[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:1139":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":15,"ima_formula":14,"elements":16,"sigelements":20,"key_elements":21,"impurities":22,"cim":23,"ima_status":24,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":11,"discovery_year":27,"strunz10ed1":28,"strunz10ed2":29,"strunz10ed3":30,"strunz10ed4":31,"dana8ed1":32,"dana8ed2":33,"dana8ed3":34,"dana8ed4":35,"csystem":36,"cclass":37,"spacegroup":11,"spacegroupset":38,"a":39,"b":40,"c":41,"alpha":38,"beta":38,"gamma":38,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":37,"csmetamict":13,"commentcrystal":42,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":43,"tlform":11,"hmin":44,"hmax":45,"hardtype":11,"vhnmin":38,"vhnmax":38,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":46,"dmeas2":47,"dcalc":48,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":49,"commentluster":11,"diapheny":50,"streak":51,"colour":52,"commentcolor":11,"colors":53,"streak_colors":56,"luminescence":11,"uv":11,"cleavage":57,"cleavagetype":58,"fracturetype":59,"tenacity":11,"commentbreak":11,"opticaltype":11,"opticalsign":11,"opticalalpha":38,"opticalalpha2":38,"opticalalphaerror":11,"opticalbeta":38,"opticalbeta2":38,"opticalbetaerror":11,"opticalgamma":38,"opticalgamma2":38,"opticalgammaerror":11,"opticalomega":38,"opticalomega2":38,"opticalomegaerror":11,"opticalepsilon":38,"opticalepsilon2":38,"opticalepsilonerror":11,"opticaln":38,"opticaln2":38,"opticalnerror":11,"optical2vcalc":38,"optical2vcalc2":38,"optical2vcalcerror":11,"optical2vmeasured":38,"optical2vmeasured2":38,"optical2vmeasurederror":11,"rimin":11,"rimax":11,"opticaldispersion":11,"opticalpleochroism":60,"opticalpleochorismdesc":61,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":62,"opticalinternal":11,"opticaltropic":63,"opticalanisotropism":64,"opticalbireflectance":11,"opticalextinction":11,"opticalr":65,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":11,"otheroccurrence":66,"type_specimen_store":67,"description_short":68,"aboutname":69,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":70,"reviewed_at":11,"variety_of":11,"varieties":71,"group_members":72,"associates":73,"confused_with":110,"type_localities":111,"occurrence_total":118,"citations":119,"images":192,"structures":337,"synonyms":364,"language_names":378,"wikidata_qid":427,"texts":428},1139,"1:1:1139:2","f98ddb9e-7353-432b-9bf8-102ed10bd55c","Cosalite","Cos",0,"mineral",null,2280,false,"Pb\u003Csub>2\u003C\u002Fsub>Bi\u003Csub>2\u003C\u002Fsub>S\u003Csub>5\u003C\u002Fsub>","Always contains minor Cu and nearly always contains minor Ag. Both seem to be essential.",[17,18,19],"Bi","Pb","S",[17,18,19],[17,18],",Cu,Fe,,","5.6.24",[25,26],"APPROVED","GRANDFATHERED","1868","2","J","B","10","3","5","9","1","Orthorhombic",8,"0","19.09","23.87","4.055","Strongly substituted (Cu, Ag, excess Bi) samples have volumes of 1830-1837 Å3 (Topa & Makovicky, 2010).","Prismatic [001]. Frequently elongated to needle-like and capillary forms. Usually massive, also in radiating prismatic, fibrous, or feathery aggregates.",2.5,3,"6.86","6.99","7.12","Metallic","Opaque","Black","Grey",[54,55],"gray","black",[55],"Very rare","Distinct\u002FGood","Irregular\u002FUneven","Weak","Very weak.","White with trace of cream","Anisotropic","Very weak, distinct in oil","(48.2,51.4) 400,\r\n(47.0,50.3) 420,\r\n(45.9,49.5) 440,\r\n(44.9,48.7) 460,\r\n(43.9,47.9) 480,\r\n(43.0,47.1) 500,\r\n(42.2,46.4) 520,\r\n(41.6,45.9) 540,\r\n(41.1,45.5) 560,\r\n(40.8,45.3) 580,\r\n(40.5,45.2) 600,\r\n(40.4,45.2) 620,\r\n(40.2,45.2) 640,\r\n(40.1,45.2) 660,\r\n(40.1,45.2) 680,\r\n(40.0,45.1) 700","Moderate temperature hydrothermal veins, contact metasomatic deposits, epithermal replacements, pegmatites.","n.d.","One of the more common lead-bismuth sulphides, along with galenobismutite.\r\n\r\nAppears to contain Cu and Ag as apparently essential constituents, according to Clark (1993) (\"Hey's Mineral Index\") and Zak et al. (1992) and the detailed study of Topa & Ma...","From the locality at the Cosala Mine, Sinaloa, Mexico.","2026-02-25 13:51:39",[],[],[74,82,91,98,104],{"id":75,"name":76,"entrytype":9,"csystem":77,"ima_formula":78,"mindat_formula":78,"hmin":79,"hmax":79,"dmeas":38,"dcalc":80,"primary_image_id":81},386,"Aschamalmite","Monoclinic","Pb\u003Csub>6-3x\u003C\u002Fsub>Bi\u003Csub>2+x\u003C\u002Fsub>S\u003Csub>9\u003C\u002Fsub>",3.5,"7.33",2154,{"id":83,"name":84,"entrytype":9,"csystem":77,"ima_formula":85,"mindat_formula":86,"hmin":87,"hmax":87,"dmeas":88,"dcalc":89,"primary_image_id":90},883,"Cannizzarite","Pb\u003Csub>8\u003C\u002Fsub>Bi\u003Csub>10\u003C\u002Fsub>S\u003Csub>23\u003C\u002Fsub>","Pb\u003Csub>48\u003C\u002Fsub>Bi\u003Csub>56\u003C\u002Fsub>S\u003Csub>132\u003C\u002Fsub>",2,"6.7","6.95",29359,{"id":92,"name":93,"entrytype":9,"csystem":36,"ima_formula":94,"mindat_formula":94,"hmin":44,"hmax":79,"dmeas":95,"dcalc":96,"primary_image_id":97},1642,"Galenobismutite","PbBi\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>","6.9","7.195",9589,{"id":99,"name":100,"entrytype":9,"csystem":36,"ima_formula":101,"mindat_formula":101,"hmin":79,"hmax":79,"dmeas":38,"dcalc":102,"primary_image_id":103},1782,"Gustavite","AgPbBi\u003Csub>3\u003C\u002Fsub>S\u003Csub>6\u003C\u002Fsub>","7.01",8064,{"id":105,"name":106,"entrytype":9,"csystem":36,"ima_formula":107,"mindat_formula":107,"hmin":87,"hmax":45,"dmeas":108,"dcalc":38,"primary_image_id":109},2400,"Lillianite","Pb\u003Csub>3-2x\u003C\u002Fsub>Ag\u003Csub>x\u003C\u002Fsub>Bi\u003Csub>2+x\u003C\u002Fsub>S\u003Csub>6\u003C\u002Fsub>","7",14508,[],[112],{"id":113,"txt":114,"latitude":115,"longitude":116,"country":117},10357,"Cosalá Mine, Cosalá, Cosalá Municipality, Sinaloa, Mexico",24.4083328,-106.6916656,"Mexico",363,[120,124,128,131,135,139,143,147,151,155,159,164,169,174,178,182,187],{"id":121,"year":122,"html":123,"doi":11},16106641,1868,"Genth, F.A. (1868) Contributions to mineralogy - No. VII. American Journal of Science and Arts: 95: 305-321. (Pp. 319-320).",{"id":125,"year":126,"html":127,"doi":11},16106642,1874,"Lundström (1874) Geol. För. Förh.: 2: 178.",{"id":129,"year":126,"html":130,"doi":11},16106643,"Groth (1874) 18.",{"id":132,"year":133,"html":134,"doi":11},16106644,1878,"Sjögren (1878) Geol. För. Förh.: 4: 107.",{"id":136,"year":137,"html":138,"doi":11},16106645,1884,"Hillebrand, W.F. (1884) On an interesting variety of löllingite and other minerals. American Journal of Science: 27: 343-358.",{"id":140,"year":141,"html":142,"doi":11},16106646,1886,"Flink (1886) Ak. Stockholm, Öfv. Bihang.: 12(2): 2, 6.",{"id":144,"year":145,"html":146,"doi":11},16106647,1910,"Bancroft, Howland (1910) Contributions to economic geology, 1909, Part I, Metals and nonmetals except fuels--Rare Metals: Bulletin 430-D: 151-218 (214).",{"id":148,"year":149,"html":150,"doi":11},16106648,1923,"Bastin, E.S. (1923) Contributions to economic geology, 1922, Part I, Metals and nonmetals except fuels--Silver enrichment in the San Juan Mountains, Colorado: Bulletin 735-D: 65-129.",{"id":152,"year":153,"html":154,"doi":11},16106649,1939,"Berry, L. G. (1939) Studies of mineral sulpho-salts. 1. Cosalite from Canada and Sweden. Univ. Toronto Studies, Geol. Ser., 23, 30.",{"id":156,"year":157,"html":158,"doi":11},1118651,1944,"Palache, Charles, Berman, Harry, Frondel, Clifford (1944) \u003Ci>The System of Mineralogy\u003C\u002Fi> (7th ed.) Vol. 1 - Elements, Sulfides, Sulfosalts, Oxides. John Wiley and Sons, New York.",{"id":160,"year":161,"html":162,"doi":163},106436,1960,"Weitz, G., Hellner, E. (1960) Über komplex zusammengesetzte sulfidische Erze VII. Zur Kristallstruktur des Cosalits, Pb2Bi2S5. \u003Ci>Zeitschrift für Kristallographie\u003C\u002Fi>,  113 (1) 385-402 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1960.113.1-6.385'>doi:10.1524\u002Fzkri.1960.113.1-6.385\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fzk\u002Fvol113\u002FZK113_385.pdf' class='refpdflink'>\u003C\u002Fa>","10.1524\u002Fzkri.1960.113.1-6.385",{"id":165,"year":166,"html":167,"doi":168},16596174,1969,"Ramdohr, Paul (1969) \u003Ci>The Ore Minerals and their Intergrowths\u003C\u002Fi>. Pergamon Press, Oxford. 1174pp. \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1016\u002Fc2013-0-10027-x'>doi:10.1016\u002Fc2013-0-10027-x\u003C\u002Fa>","10.1016\u002Fc2013-0-10027-x",{"id":170,"year":171,"html":172,"doi":173},108788,1974,"Srikrishnan, T.; Nowacki, Werner (1974) A redetermination of the crystal structure of cosalite, Pb\u003Csub>2\u003C\u002Fsub>Bi\u003Csub>2\u003C\u002Fsub>S\u003Csub>5\u003C\u002Fsub>. \u003Ci>Zeitschrift für Kristallographie\u003C\u002Fi>,  140 (1-2). 114-136 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri-1974-1-209'>doi:10.1524\u002Fzkri-1974-1-209\u003C\u002Fa>","10.1524\u002Fzkri-1974-1-209",{"id":175,"year":176,"html":177,"doi":11},17057143,1992,"Zak, L., Megarskaya, L., Mumme, W. G. (1992) Rezbanyite from Ocna de fier (Vasko): a mixture of bismuthinite derivatives and cosalite. \u003Ci>Neues Jahrbuch für Mineralogie - Monatshefte\u003C\u002Fi>,  1992. 69-79",{"id":179,"year":180,"html":181,"doi":11},16963811,2005,"(2005) Cosalite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fcosalite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":183,"year":184,"html":185,"doi":186},64804,2010,"Topa, D.; Makovicky, E. (2010) The crystal chemistry of cosalite based on new electron-microprobe data and single-crystal determinations of the structure. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  48 (5). 1081-1107 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3749\u002Fcanmin.48.5.1081'>doi:10.3749\u002Fcanmin.48.5.1081\u003C\u002Fa>","10.3749\u002Fcanmin.48.5.1081",{"id":188,"year":189,"html":190,"doi":191},65590,2019,"Kovač, Sabina, Dabić, Predrag, Kremenović, Aleksandar, Pačevski, Aleksandar, Karanović, Ljiiljana, Rodić, Marko V., Tribus, Martina (2019) Polyhedral characteristics of the cosalite-type crystal structures. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  57 (5) 647-662 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3749\u002Fcanmin.1900017'>doi:10.3749\u002Fcanmin.1900017\u003C\u002Fa>","10.3749\u002Fcanmin.1900017",[193,203,210,220,228,238,246,252,258,264,270,279,286,294,301,307,313,319,325,331],{"id":194,"source_url":195,"license_code":196,"credit_html":197,"title":198,"description":199,"author":200,"original_width":201,"original_height":202},6359,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=6331891","CC BY-SA 3.0","Ra'ike (Wikipedia), via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=6331891\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cosalit - Willroth, Westerwald.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCosalite\" class=\"extiw\" title=\"en:Cosalite\">Cosalite\u003C\u002Fa> - Locality: Georg Mine near Willroth, Westerwald - Exposed in the Mineralogical Museum, Bonn, Germany","Ra'ike (Wikipedia)",1600,1300,{"id":204,"source_url":205,"license_code":206,"credit_html":207,"title":7,"description":11,"author":11,"original_width":208,"original_height":209},29540,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F119355","CC BY 4.0","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F119355\" rel=\"noopener\">Department of Geology, TalTech\u003C\u002Fa> via Europeana",1000,666,{"id":211,"source_url":212,"license_code":213,"credit_html":214,"title":215,"description":216,"author":217,"original_width":218,"original_height":219},6364,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118194269","CC BY-SA 2.0","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118194269\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cosalite (48904895192).jpg","\u003Cp>Lime Creek Mine, Alice Arm\n\u003C\u002Fp>\nB.C., Canada","Pacific Museum of Earth from Canada",3838,5889,{"id":221,"source_url":222,"license_code":213,"credit_html":223,"title":224,"description":225,"author":217,"original_width":226,"original_height":227},50890,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118193846","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118193846\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cosalite (49024755468).jpg","\u003Cp>Comet Vale, Coolgardie\n\u003C\u002Fp>\nWestern Australia, Australia",4000,6000,{"id":229,"source_url":230,"license_code":231,"credit_html":232,"title":233,"description":234,"author":235,"original_width":236,"original_height":237},6365,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163482155","CC0 1.0","Nessa Eull, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163482155\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cosalite (GeoDIL number - 1162).jpg","The dark gray material is cosalite, Pb2Bi2S5, a mineral consisting of lead, bismuth, and sulfur. Here it is seem with salmon colored calcite. Cosalite is found in many places, but generally in very small amounts. This specimen is 4.5 cm tall.","Nessa Eull",1577,1585,{"id":239,"source_url":240,"license_code":231,"credit_html":241,"title":242,"description":243,"author":235,"original_width":244,"original_height":245},6366,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163482171","Nessa Eull, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163482171\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cosalite (GeoDIL number - 1164).jpg","The dark gray material is cosalite, Pb2Bi2S5, a mineral consisting of lead, bismuth, and sulfur. (The white on top is a label.) Cosalite is found in many places, often associated with hydrothermal ore deposits, but generally in very small amounts. This specimen is 3.5 cm long.",1469,1489,{"id":247,"source_url":248,"license_code":213,"credit_html":249,"title":250,"description":251,"author":217,"original_width":227,"original_height":226},50892,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118205702","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118205702\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cosalite (46995654255).jpg","\u003Cp>McElroy Township\nOntario, Canada\n\u003C\u002Fp>\nS-74-1988",{"id":253,"source_url":254,"license_code":213,"credit_html":255,"title":256,"description":257,"author":217,"original_width":227,"original_height":226},50893,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118205707","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118205707\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cosalite (46995654495).jpg","\u003Cp>Cariboo Gold Quartz Mine\nBritish Columbia, Canada\n\u003C\u002Fp>\nS-74-1987",{"id":259,"source_url":260,"license_code":213,"credit_html":261,"title":262,"description":263,"author":217,"original_width":227,"original_height":226},50894,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118205710","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118205710\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cosalite (46995654655).jpg","\u003Cp>Alice Arm\nBritish Columbia, Canada\n\u003C\u002Fp>\nS-74-1986",{"id":265,"source_url":266,"license_code":213,"credit_html":267,"title":268,"description":269,"author":217,"original_width":227,"original_height":226},50896,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118205739","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118205739\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cosalite (40945005883).jpg","\u003Cp>Boliden Mine\nNorth Sweden\n\u003C\u002Fp>\nS-74-1982",{"id":271,"source_url":272,"license_code":196,"credit_html":273,"title":274,"description":275,"author":276,"original_width":277,"original_height":278},6360,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10149982","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10149982\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cosalite-Fluorite-171717.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCosalite\" class=\"extiw\" title=\"en:Cosalite\">Cosalite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FFluorite\" class=\"extiw\" title=\"en:Fluorite\">Fluorite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Kara-Oba W deposit, Betpakdala Desert (Bet-Pak-Dal Desert), Qaraghandy Oblysy (Karaganda Oblast'), Kazakhstan (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2222.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 4.5 x 4.0 x 2.7 cm.\u003C\u002Fdd>\n\u003Cdd>A RARE and showy combination specimen from Kara-Oba, Kazakhstan and the Eric Asselborn Collection. Metalllic-bright cosalite needles are aesthetically crossed and included within a water-clear, sea-green fluorite cube with purple zoning. The cosalite needles are revealed through a thin, secondary fluorite overgrowth layer. Cosalite is an uncommon lead bismuth sulfide. The scattering of quartz crystals are a nice accent to this mounded, 3-dimensional piece.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Robert M. Lavinsky",550,503,{"id":280,"source_url":281,"license_code":196,"credit_html":282,"title":283,"description":275,"author":276,"original_width":284,"original_height":285},6361,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10149983","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10149983\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cosalite-Fluorite-171718.jpg",375,317,{"id":287,"source_url":288,"license_code":196,"credit_html":289,"title":290,"description":291,"author":276,"original_width":292,"original_height":293},6362,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10164876","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10164876\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cosalite-Quartz-237633.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCosalite\" class=\"extiw\" title=\"en:Cosalite\">Cosalite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FQuartz\" class=\"extiw\" title=\"en:Quartz\">Quartz\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Kara-Oba W deposit, Betpakdala Desert (Bet-Pak-Dal Desert), Qaraghandy Oblysy (Karaganda Oblast'), Kazakhstan (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2222.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 4.0 x 2.1 x 2.1 cm.\u003C\u002Fdd>\n\u003Cdd>A rich nest of cosalite needles is visible within a stocky, water-clear quartz crystal in this fine specimen from the Kara-Oba deposit of Kazakhstan. Cosalite is an uncommon lead, bismuth sulfosalt and this is a superb and very uncommon combination of the two species. A fine, 2.0 cm, doubly terminated quartz crystal is embedded in one side. The quartz crystal is complete-all-around and nearly pristine.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",382,600,{"id":295,"source_url":296,"license_code":196,"credit_html":297,"title":298,"description":291,"author":276,"original_width":299,"original_height":300},6363,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10164877","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10164877\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cosalite-Quartz-237634.jpg",354,400,{"id":302,"source_url":303,"license_code":213,"credit_html":304,"title":305,"description":306,"author":217,"original_width":227,"original_height":226},50891,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118198542","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118198542\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cosalite with Quartz (48603360207).jpg","\u003Cp>Cariboo Gold Quartz Mine - Wells\n\u003C\u002Fp>\nBritish Columbia, Canada",{"id":308,"source_url":309,"license_code":213,"credit_html":310,"title":311,"description":312,"author":217,"original_width":227,"original_height":226},9592,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118205539","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118205539\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Galenobismutite with Cosalite and Gold (46995644805).jpg","\u003Cp>Wells\nBritish Columbia, Canada\n\u003C\u002Fp>\nS-74-2021",{"id":314,"source_url":315,"license_code":213,"credit_html":316,"title":317,"description":318,"author":217,"original_width":227,"original_height":226},50895,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118205721","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118205721\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cosalite with Native Bismuth (40945005273).jpg","\u003Cp>Salmo\nBritish Columbia, Canada\n\u003C\u002Fp>\nS-74-1985",{"id":320,"source_url":321,"license_code":213,"credit_html":322,"title":323,"description":324,"author":217,"original_width":227,"original_height":226},9594,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118205722","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118205722\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cosalite with Pyrite, Galena, Quartz, and Galenobismutite (46995655085).jpg","\u003Cp>Cariboo Gold Quartz Mine\nBritish Columbia, Canada\n\u003C\u002Fp>\nS-74-1984",{"id":326,"source_url":327,"license_code":213,"credit_html":328,"title":329,"description":330,"author":217,"original_width":227,"original_height":226},50897,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118205755","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118205755\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cosalite with Gold in Quartz (46995655935).jpg","\u003Cp>Wells\nBritish Columbia, Canada\n\u003C\u002Fp>\nS-74-1979",{"id":332,"source_url":333,"license_code":213,"credit_html":334,"title":335,"description":336,"author":217,"original_width":226,"original_height":227},9595,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118206756","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118206756\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Pyrite with Cosalite, Gold, and Galenobismutite (47859659382).jpg","\u003Cp>Wells\nBritish Columbia, Canada\n\u003C\u002Fp>\nS-74-1672",[338,344,349,354,359],{"id":339,"url":340,"label":341,"formula":342,"spacegroup":343,"year":184},3268,"\u002Fcif\u002F3268.cif","Topa 2010 · Bi4 Pb3.904 Ag.014 Cu.132 S10","Bi4 Pb3.904 Ag.014 Cu.132 S10","P n m a",{"id":345,"url":346,"label":347,"formula":348,"spacegroup":343,"year":184},3269,"\u002Fcif\u002F3269.cif","Topa 2010 · Bi4 Pb3.867 Cu.26 S10","Bi4 Pb3.867 Cu.26 S10",{"id":350,"url":351,"label":352,"formula":353,"spacegroup":343,"year":184},3270,"\u002Fcif\u002F3270.cif","Topa 2010 · Bi3.875 Sb.447 Pb3.32 Ag.331 Cu.203 S10","Bi3.875 Sb.447 Pb3.32 Ag.331 Cu.203 S10",{"id":355,"url":356,"label":357,"formula":358,"spacegroup":343,"year":184},3271,"\u002Fcif\u002F3271.cif","Topa 2010 · Bi4 Pb3.695 Cu.73 S10","Bi4 Pb3.695 Cu.73 S10",{"id":360,"url":361,"label":362,"formula":363,"spacegroup":343,"year":184},3272,"\u002Fcif\u002F3272.cif","Topa 2010 · Bi4 Pb3.643 Ag.308 Cu.358 S10","Bi4 Pb3.643 Ag.308 Cu.358 S10",[365,366,367,368,369,370,371,372,373,374,375,376,377],"Bjelkeit","Bjelkit","Bjelkite","Bjelkitea","Bleibismutit","Bleibismutita","Cosaliet","Cuprocosalit","Cuprocosalita","Cuprocosalite","Retzbanyite (of Hermann)","Rezbanyite (of Hermann)","Vismutsvafladt Svafvelbly",[379,383,387,391,395,400,404,408,412,416,419,423],{"lang":380,"names":381},"az",[382],"Kozalit",{"lang":384,"names":385},"ca",[386],"cosalita",{"lang":388,"names":389},"de",[390],"Cosalit",{"lang":392,"names":393},"et",[394],"kosaliit",{"lang":396,"names":397},"eu",[398,399],"Cosalita","Kosalita",{"lang":401,"names":402},"fa",[403],"کوزالیت",{"lang":405,"names":406},"it",[407],"cosalite",{"lang":409,"names":410},"nb",[411],"cosalitt",{"lang":413,"names":414},"nn",[415],"Cosalitt",{"lang":417,"names":418},"pl",[390],{"lang":420,"names":421},"ru",[422],"Козалит",{"lang":424,"names":425},"uk",[426],"Косаліт","Q1135968",{"history":11,"applications":11}]