[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:1746":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":15,"elements":16,"sigelements":19,"key_elements":20,"impurities":21,"cim":22,"ima_status":23,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":11,"discovery_year":26,"strunz10ed1":27,"strunz10ed2":28,"strunz10ed3":29,"strunz10ed4":30,"dana8ed1":27,"dana8ed2":31,"dana8ed3":32,"dana8ed4":27,"csystem":33,"cclass":34,"spacegroup":35,"spacegroupset":36,"a":37,"b":36,"c":38,"alpha":36,"beta":36,"gamma":36,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":39,"csmetamict":14,"commentcrystal":11,"twinning":40,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":41,"tlform":11,"hmin":42,"hmax":43,"hardtype":42,"vhnmin":44,"vhnmax":36,"vhnerror":11,"vhng":45,"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":57,"luminescence":11,"uv":11,"cleavage":58,"cleavagetype":59,"fracturetype":60,"tenacity":61,"commentbreak":11,"opticaltype":62,"opticalsign":63,"opticalalpha":36,"opticalalpha2":36,"opticalalphaerror":11,"opticalbeta":36,"opticalbeta2":36,"opticalbetaerror":11,"opticalgamma":36,"opticalgamma2":36,"opticalgammaerror":11,"opticalomega":64,"opticalomega2":36,"opticalomegaerror":11,"opticalepsilon":65,"opticalepsilon2":36,"opticalepsilonerror":11,"opticaln":36,"opticaln2":36,"opticalnerror":11,"optical2vcalc":36,"optical2vcalc2":36,"optical2vcalcerror":11,"optical2vmeasured":36,"optical2vmeasured2":36,"optical2vmeasurederror":11,"rimin":66,"rimax":67,"opticaldispersion":11,"opticalpleochroism":68,"opticalpleochorismdesc":11,"opticalbirefringence":11,"opticalcomments":69,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":11,"opticalr":11,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":11,"otheroccurrence":70,"type_specimen_store":11,"description_short":71,"aboutname":72,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":73,"reviewed_at":11,"variety_of":11,"varieties":74,"group_members":79,"associates":106,"confused_with":135,"type_localities":142,"occurrence_total":149,"citations":150,"images":269,"structures":441,"synonyms":456,"language_names":459,"wikidata_qid":544,"texts":545},1746,"1:1:1746:2","bcd35f10-2885-4605-b9f9-0ba9f58c86ae","Greenockite","Gnk",0,"mineral",null,10922,5207,false,"CdS",[17,18],"Cd","S",[17,18],[17],",Zn,,","3.4.7",[24,25],"APPROVED","GRANDFATHERED","1840","2","C","B","45","8","7","Hexagonal",18,114,"0","4.136","6.713",2,"Twin plane \u003Cmi>{11_22}\u003C\u002Fmi> rare forming trillings.","Crystals hemimorphic pyramidal. Earthy coatings (sphalerite)",3,3.5,"98",25,"4.8","4.9","4.824","Adamantine,Resinous","Translucent","Orange-yellow to brick red.","Yellow to red.",[54,55,56],"yellow","red","orange",[56,54,55],"Distinct on \u003Cmi>{11_22}\u003C\u002Fmi>, imperfect on {0001}.","Distinct\u002FGood","Conchoidal","brittle","Uniaxial","-","2.529","2.506",2.506,2.529,"Weak","Uniaxial + for wavelengths red to blue-green","An uncommon mineral of sulfide deposits.","Typically found as yellow to red hemimorphic pyramidal crystals and earthy coatings. Caution should be used in sight identifying yellow cadmium sulfide coatings as hawleyite (dimorph of greenockite) is not a very rare species and occurs in identical ap...","The naming of the mineral is often attributed to Henry James Brooke and Arthur Connell in 1840. The original description was actually made by Robert Jameson who first described greenockite, and the first description was in “his journal”: The Edinburgh New Philosophical Journal. The mineral was named for Lord Greenock - later Earl Charles Murray Cathcart, 2nd Earl Cathcart [December 21, 1783, Walton-on-the-Naze, Essex, England, UK - July 16, 1859, St Leonards-on-Sea, Hastings, England, UK]. Earl Charles Murray Cathcart was a general in the British army and served as Governor of the Province of Canada. He was also the author of two papers: one on igneous rocks in Edinburgh, Scotland and one on coal in southern Scotland.","2026-03-30 14:26:52",[75],{"id":76,"name":77,"entrytype":39,"csystem":11,"ima_formula":11,"mindat_formula":78,"hmin":11,"hmax":11,"dmeas":36,"dcalc":11,"primary_image_id":11},11026,"Zinc-bearing Greenockite","(Cd,Zn)S",[80,85,93,98],{"id":81,"name":82,"entrytype":9,"csystem":33,"ima_formula":83,"mindat_formula":83,"hmin":11,"hmax":11,"dmeas":11,"dcalc":84,"primary_image_id":11},42371,"Buseckite","(Fe,Zn,Mn)S","3.697",{"id":86,"name":87,"entrytype":9,"csystem":33,"ima_formula":88,"mindat_formula":88,"hmin":89,"hmax":89,"dmeas":90,"dcalc":91,"primary_image_id":92},844,"Cadmoselite","CdSe",4,"5.47","5.807",4295,{"id":94,"name":95,"entrytype":9,"csystem":33,"ima_formula":96,"mindat_formula":96,"hmin":89,"hmax":89,"dmeas":36,"dcalc":36,"primary_image_id":97},7268,"Rambergite","MnS",20505,{"id":99,"name":100,"entrytype":9,"csystem":33,"ima_formula":101,"mindat_formula":102,"hmin":43,"hmax":89,"dmeas":103,"dcalc":104,"primary_image_id":105},4318,"Wurtzite","ZnS","(Zn,Fe)S","4","4.09",31000,[107,118,128],{"id":108,"name":109,"entrytype":9,"csystem":110,"ima_formula":111,"mindat_formula":112,"hmin":113,"hmax":114,"dmeas":115,"dcalc":116,"primary_image_id":117},3277,"Prehnite","Orthorhombic","Ca\u003Csub>2\u003C\u002Fsub>Al(Si\u003Csub>3\u003C\u002Fsub>Al)O\u003Csub>10\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>","Ca\u003Csub>2\u003C\u002Fsub>Al\u003Csub>2\u003C\u002Fsub>Si\u003Csub>3\u003C\u002Fsub>O\u003Csub>10\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>",6,6.5,"2.8","2.9",19927,{"id":119,"name":120,"entrytype":9,"csystem":121,"ima_formula":122,"mindat_formula":123,"hmin":89,"hmax":124,"dmeas":125,"dcalc":126,"primary_image_id":127},3688,"Smithsonite","Trigonal","Zn(CO\u003Csub>3\u003C\u002Fsub>)","ZnCO\u003Csub>3\u003C\u002Fsub>",4.5,"4.42","4.43",30707,{"id":129,"name":130,"entrytype":9,"csystem":131,"ima_formula":101,"mindat_formula":101,"hmin":43,"hmax":89,"dmeas":132,"dcalc":133,"primary_image_id":134},3727,"Sphalerite","Isometric","3.9","4.096",66200,[136],{"id":137,"name":138,"entrytype":9,"csystem":131,"ima_formula":15,"mindat_formula":15,"hmin":139,"hmax":42,"dmeas":36,"dcalc":140,"primary_image_id":141},1834,"Hawleyite",2.5,"4.87",10955,[143],{"id":144,"txt":145,"latitude":146,"longitude":147,"country":148},3003,"Bishopton tunnel, Bishopton, Renfrewshire, Scotland, UK",55.9154529,-4.5147854,"UK",754,[151,156,160,163,166,170,174,178,183,187,192,196,200,203,207,211,215,219,224,229,233,237,241,246,251,256,261,265],{"id":152,"year":153,"html":154,"doi":155},4458777,1840,"Brooke, J.; Connell, A. (1840) Der Greenockit, ein neues Mineral. \u003Ci>Annalen der Physik\u003C\u002Fi>,  127 (10). 274-275 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1002\u002Fandp.18401271008'>doi:10.1002\u002Fandp.18401271008\u003C\u002Fa>","10.1002\u002Fandp.18401271008",{"id":157,"year":153,"html":158,"doi":159},4458810,"Breithaupt, A. (1840) Greenockit, ein neues Mineral. \u003Ci>Annalen der Physik und Chemie\u003C\u002Fi>, 127. 507-510 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1002\u002Fandp.18401271205'>doi:10.1002\u002Fandp.18401271205\u003C\u002Fa>","10.1002\u002Fandp.18401271205",{"id":161,"year":153,"html":162,"doi":11},16110864,"Connell, A. (1840) On Sulphuret of Cadmium, or Greenockite, a new Mineral. Earth and Environmental Science Transactions of The Royal Society of Edinburgh: 14(2): 619-623.",{"id":164,"year":153,"html":165,"doi":11},16110865,"Thompson, T. (1840) Notice of greenockite, a new mineral species of the order blende. The Edinburgh New Philosophical Journal: 28: 390-292.",{"id":167,"year":168,"html":169,"doi":11},16110866,1845,"Brewster, D. (1845) On the Optical Properties of Greenockite, by Sir David Brewster, in a letter to Lord Greenock. Proceedings of the Royal Society of Edinburgh: 1: 342-342.",{"id":171,"year":172,"html":173,"doi":11},16110867,1887,"Heddle, M.F. (1887) On the Occurrence of Greenockite at a New Locality. The Mineralogical Magazine and Journal of the Mineralogical Society: 7: 133-137.",{"id":175,"year":176,"html":177,"doi":11},16110868,1902,"Cornwall, H.B. (1902) Occurrence of Greenockite on Calcite from Joplin. Missouri. American Journal of Science: 14(79): 7.",{"id":179,"year":180,"html":181,"doi":182},103768,1925,"Ulrich, F.; Zachariasen, W. (1925) Über die Kristallstruktur des α- und ß-CdS, sowie des Wurtzits. \u003Ci>Zeitschrift für Kristallographie\u003C\u002Fi>,  62 (1-6). 260-273 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1925.62.1.260'>doi:10.1524\u002Fzkri.1925.62.1.260\u003C\u002Fa>","10.1524\u002Fzkri.1925.62.1.260",{"id":184,"year":185,"html":186,"doi":11},16110869,1929,"Whitlock, H.P. (1929) A crystallographic note on greenockite from West Paterson, New Jersey. American Museum novitates; no. 372.",{"id":188,"year":189,"html":190,"doi":191},2245424,1939,"KINGSBURY, ARTHUR W. G., FRIEND, J. NEWTON (1939) Occurrence of Greenockite in the Mendips. \u003Ci>Nature\u003C\u002Fi>, 144 (3659) 1013 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1038\u002F1441013a0'>doi:10.1038\u002F1441013a0\u003C\u002Fa>","10.1038\u002F1441013a0",{"id":193,"year":194,"html":195,"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":197,"year":198,"html":199,"doi":11},522100,1951,"Ahlfeld, Frederico (1951) A new locality for greenockite crystals in Bolivia. \u003Ci>American Mineralogist\u003C\u002Fi>,  36 (1-2) 165-166 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM36\u002FAM36_165.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":201,"year":198,"html":202,"doi":11},522141,"Harwood, H. F. (1951) The greenockite locality at Bishopton, Scotland. \u003Ci>American Mineralogist\u003C\u002Fi>,  36 (7-8) 630 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM36\u002FAM36_630.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":204,"year":205,"html":206,"doi":11},522894,1957,"Hurlbut, Cornelius S. (1957) The wurtzite-greenockite series. \u003Ci>American Mineralogist\u003C\u002Fi>,  42 (3-4) 184-190 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM42\u002FAM42_184.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":208,"year":209,"html":210,"doi":11},523624,1961,"Skinner, B.J., Bethke, P. M. (1961) The relationship between unit-cell edges and composition of synthetic wurtzites. \u003Ci>American Mineralogist\u003C\u002Fi>,  46 (11-12) 1382-1398 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM46\u002FAM46_1382.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":212,"year":213,"html":214,"doi":11},16110876,1963,"Wyckoff, R.W.G. (1963) Greenockite cell parameters. Crystal Structures: 1: 85-237.",{"id":216,"year":217,"html":218,"doi":11},15955499,1985,"Patterson, D.J. (1985) Zincian greenockite in stratiform lead-zinc-silver mineralization at Lady Loretta, northwest Queensland. The Canadian Mineralogist: 23: 89-94.",{"id":220,"year":221,"html":222,"doi":223},15775,1989,"Tarkian, M., Breskovska, V. (1989) Greenockite from the Madjarovo Pb-Zn Ore District, Eastern Rhodope, Bulgaria. \u003Ci>Mineralogy and Petrology\u003C\u002Fi>,  40 (2) 137-144 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fbf01164324'>doi:10.1007\u002Fbf01164324\u003C\u002Fa>","10.1007\u002Fbf01164324",{"id":225,"year":226,"html":227,"doi":228},14121560,1993,"Xu, Yong-Nian, Ching, W. Y. (1993) Electronic, optical, and structural properties of some wurtzite crystals. \u003Ci>Physical Review B\u003C\u002Fi>, 48 (7) 4335-4351 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1103\u002Fphysrevb.48.4335'>doi:10.1103\u002Fphysrevb.48.4335\u003C\u002Fa>","10.1103\u002Fphysrevb.48.4335",{"id":230,"year":231,"html":232,"doi":11},1118654,1997,"Gaines, Richard V.; Skinner, H. Catherine W.; Foord, Eugene E.; Mason, Brian; Rosenzweig, Abraham; King, Vandall T. (1997) \u003Ci>Dana's New Mineralogy\u003C\u002Fi> (8th ed.). Wiley-Interscience. 1872 pp.",{"id":234,"year":235,"html":236,"doi":11},16110880,2004,"Tiegeng, L., Qian, Z., Lin, Y., Shuxun, S. (2004) Discovery of primary greenockite in nature, as exemplified by the Niujiaotang cadmium zinc deposit, Guizhou. Acta Mineralogica Sinica: 2: 191-196.",{"id":238,"year":239,"html":240,"doi":11},16964657,2005,"(2005) Greenockite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fgreenockite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":242,"year":243,"html":244,"doi":245},395476,2006,"Deore, S., Navrotsky, A. (2006) Oxide melt solution calorimetry of sulfides: Enthalpy of formation of sphalerite, galena, greenockite, and hawleyite. \u003Ci>American Mineralogist\u003C\u002Fi>,  91 (2) 400-403 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam.2006.1921'>doi:10.2138\u002Fam.2006.1921\u003C\u002Fa>","10.2138\u002Fam.2006.1921",{"id":247,"year":248,"html":249,"doi":250},244483,2014,"Parnell, J., Still, J., Spinks, S., Thayalan, W., Bowden, S. (2014) Cadmium sulfide in a Mesoproterozoic terrestrial environment. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  78 (1) 47-54 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.2014.078.1.04'>doi:10.1180\u002Fminmag.2014.078.1.04\u003C\u002Fa>","10.1180\u002Fminmag.2014.078.1.04",{"id":252,"year":253,"html":254,"doi":255},16110883,2016,"Mishra, Biswajit, Hazarika, Pranjit (2016) Rare greenockite (CdS) within the chromite–PGE association in the Bangur Gabbro, Baula-Nuasahi Complex, Eastern India. \u003Ci>Ore Geology Reviews\u003C\u002Fi>,  72. 1327-1334 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.oregeorev.2015.04.006'>doi:10.1016\u002Fj.oregeorev.2015.04.006\u003C\u002Fa>","10.1016\u002Fj.oregeorev.2015.04.006",{"id":257,"year":258,"html":259,"doi":260},7734759,2017,"Liu, Jianping; Zhang, Shugen (2017) A New Zincian Greenockite Occurrence in the Saishitang Cu Skarn Deposit, Qinghai Province, Northwest China. \u003Ci>Minerals\u003C\u002Fi>,  7 (8). 132 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3390\u002Fmin7080132'>doi:10.3390\u002Fmin7080132\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fwww.mdpi.com\u002F2075-163X\u002F7\u002F8\u002F132\u002Fpdf?version=1501244376' class='refpdflink'>\u003C\u002Fa>","10.3390\u002Fmin7080132",{"id":262,"year":263,"html":264,"doi":11},16110885,2020,"Pelckmans, H. (2020) On the History of Greenockite. Mineral News: 36(10): 2.",{"id":266,"year":263,"html":267,"doi":268},13423350,"Nowak, Katarzyna, Galuskina, Irina, Galuskin, Evgeny (2020) Greenockite Whiskers from the Bytom Burned Coal Dump, Upper Silesia, Poland. \u003Ci>Minerals\u003C\u002Fi>, 10 (5) 470 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3390\u002Fmin10050470'>doi:10.3390\u002Fmin10050470\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fwww.mdpi.com\u002F2075-163X\u002F10\u002F5\u002F470\u002Fpdf?version=1590148744' class='refpdflink'>\u003C\u002Fa>","10.3390\u002Fmin10050470",[270,277,287,294,303,313,321,331,339,348,356,363,370,377,385,391,398,405,411,417,423,432],{"id":271,"source_url":272,"license_code":273,"credit_html":274,"title":7,"description":11,"author":11,"original_width":275,"original_height":276},29813,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F198099","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\u002F198099\" rel=\"noopener\">University of Tartu, Natural History Museum\u003C\u002Fa> via Europeana",1000,967,{"id":278,"source_url":279,"license_code":280,"credit_html":281,"title":282,"description":283,"author":284,"original_width":285,"original_height":286},10426,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10464203","CC BY-SA 3.0","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10464203\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Greenockite-t06-119a.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGreenockite\" class=\"extiw\" title=\"en:Greenockite\">Greenockite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Andesite quarry, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FKreimbach-Kaulbach\" class=\"extiw\" title=\"en:Kreimbach-Kaulbach\">Kreimbach-Kaulbach\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FWolfstein\" class=\"extiw\" title=\"en:Wolfstein\">Wolfstein\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FRhineland-Palatinate\" class=\"extiw\" title=\"en:Rhineland-Palatinate\">Rhineland-Palatinate\u003C\u002Fa>, Germany (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-14808.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: small cabinet, 8.9 x 6 x 4 cm\n\u003Cdl>\u003Cdt>Greenockite\u003C\u002Fdt>\u003C\u002Fdl>\u003C\u002Fdd>\n\u003Cdd>A 7 x 7 x 5 mm MATRIX greenockite from a remarkable , small find that has produced what many consider to be the bets of the species for this rarity. I had never seen such a good matrix piece for sale! This crystal is gemmy and bright, and perched nicely on matrix with calcite, prehnite, laumontite, and other minerals. It is spectacular for the species. Ex. Gerald Herfurth Collection (and he paid about the same a decade ago so this is being recycled without accounting for appreciation). Is it expensive? surely. but it is a thing of such rarity that it is impossible to replace at any price.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Robert M. Lavinsky",600,477,{"id":288,"source_url":289,"license_code":280,"credit_html":290,"title":291,"description":283,"author":284,"original_width":292,"original_height":293},10427,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10464205","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10464205\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Greenockite-t06-119b.jpg",400,324,{"id":295,"source_url":296,"license_code":280,"credit_html":297,"title":298,"description":299,"author":300,"original_width":301,"original_height":302},10428,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14865879","Christian Rewitzer, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14865879\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Greenockite-259580.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGreenockite\" class=\"extiw\" title=\"en:Greenockite\">Greenockite\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>Picture width 1 mm. Collection and photograph Christian Rewitzer\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Christian Rewitzer",985,1024,{"id":304,"source_url":305,"license_code":306,"credit_html":307,"title":308,"description":309,"author":310,"original_width":311,"original_height":312},10429,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=96151200","CC BY 2.0","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=96151200\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Greenockite (Nevada, USA).jpg","Greenockite from Nevada, USA. (public display, Montana Bureau of Mines and Geology Mineral Museum, Butte, Montana, USA)\n\u003Cp>A mineral is a naturally-occurring, solid, inorganic, crystalline substance having a fairly definite chemical composition and having fairly definite physical properties.  At its simplest, a mineral is a naturally-occurring solid chemical.  Currently, there are over 4900 named and described minerals - about 200 of them are common and about 20 of them are very common.  Mineral classification is based on anion chemistry.  Major categories of minerals are: elements, sulfides, oxides, halides, carbonates, sulfates, phosphates, and silicates.\n\u003C\u002Fp>\u003Cp>The sulfide minerals contain one or more sulfide anions (S-2).  The sulfides are usually considered together with the arsenide minerals, the sulfarsenide minerals, and the telluride minerals.  Many sulfides are economically significant, as they occur commonly in ores.  The metals that combine with S-2 are mainly Fe, Cu, Ni, Ag, etc.  Most sulfides have a metallic luster, are moderately soft, and are noticeably heavy for their size.  These minerals will not form in the presence of free oxygen.  Under an oxygen-rich atmosphere, sulfide minerals tend to chemically weather to various oxide and hydroxide minerals.\n\u003C\u002Fp>\u003Cp>Greenockite is a scarce cadium sulfide mineral, CdS.  It has a nonmetallic luster, a yellow to red color, an orangish-yellowish to maroon streak, and is somewhat soft (H = 3 to 3.5).  It can occur as discrete crystals or as earthy, powdery coatings.\n\u003C\u002Fp>\u003Cp>In the mining districts of America's Mississippi Valley, sphalerite weathers into bright yellow powder in the supergene zone (= above the water table) - the powder can be a mix of metal sulfides that includes cadmium (for example (Zn,Fe,Cd)S).\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>Photo gallery of greenockite:\n\u003C\u002Fp>\nwww.mindat.org\u002Fgallery.php?min=1746","James St. John",1819,926,{"id":314,"source_url":315,"license_code":306,"credit_html":316,"title":317,"description":318,"author":310,"original_width":319,"original_height":320},10430,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=129024001","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=129024001\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Greenockite (Arkansas, USA) 1.jpg","Greenockite from Arkansas, USA. (public display, Carnegie Museum of Natural History, Pittsburgh, Pennsylvania, USA)\n\u003Cp>A mineral is a naturally-occurring, solid, inorganic, crystalline substance having a fairly definite chemical composition and having fairly definite physical properties.  At its simplest, a mineral is a naturally-occurring solid chemical.  Currently, there are over 5800 named and described minerals - about 200 of them are common and about 20 of them are very common.  Mineral classification is based on anion chemistry.  Major categories of minerals are: elements, sulfides, oxides, halides, carbonates, sulfates, phosphates, and silicates.\n\u003C\u002Fp>\u003Cp>The sulfide minerals contain one or more sulfide anions (S-2).  The sulfides are usually considered together with the arsenide minerals, the sulfarsenide minerals, and the telluride minerals.  Many sulfides are economically significant, as they occur commonly in ores.  The metals that combine with S-2 are mainly Fe, Cu, Ni, Ag, etc.  Most sulfides have a metallic luster, are moderately soft, and are noticeably heavy for their size.  These minerals will not form in the presence of free oxygen.  Under an oxygen-rich atmosphere, sulfide minerals tend to chemically weather to various oxide and hydroxide minerals.\n\u003C\u002Fp>\u003Cp>Greenockite is a scarce cadium sulfide mineral, CdS.  It has a nonmetallic luster, a yellow to red color, an orangish-yellowish to maroon streak, and is somewhat soft (H = 3 to 3.5).  It can occur as discrete crystals or as earthy, powdery coatings.\n\u003C\u002Fp>\u003Cp>In the mining districts of America's Mississippi Valley, sphalerite weathers into bright yellow powder in the supergene zone (= above the water table) - the powder can be a mix of metal sulfides that includes cadmium (for example (Zn,Fe,Cd)S).\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>Photo gallery of greenockite:\n\u003C\u002Fp>\nwww.mindat.org\u002Fgallery.php?min=1746",3988,2726,{"id":322,"source_url":323,"license_code":324,"credit_html":325,"title":326,"description":327,"author":328,"original_width":329,"original_height":330},57406,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=72722432","Public domain","Andrew Silver, USGS, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=72722432\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Greenockite.jpg","Greenockite. Pen for scale. Mineral collection of Bringham Young University Department of Geology, Provo, Utah. BYU index 2-4073, CdS.","Andrew Silver, USGS",700,413,{"id":332,"source_url":333,"license_code":306,"credit_html":334,"title":335,"description":336,"author":310,"original_width":337,"original_height":338},57407,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=129024007","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=129024007\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Greenockite (Arkansas, USA) 2.jpg","Greenockite from Arkansas, USA. (public display, Carnegie Museum of Natural History, Pittsburgh, Pennsylvania, USA)\n\u003Cp>A mineral is a naturally-occurring, solid, inorganic, crystalline substance having a fairly definite chemical composition and having fairly definite physical properties.  At its simplest, a mineral is a naturally-occurring solid chemical.  Currently, there are over 4900 named and described minerals - about 200 of them are common and about 20 of them are very common.  Mineral classification is based on anion chemistry.  Major categories of minerals are: elements, sulfides, oxides, halides, carbonates, sulfates, phosphates, and silicates.\n\u003C\u002Fp>\u003Cp>The sulfide minerals contain one or more sulfide anions (S-2).  The sulfides are usually considered together with the arsenide minerals, the sulfarsenide minerals, and the telluride minerals.  Many sulfides are economically significant, as they occur commonly in ores.  The metals that combine with S-2 are mainly Fe, Cu, Ni, Ag, etc.  Most sulfides have a metallic luster, are moderately soft, and are noticeably heavy for their size.  These minerals will not form in the presence of free oxygen.  Under an oxygen-rich atmosphere, sulfide minerals tend to chemically weather to various oxide and hydroxide minerals.\n\u003C\u002Fp>\u003Cp>Greenockite is a scarce cadium sulfide mineral, CdS.  It has a nonmetallic luster, a yellow to red color, an orangish-yellowish to maroon streak, and is somewhat soft (H = 3 to 3.5).  It can occur as discrete crystals or as earthy, powdery coatings.\n\u003C\u002Fp>\u003Cp>In the mining districts of America's Mississippi Valley, sphalerite weathers into bright yellow powder in the supergene zone (= above the water table) - the powder can be a mix of metal sulfides that includes cadmium (for example (Zn,Fe,Cd)S).\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>Photo gallery of greenockite:\n\u003C\u002Fp>\nwww.mindat.org\u002Fgallery.php?min=1746",3583,2444,{"id":340,"source_url":341,"license_code":324,"credit_html":342,"title":343,"description":344,"author":345,"original_width":346,"original_height":347},10424,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=6969399","Andrew Silver, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=6969399\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Greenockite - USGS Mineral Specimens 592.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGreenockite\" class=\"extiw\" title=\"en:Greenockite\">Greenockite\u003C\u002Fa> (pen for scale) - Mineral collection of Bringham Young University Department of Geology, Provo, Utah - BYU index 2-4074","Andrew Silver",1400,1099,{"id":349,"source_url":350,"license_code":324,"credit_html":351,"title":352,"description":353,"author":354,"original_width":346,"original_height":355},57393,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=6666010","Photograph by Andrew Silver, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=6666010\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Greenokite byu00593.jpg","\u003Ca href=\"\u002F\u002Fcommons.wikimedia.org\u002Fwiki\u002FGreenockite\" class=\"mw-redirect\" title=\"Greenockite\">Greenockite\u003C\u002Fa>. Pen for scale. Mineral collection of Bringham Young University Department of Geology, Provo, \u003Ca href=\"\u002F\u002Fcommons.wikimedia.org\u002Fwiki\u002FUtah\" title=\"Utah\">Utah\u003C\u002Fa>","Photograph by Andrew Silver",1050,{"id":357,"source_url":358,"license_code":280,"credit_html":359,"title":360,"description":361,"author":284,"original_width":285,"original_height":362},10425,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10155670","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10155670\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Greenockite-Sphalerite-192714.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGreenockite\" class=\"extiw\" title=\"en:Greenockite\">Greenockite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSphalerite\" class=\"extiw\" title=\"en:Sphalerite\">Sphalerite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Joplin Field, Tri-State District, Jasper County, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMissouri\" class=\"extiw\" title=\"en:Missouri\">Missouri\u003C\u002Fa>, USA (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-3862.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 4.5 x 3.5 x 2.3 cm.\u003C\u002Fdd>\n\u003Cdd>Greenockite is an uncommon cadmium sulfide. Apple-green microcrystals of greenockite richly cover the hummocky matrix of sphalerite crystals on this fine, old-time specimen from the famous Joplin Field of the Tri-State District. Ex. Underhill and Feist Collections.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",551,{"id":364,"source_url":365,"license_code":280,"credit_html":366,"title":367,"description":368,"author":284,"original_width":285,"original_height":369},57395,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10145057","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10145057\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Smithsonite-Greenockite-146131.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSmithsonite\" class=\"extiw\" title=\"en:Smithsonite\">Smithsonite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGreenockite\" class=\"extiw\" title=\"en:Greenockite\">Greenockite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Gobbler Mine, Joplin Field, Tri-State District, Jasper County, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMissouri\" class=\"extiw\" title=\"en:Missouri\">Missouri\u003C\u002Fa>, USA (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-171305.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 9.0 x 5.7 x 3.7 cm.\u003C\u002Fdd>\n\u003Cdd>Lustrous botryoids of bladed, reddish-brown smithsonite form an aesthetic, old-time specimen from the Tri-State District of Missouri. This is a solid, two-sided crust of smithsonite and the botryoids on the backside are coated with yellow-tan greenockite. Bruising on some of the botryoids on the front are noted, but are really not very detracting on this fine old-timer, which comes from an UNCOMMON Joplin locality - the Gobbler Mine. Ex. George Elling Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",418,{"id":371,"source_url":372,"license_code":280,"credit_html":373,"title":374,"description":361,"author":284,"original_width":375,"original_height":376},57396,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10155671","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10155671\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Greenockite-Sphalerite-192715.jpg",500,386,{"id":378,"source_url":379,"license_code":280,"credit_html":380,"title":381,"description":382,"author":284,"original_width":383,"original_height":384},57397,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10159502","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10159502\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Greenockite-Cassiterite-202144.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGreenockite\" class=\"extiw\" title=\"en:Greenockite\">Greenockite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCassiterite\" class=\"extiw\" title=\"en:Cassiterite\">Cassiterite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Siglo Veinte Mine (Siglo XX Mine; Llallagua Mine; Catavi), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FLlallagua\" class=\"extiw\" title=\"en:Llallagua\">Llallagua\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FRafael_Bustillo_Province\" class=\"extiw\" title=\"en:Rafael Bustillo Province\">Rafael Bustillo Province\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FPotos%C3%AD_Department\" class=\"extiw\" title=\"en:Potosí Department\">Potosí Department\u003C\u002Fa>, Bolivia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-336.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 8.1 x 5.6 x 4.8 cm.\u003C\u002Fdd>\n\u003Cdd>This piece has several rich pockets of dense microcrystallized orange\u002Fred greenockite, in protected cavities of cassiterite ore. A rare old-time specimen from Llallagua with rich association of the very rare cadmium sulfide greenockite. This is one of two associated specimens (perhaps once joined), that were collected during the famous 4th Vaux-Academy expedition to Bolivia in 1929-1930. Ex. Academy of Natural Sciences Philadelphia Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",800,576,{"id":386,"source_url":387,"license_code":280,"credit_html":388,"title":389,"description":382,"author":284,"original_width":292,"original_height":390},57398,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10159503","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10159503\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Greenockite-Cassiterite-202145.jpg",355,{"id":392,"source_url":393,"license_code":280,"credit_html":394,"title":395,"description":396,"author":284,"original_width":383,"original_height":397},57399,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10159504","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10159504\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Greenockite-Cassiterite-202146.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGreenockite\" class=\"extiw\" title=\"en:Greenockite\">Greenockite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCassiterite\" class=\"extiw\" title=\"en:Cassiterite\">Cassiterite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Siglo Veinte Mine (Siglo XX Mine; Llallagua Mine; Catavi), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FLlallagua\" class=\"extiw\" title=\"en:Llallagua\">Llallagua\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FRafael_Bustillo_Province\" class=\"extiw\" title=\"en:Rafael Bustillo Province\">Rafael Bustillo Province\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FPotos%C3%AD_Department\" class=\"extiw\" title=\"en:Potosí Department\">Potosí Department\u003C\u002Fa>, Bolivia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-336.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 8.0 x 6.3 x 3.5 cm.\u003C\u002Fdd>\n\u003Cdd>This piece has several rich pockets of dense microcrystallized orange\u002Fred greenockite, in protected cavities of cassiterite ore. A rare old-time specimen from Llallagua with rich association of the very rare cadmium sulfide greenockite. This is one of two associated specimens (perhaps once joined), that were collected during the famous 4th Vaux-Academy expedition to Bolivia in 1929-1930. Ex. Academy of Natural Sciences Philadelphia Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",578,{"id":399,"source_url":400,"license_code":280,"credit_html":401,"title":402,"description":403,"author":284,"original_width":285,"original_height":404},57401,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10173054","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10173054\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Greenockite-Hemimorphite-Sphalerite-285103.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGreenockite\" class=\"extiw\" title=\"en:Greenockite\">Greenockite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHemimorphite\" class=\"extiw\" title=\"en:Hemimorphite\">Hemimorphite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSphalerite\" class=\"extiw\" title=\"en:Sphalerite\">Sphalerite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Joplin Field, Tri-State District, Jasper County, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMissouri\" class=\"extiw\" title=\"en:Missouri\">Missouri\u003C\u002Fa>, USA (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-3862.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 3.4 x 2.8 x 1.8 cm.\u003C\u002Fdd>\n\u003Cdd>A true, old-time, combination classic from the Joplin Field of the Tri-State District. Canary-yellow greenockite is included in striking radial sprays of gemmy hemimorphite blades. The sprays are richly and attractively scattered on the 3-dimensional matrix of translucent, honey-yellow sphalerite crystals on limestone matrix. Highly desirable and very showy combination material, at least 50 years old, from this historic district. From the noted Tri-State collection of George Feist.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",554,{"id":406,"source_url":407,"license_code":280,"credit_html":408,"title":409,"description":403,"author":284,"original_width":410,"original_height":285},57402,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10173055","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10173055\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Greenockite-Hemimorphite-Sphalerite-285104.jpg",557,{"id":412,"source_url":413,"license_code":280,"credit_html":414,"title":415,"description":416,"author":284,"original_width":383,"original_height":397},57403,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10456323","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10456323\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cassiterite-Greenockite-pas-166a.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCassiterite\" class=\"extiw\" title=\"en:Cassiterite\">Cassiterite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGreenockite\" class=\"extiw\" title=\"en:Greenockite\">Greenockite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Siglo Veinte Mine (Siglo XX Mine; Llallagua Mine; Catavi), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FLlallagua\" class=\"extiw\" title=\"en:Llallagua\">Llallagua\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FRafael_Bustillo_Province\" class=\"extiw\" title=\"en:Rafael Bustillo Province\">Rafael Bustillo Province\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FPotos%C3%AD_Department\" class=\"extiw\" title=\"en:Potosí Department\">Potosí Department\u003C\u002Fa>, Bolivia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-336.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: small cabinet, 8.0 x 6.3 x 3.5 cm\n\u003Cdl>\u003Cdt>Greenockite on Cassiterite\u003C\u002Fdt>\u003C\u002Fdl>\u003C\u002Fdd>\n\u003Cdd>This piece has several rich pockets of dense microcrystallized orange\u002Fred greenockite, in protected cavities of cassiterite ore. A rare oldtime specimen from Llallagua with rich association of the very rare cadmian sulfide greenockite. I have not seen a specimen of this material for sale before, and in fact was not aware that the species had even been found here until I looked it up. This is one of two associated specimens (perhaps once joined), that were collected during the famous 4th Vaux-Academy expedition to Bolivia in 1929-1930, and comes with one of the two original labels that accompanied the box they were in all these years.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",{"id":418,"source_url":419,"license_code":280,"credit_html":420,"title":421,"description":416,"author":284,"original_width":422,"original_height":292},57404,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10456324","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10456324\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cassiterite-Greenockite-pas-166b.jpg",372,{"id":424,"source_url":425,"license_code":280,"credit_html":426,"title":427,"description":428,"author":429,"original_width":430,"original_height":431},57405,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=20548619","Chris857, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=20548619\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Greenockite on Calcite - Joplin, Missouri.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGreenockite\" class=\"extiw\" title=\"w:Greenockite\">Greenockite\u003C\u002Fa> on \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002Fcalcite\" class=\"extiw\" title=\"w:calcite\">calcite\u003C\u002Fa> from \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FJoplin,_Missouri\" class=\"extiw\" title=\"w:Joplin, Missouri\">Joplin, Missouri\u003C\u002Fa>. Held in the \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FA._E._Seaman_Mineral_Museum\" class=\"extiw\" title=\"w:A. E. Seaman Mineral Museum\">A. E. Seaman Mineral Museum\u003C\u002Fa>.","Chris857",2866,2976,{"id":433,"source_url":434,"license_code":280,"credit_html":435,"title":436,"description":437,"author":438,"original_width":439,"original_height":440},31232,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=162903998","HolDu, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=162903998\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Greenockit, Prehnit 2.JPG","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGreenockite\" class=\"extiw\" title=\"en:Greenockite\">Greenockite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FPrehnite\" class=\"extiw\" title=\"en:Prehnite\">Prehnite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Bishopton, Renfrewshire, England\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","HolDu",5184,3888,[442,448,452],{"id":443,"url":444,"label":445,"formula":446,"spacegroup":447,"year":226},5714,"\u002Fcif\u002F5714.cif","Xu 1993","Cd S","P 63 m c",{"id":449,"url":450,"label":451,"formula":446,"spacegroup":447,"year":213},5715,"\u002Fcif\u002F5715.cif","Wyckoff 1963",{"id":453,"url":454,"label":455,"formula":446,"spacegroup":447,"year":180},5716,"\u002Fcif\u002F5716.cif","Ulrich 1925",[457,458],"Cadmium blende","Kadmiumocker",[460,464,468,472,476,480,485,488,492,495,499,502,506,510,514,517,521,524,528,531,535,539],{"lang":461,"names":462},"ca",[463],"greenockita",{"lang":465,"names":466},"cs",[467],"Greenockit",{"lang":469,"names":470},"de",[471,467],"Cadmiumblende",{"lang":473,"names":474},"el",[475],"Γρηνοκίτης",{"lang":477,"names":478},"es",[479],"Greenockita",{"lang":481,"names":482},"et",[483,484],"Griinokiit","grinokiit",{"lang":486,"names":487},"eu",[479],{"lang":489,"names":490},"fa",[491],"گرینوکیت",{"lang":493,"names":494},"fr",[7],{"lang":496,"names":497},"hu",[498],"greenockit",{"lang":500,"names":501},"it",[7],{"lang":503,"names":504},"ja",[505],"硫カドミウム鉱",{"lang":507,"names":508},"nb",[509],"greenockitt",{"lang":511,"names":512},"nl",[513],"Greenockiet",{"lang":515,"names":516},"nn",[509],{"lang":518,"names":519},"pl",[520],"Grenokit",{"lang":522,"names":523},"pt",[463],{"lang":525,"names":526},"ru",[527],"Гринокит",{"lang":529,"names":530},"sk",[467],{"lang":532,"names":533},"sl",[534],"Grinokit",{"lang":536,"names":537},"uk",[538],"Гринокіт",{"lang":540,"names":541},"zh",[542,543],"硫鎘礦","硫镉矿","Q414138",{"history":11,"applications":11}]