[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:1969":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":14,"elements":15,"sigelements":20,"key_elements":21,"impurities":11,"cim":22,"ima_status":23,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":26,"discovery_year":11,"strunz10ed1":27,"strunz10ed2":28,"strunz10ed3":29,"strunz10ed4":30,"dana8ed1":31,"dana8ed2":32,"dana8ed3":32,"dana8ed4":33,"csystem":34,"cclass":35,"spacegroup":36,"spacegroupset":37,"a":38,"b":37,"c":39,"alpha":37,"beta":37,"gamma":37,"aerror":40,"berror":11,"cerror":41,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":42,"csmetamict":13,"commentcrystal":43,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":44,"tlform":11,"hmin":45,"hmax":45,"hardtype":11,"vhnmin":37,"vhnmax":37,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":46,"dmeas2":46,"dcalc":47,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":48,"commentluster":11,"diapheny":49,"streak":50,"colour":51,"commentcolor":11,"colors":52,"streak_colors":56,"luminescence":11,"uv":57,"cleavage":58,"cleavagetype":59,"fracturetype":60,"tenacity":61,"commentbreak":11,"opticaltype":62,"opticalsign":63,"opticalalpha":37,"opticalalpha2":37,"opticalalphaerror":11,"opticalbeta":37,"opticalbeta2":37,"opticalbetaerror":11,"opticalgamma":37,"opticalgamma2":37,"opticalgammaerror":11,"opticalomega":64,"opticalomega2":37,"opticalomegaerror":11,"opticalepsilon":65,"opticalepsilon2":37,"opticalepsilonerror":11,"opticaln":37,"opticaln2":37,"opticalnerror":11,"optical2vcalc":37,"optical2vcalc2":37,"optical2vcalcerror":11,"optical2vmeasured":37,"optical2vmeasured2":37,"optical2vmeasurederror":11,"rimin":66,"rimax":67,"opticaldispersion":11,"opticalpleochroism":68,"opticalpleochorismdesc":11,"opticalbirefringence":69,"opticalcomments":11,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":70,"opticalr":11,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":71,"industrial":11,"occurrence":72,"otheroccurrence":11,"type_specimen_store":11,"description_short":73,"aboutname":74,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":75,"reviewed_at":11,"variety_of":11,"varieties":76,"group_members":77,"associates":78,"confused_with":146,"type_localities":147,"occurrence_total":154,"citations":155,"images":227,"structures":277,"synonyms":295,"language_names":298,"wikidata_qid":338,"texts":339},1969,"1:1:1969:5","a4f49f8b-05db-4229-9bef-c334fb049be9","Hydrocerussite","Hcer",0,"mineral",null,2790,false,"Pb\u003Csub>3\u003C\u002Fsub>(CO\u003Csub>3\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>",[16,17,18,19],"Pb","O","C","H",[16,17,18,19],[16],"11.9.2",[24,25],"APPROVED","GRANDFATHERED",1877,"5","B","E","10","16a","2","1","Trigonal",13,99,"0","5.239","23.65",5,2,3,"Space group R-3m, with a = 5.2465(6) and c = 23.702(3) A, is given by Martinetto et al. (2002), on the basis of a structure solution from powder data.","Crystals steep pyramidal \u003Cmi>{h0h_1}\u003C\u002Fmi> with {0001} very small at times. Thin scales with a hexagonal presentation and flattened {0001}; also thick tabular {0001}. Frequently as a surface alteration of lead, cerussite, etc.",3.5,"6.8","6.94","Adamantine,Pearly,Dull","Transparent,Translucent","White","White or gray; colourless in transmitted light",[53,54,55],"white","gray","colorless",[53],"Usually fluoresces medium to dull white, also dull-yellow. Bright white in 365nm LED.","On {0001}.","Perfect","Irregular\u002FUneven","brittle","Uniaxial","-","2.09","1.94",1.94,2.09,"Non-pleochroic","0.15","Parallel","Soluble in acids with effervescence.","Metamorphosed Mn-Fe deposit.","Hydrocerussite is a secondary mineral usually found in oxidized lead ore deposits. It it less common than cerussite (anhydrous lead carbonate). Also reported as a mineralised component of the mycobiont of the Stereocaulon vesuvianum lichen found in a r...","Named in 1877 by Nils Adolf Erik Nordenskiöld in allusion to the composition, being a HYDRated lead carbonate, similar to cerussite.","2026-04-18 16:41:38",[],[],[79,88,97,106,115,124,132,139],{"id":80,"name":81,"entrytype":9,"csystem":82,"ima_formula":83,"mindat_formula":84,"hmin":42,"hmax":45,"dmeas":85,"dcalc":86,"primary_image_id":87},934,"Cerussite","Orthorhombic","Pb(CO\u003Csub>3\u003C\u002Fsub>)","PbCO\u003Csub>3\u003C\u002Fsub>","6.53","6.558",5045,{"id":89,"name":90,"entrytype":9,"csystem":91,"ima_formula":92,"mindat_formula":92,"hmin":93,"hmax":93,"dmeas":94,"dcalc":95,"primary_image_id":96},1641,"Galena","Isometric","PbS",2.5,"7.60","7.57",9582,{"id":98,"name":99,"entrytype":9,"csystem":100,"ima_formula":101,"mindat_formula":102,"hmin":93,"hmax":42,"dmeas":103,"dcalc":104,"primary_image_id":105},2361,"Leadhillite","Monoclinic","Pb\u003Csub>4\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)(CO\u003Csub>3\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>","Pb\u003Csub>4\u003C\u002Fsub>(CO\u003Csub>3\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)(OH)\u003Csub>2\u003C\u002Fsub>","6.55","6.57",14233,{"id":107,"name":108,"entrytype":9,"csystem":109,"ima_formula":110,"mindat_formula":111,"hmin":93,"hmax":42,"dmeas":112,"dcalc":113,"primary_image_id":114},2593,"Matlockite","Tetragonal","PbClF","PbFCl","7.12","7.16",15598,{"id":116,"name":117,"entrytype":9,"csystem":118,"ima_formula":119,"mindat_formula":120,"hmin":45,"hmax":121,"dmeas":37,"dcalc":122,"primary_image_id":123},2597,"Mattheddleite","Hexagonal","Pb\u003Csub>5\u003C\u002Fsub>(SiO\u003Csub>4\u003C\u002Fsub>)\u003Csub>1.5\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)\u003Csub>1.5\u003C\u002Fsub>Cl","Pb\u003Csub>5\u003C\u002Fsub>(SiO\u003Csub>4\u003C\u002Fsub>)\u003Csub>1.5\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)\u003Csub>1.5\u003C\u002Fsub>(Cl,OH)",4.5,"6.96",15615,{"id":125,"name":126,"entrytype":9,"csystem":82,"ima_formula":127,"mindat_formula":128,"hmin":93,"hmax":42,"dmeas":129,"dcalc":130,"primary_image_id":131},2641,"Mendipite","Pb\u003Csub>3\u003C\u002Fsub>O\u003Csub>2\u003C\u002Fsub>Cl\u003Csub>2\u003C\u002Fsub>","Pb\u003Csub>3\u003C\u002Fsub>Cl\u003Csub>2\u003C\u002Fsub>O\u003Csub>2\u003C\u002Fsub>","7.24","7.22",30182,{"id":133,"name":134,"entrytype":9,"csystem":91,"ima_formula":16,"mindat_formula":16,"hmin":135,"hmax":135,"dmeas":136,"dcalc":137,"primary_image_id":138},2358,"Native Lead",1.5,"11.37","11.341",17194,{"id":140,"name":141,"entrytype":9,"csystem":100,"ima_formula":142,"mindat_formula":142,"hmin":42,"hmax":42,"dmeas":143,"dcalc":144,"primary_image_id":145},3096,"Paralaurionite","PbCl(OH)","6.15","6.28",72629,[],[148],{"id":149,"txt":150,"latitude":151,"longitude":152,"country":153},3167,"Långban Mine, Långban Ore District, Filipstad, Värmland County, Sweden",59.8553767,14.2648029,"Sweden",221,[156,159,164,169,173,178,182,186,191,195,199,204,208,213,218,222],{"id":157,"year":26,"html":158,"doi":11},16112397,"Nordenskild (1877) Geologiska Föeningens I Stockholm. Förhandlinger, Stockholm: 3: 381.",{"id":160,"year":161,"html":162,"doi":163},399623,1888,"Bourgeois, Léon (1888) Sur la reproduction artificielle de l'hydrocérusite, sur la composition chimique de cette espèce minérale et sur la constitution du blanc de céruse. \u003Ci>Bulletin de Minéralogie\u003C\u002Fi>,  11 (6) 221-225 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3406\u002Fbulmi.1888.3192'>doi:10.3406\u002Fbulmi.1888.3192\u003C\u002Fa>","10.3406\u002Fbulmi.1888.3192",{"id":165,"year":166,"html":167,"doi":168},5400,1889,"Heddle, Matthew Forster (1889) On Dudgeonite, Hydroplumbite, Plumbonacrite. and Plattnerite. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  8 (39) 200-203 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1889.008.39.07'>doi:10.1180\u002Fminmag.1889.008.39.07\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_8\u002F8-39-200.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1889.008.39.07",{"id":170,"year":171,"html":172,"doi":11},16112399,1901,"Flink (1901) Bull. Geol. Inst. Upsala: 5: 94.",{"id":174,"year":175,"html":176,"doi":177},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":179,"year":180,"html":181,"doi":11},16112401,1925,"Spencer (1925) Mineralogical Magazine: 20: 80.",{"id":183,"year":184,"html":185,"doi":11},16112402,1926,"Aminoff (1926) Geologiska Föeningens I Stockholm. Förhandlinger, Stockholm: 48: 44.",{"id":187,"year":188,"html":189,"doi":190},1051528,1953,"Kokkoros, P., Vassiliadis, K. (1953) Röntgenkristallographie von Hydrocerussit. \u003Ci>Tschermaks Mineralogische und Petrographische Mitteilungen\u003C\u002Fi>,  3 (4). 298-304 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fbf01135346'>doi:10.1007\u002Fbf01135346\u003C\u002Fa>","10.1007\u002Fbf01135346",{"id":192,"year":193,"html":194,"doi":11},16112404,1964,"Voronova, A. A. and Vainshtein, B. K. (1964): An electron-diffraction study of the crystal structure of PbCO3PbO(H2O)2. Kristallografiya 9, 197-203. (in Russian).",{"id":196,"year":197,"html":198,"doi":11},15939621,1977,"Keller, P. (1977): Hydrocerussit von Tsumeb\u002FSüdwestafrika. Der Aufschluss, 28, 413-415.",{"id":200,"year":201,"html":202,"doi":203},8311287,1984,"Taylor, Peter, Lopata, Vincent J. (1984) Stability and solubility relationships between some solids in the system PbO–CO2–H2O. \u003Ci>Canadian Journal of Chemistry\u003C\u002Fi>, 62 (3). 395-402 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1139\u002Fv84-070'>doi:10.1139\u002Fv84-070\u003C\u002Fa>","10.1139\u002Fv84-070",{"id":205,"year":201,"html":206,"doi":207},12666099,"Flemming, Nona J., Lopata, Vincent J., Sanipelli, Barbara L., Taylor, Peter (1984) Thermal decomposition of basic lead carbonates: A comparison of hydrocerussite and plumbonacrite. \u003Ci>Thermochimica Acta\u003C\u002Fi>, 81. 1-8 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1016\u002F0040-6031(84)85104-7'>doi:10.1016\u002F0040-6031(84)85104-7\u003C\u002Fa>","10.1016\u002F0040-6031(84)85104-7",{"id":209,"year":210,"html":211,"doi":212},195408,2002,"Martinetto, Pauline, Anne, Michel, Dooryhée, Eric, Walter, Philippe, Tsoucaris, Georges (2002) Synthetic hydrocerussite, 2PbCO\u003Csub>3\u003C\u002Fsub>·Pb(OH)\u003Csub>2\u003C\u002Fsub>, by X-ray powder diffraction. \u003Ci>Acta Crystallographica Section C Crystal Structure Communications\u003C\u002Fi>,  58 (6). i82-i84 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1107\u002Fs0108270102006844'>doi:10.1107\u002Fs0108270102006844\u003C\u002Fa>","10.1107\u002Fs0108270102006844",{"id":214,"year":215,"html":216,"doi":217},16109136,2003,"BURFORD, EUAN P., KIERANS, MARTIN, GADD, GEOFFREY M. (2003) Geomycology: fungi in mineral substrata. \u003Ci>Mycologist\u003C\u002Fi>,  17 (3). 98-107 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1017\u002Fs0269915x03003112'>doi:10.1017\u002Fs0269915x03003112\u003C\u002Fa>","10.1017\u002Fs0269915x03003112",{"id":219,"year":220,"html":221,"doi":11},16964928,2005,"(2005) Hydrocerussite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fhydrocerussite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":223,"year":224,"html":225,"doi":226},8511210,2018,"Siidra, Oleg, Nekrasova, Diana, Depmeier, Wulf, Chukanov, Nikita, Zaitsev, Anatoly, Turner, Rick (2018) Hydrocerussite-related minerals and materials: structural principles, chemical variations and infrared spectroscopy. \u003Ci>Acta Crystallographica Section B Structural Science, Crystal Engineering and Materials\u003C\u002Fi>, 74 (2). 182-195 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1107\u002Fs2052520618000768'>doi:10.1107\u002Fs2052520618000768\u003C\u002Fa>","10.1107\u002Fs2052520618000768",[228,238,247,255,263,271],{"id":229,"source_url":230,"license_code":231,"credit_html":232,"title":233,"description":234,"author":235,"original_width":236,"original_height":237},11820,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14865770","CC BY-SA 3.0","Christian Rewitzer, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14865770\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hydrocerussite-163774.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHydrocerussite\" class=\"extiw\" title=\"en:Hydrocerussite\">Hydrocerussite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Passa Limani Cove slag locality, Passa Limani area, Lavrion District slag localities, Lavrion (Laurion; Laurium) District, Attikí (Attica; Attika) Prefecture, Greece\u003C\u002Fdd>\n\u003Cdd>Picture width 2 mm. Collection and photograph Christian Rewitzer\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Christian Rewitzer",1024,961,{"id":239,"source_url":240,"license_code":231,"credit_html":241,"title":242,"description":243,"author":244,"original_width":245,"original_height":246},11815,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10126428","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10126428\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cerussite-Hydrocerussite-38165.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\u002FHydrocerussite\" class=\"extiw\" title=\"en:Hydrocerussite\">Hydrocerussite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Tsumeb Mine (Tsumcorp Mine), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FTsumeb\" class=\"extiw\" title=\"en:Tsumeb\">Tsumeb\u003C\u002Fa>, Otjikoto (Oshikoto) Region, Namibia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2428.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>An excellent and showy specimen of floater, cyclically-twinned, gray cerussite crystals altering to hydrocerussite, showing partial alteration on the outside of the cerussite, from Tsumeb. The end-on shots highlight the intricate twinning of the crystals. Very minor edgewear is certainly not detracting from such an uncommon Tsumeb mineral in good crystals. 3.6 x 3.5 x 2.2 cm\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Robert M. Lavinsky",540,508,{"id":248,"source_url":249,"license_code":231,"credit_html":250,"title":251,"description":252,"author":244,"original_width":253,"original_height":254},11816,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10150551","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10150551\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hydrocerussite-Cerussite-173902.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHydrocerussite\" class=\"extiw\" title=\"en:Hydrocerussite\">Hydrocerussite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCerussite\" class=\"extiw\" title=\"en:Cerussite\">Cerussite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Tsumeb Mine (Tsumcorp Mine), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FTsumeb\" class=\"extiw\" title=\"en:Tsumeb\">Tsumeb\u003C\u002Fa>, Otjikoto (Oshikoto) Region, Namibia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2428.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 5.7 x 1.9 x 1.5 cm.\u003C\u002Fdd>\n\u003Cdd>A super-sharp and attractive pseudomorph-in-progress with an excellent habit and interesting and unusual tan color. Ex. Willy Israel Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",274,700,{"id":256,"source_url":257,"license_code":231,"credit_html":258,"title":259,"description":260,"author":244,"original_width":261,"original_height":262},11817,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10174558","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10174558\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hydrocerussite-Anglesite-290656.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHydrocerussite\" class=\"extiw\" title=\"en:Hydrocerussite\">Hydrocerussite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnglesite\" class=\"extiw\" title=\"en:Anglesite\">Anglesite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Tsumeb Mine (Tsumcorp Mine), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FTsumeb\" class=\"extiw\" title=\"en:Tsumeb\">Tsumeb\u003C\u002Fa>, Otjikoto (Oshikoto) Region, Namibia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2428.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 8.4 x 6.4 x 5.4 cm.\u003C\u002Fdd>\n\u003Cdd>A superb specimen from the Ed Swoboda Pseudomorph Collection. It has snow-white pseudomorphs of hydrocerussite after sharp blocky, pyramidal anglesite crystals from Tsumeb. The second is rare enough; the replacement I cannot say I have seen another as good in this style. It is so sharp it looks carved. The large crystal is 3.7 cm. Very rare in this size and quality. Probably one of the finest hydrocerussite pseudomorphs around. Ex. Rob Smith Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",465,433,{"id":264,"source_url":265,"license_code":231,"credit_html":266,"title":267,"description":268,"author":244,"original_width":269,"original_height":270},7494,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=61338336","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=61338336\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Dundasite, Hydrocerussite-393112.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\u002FHydrocerussite\" class=\"extiw\" title=\"en:Hydrocerussite\">Hydrocerussite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Tsumeb Mine (Tsumcorp Mine), Tsumeb, Otjikoto Region (Oshikoto), Namibia\u003C\u002Fdd>\n\u003Cdd>Size: 8 cm x 7 cm x 5.7 cm\u003C\u002Fdd>\n\u003Cdd>Dundasite is a very rare hydrated lead, aluminum carbonate species. This relatively large specimen hosts the richest single amount of Dundasite I have seen on a Tsumeb piece. Normally the mineral is white from other locales, and seldom found in such color intensity. It was in an old African collection, and later comes from the Marshall Sussman Tsumeb collection. What is more, the intense blue crystal clusters of dundasite are perched on contrasting, stark white crystals of reticulated cerussite. The unusual bright white color of the cerussite is due to their alteration to hydrocerussite - probably a partial alteration, if not quite complete. Joe Budd photos\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",944,768,{"id":272,"source_url":273,"license_code":231,"credit_html":274,"title":275,"description":268,"author":244,"original_width":276,"original_height":270},52799,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=61338398","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=61338398\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Dundasite, Hydrocerussite-393113.jpg",928,[278,284,288],{"id":279,"url":280,"label":281,"formula":282,"spacegroup":283,"year":224},6353,"\u002Fcif\u002F6353.cif","Siidra 2018","Pb1.5 C O4 H","R -3 m",{"id":285,"url":286,"label":287,"formula":282,"spacegroup":283,"year":210},6355,"\u002Fcif\u002F6355.cif","Martinetto 2002",{"id":289,"url":290,"label":291,"formula":292,"spacegroup":293,"year":294},6356,"\u002Fcif\u002F6356.cif","Cowley 1956","Pb3 C2 O8 H2","P 3 1 m",1956,[296,297],"Hydrocerussiet","Hydrocerussita",[299,303,307,311,315,319,323,326,330,334],{"lang":300,"names":301},"ca",[302],"hidrocerussita",{"lang":304,"names":305},"de",[306],"Hydrocerussit",{"lang":308,"names":309},"eu",[310],"Hidrocerussita",{"lang":312,"names":313},"fr",[314],"hydrocérusite",{"lang":316,"names":317},"it",[318],"Idrocerussite",{"lang":320,"names":321},"nb",[322],"hydrocerussitt",{"lang":324,"names":325},"nn",[322],{"lang":327,"names":328},"sl",[329],"hidrocerusit",{"lang":331,"names":332},"sr",[333],"хидроцерузит",{"lang":335,"names":336},"uk",[337],"гідроцерусит","Q3791946",{"history":11,"applications":11}]