":854,"reviewed_at":11},"Grind crocoite to a powder and it turns the orange of saffron threads. That likeness gave the mineral its name. The French mineralogist François Sulpice Beudant coined *crocoise* in 1832, from the Greek *krokos* — saffron — for the colour[1]. The word was soon altered to *crocoisite*, then settled as crocoite.\n\nThe mineral was found long before it had that name. It came from the Beresof mines, near Yekaterinburg in the Ural Mountains of Russia[2]. In 1763, the Russian scholar Mikhail Lomonosov recognised it as a red lead ore[3]. Johann Gottlob Lehmann knew the same orange-red stone from that field. In 1766 he described it as *Nova Minera Plumbi* — a new lead ore[3][4]. Across Europe it became known as Siberian red lead[2].\n\nThe early names all pointed at the two things anyone could see: lead and the colour red. Werner called it *Rothes bleierz* — red lead ore — in 1774; Jean-Baptiste Macquart wrote *Plomb rouge*, red lead, in 1789[3].\n\nThen a chemist took the stone apart. Louis-Nicolas Vauquelin received samples of the Siberian ore and, in 1797, found a new metallic element hiding inside it[5]. He produced an orange oxide from the crocoite, then heated it with charcoal to isolate the metal itself[5]. He named the element chromium, from the Greek *chroma* — colour — because its compounds came in so many vivid shades[5]. Martin Klaproth reached the same discovery independently[6]. Crocoite had given the world a new element.\n\nAfter chromium was announced, the mineral picked up names built on the metal. René Just Haüy called it *Plomb chromaté* — chromated lead — in 1801, and Johann Hausmann coined *Kallochrom* in 1813[3]. Beudant's *crocoise* of 1832 eventually won out[1]. Later writers offered rivals that did not last: Breithaupt's *Krokoit* in 1841, Shepard's *Beresofite* in 1844, and *Lehmannite*, named for Lehmann by Henry Brooke and William Miller in 1852[3].\n\nThe most celebrated crocoite came much later, and from the other side of the world. The Adelaide mine at Dundas, in western Tasmania, is described as probably the prime source of crocoite in the world[7]. Its long, blade-like scarlet crystals are prized by collectors, and the mineral is the official mineral emblem of Tasmania[7].","claude-opus-4-8","1.7.0",{"markdown":856,"model_version":853,"prompt_version":854,"reviewed_at":11},"Crocoite has almost no industrial use today. It is lead chromate, and its composition is identical to the artificial product chrome yellow once used as a paint pigment[1]. But that pigment is made synthetically, not mined from crocoite. Chromium for industry now comes from chromite, a far more common ore that displaced crocoite as the metal's main source[2]. Because the mineral carries both lead and hexavalent chromium, it is also toxic, which rules out everyday handling[1].\n\nWhat demand exists is from collectors. Crocoite's long, blade-like scarlet crystals make it one of the most prized specimens a cabinet can hold. The Adelaide mine at Dundas, Tasmania, is regarded as probably the prime source in the world[3]. Beyond the specimen trade, the mineral has no current commercial application."]