[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:1860":3},{"id":4,"longid":5,"guid":6,"name":7,"shortcode_ima":8,"entrytype":9,"entrytype_text":10,"varietyof":11,"synid":11,"polytypeof":11,"groupid":11,"weighting":12,"nolocadd":13,"blacklisted":13,"mindat_formula":14,"mindat_formula_note":11,"ima_formula":15,"elements":16,"sigelements":21,"key_elements":22,"impurities":23,"cim":24,"ima_status":25,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":11,"discovery_year":28,"strunz10ed1":29,"strunz10ed2":30,"strunz10ed3":31,"strunz10ed4":32,"dana8ed1":33,"dana8ed2":34,"dana8ed3":35,"dana8ed4":34,"csystem":36,"cclass":37,"spacegroup":38,"spacegroupset":39,"a":40,"b":41,"c":42,"alpha":43,"beta":43,"gamma":43,"aerror":44,"berror":11,"cerror":45,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":46,"csmetamict":13,"commentcrystal":11,"twinning":47,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":48,"tlform":11,"hmin":49,"hmax":44,"hardtype":11,"vhnmin":43,"vhnmax":43,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":50,"dmeas2":50,"dcalc":51,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":52,"commentluster":11,"diapheny":53,"streak":54,"colour":55,"commentcolor":11,"colors":56,"streak_colors":63,"luminescence":11,"uv":64,"cleavage":65,"cleavagetype":66,"fracturetype":67,"tenacity":68,"commentbreak":11,"opticaltype":69,"opticalsign":70,"opticalalpha":71,"opticalalpha2":43,"opticalalphaerror":11,"opticalbeta":72,"opticalbeta2":43,"opticalbetaerror":11,"opticalgamma":73,"opticalgamma2":43,"opticalgammaerror":11,"opticalomega":43,"opticalomega2":43,"opticalomegaerror":11,"opticalepsilon":43,"opticalepsilon2":43,"opticalepsilonerror":11,"opticaln":43,"opticaln2":43,"opticalnerror":11,"optical2vcalc":74,"optical2vcalc2":43,"optical2vcalcerror":11,"optical2vmeasured":75,"optical2vmeasured2":43,"optical2vmeasurederror":11,"rimin":76,"rimax":77,"opticaldispersion":78,"opticalpleochroism":11,"opticalpleochorismdesc":11,"opticalbirefringence":79,"opticalcomments":11,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":80,"opticalr":11,"specdispm":11,"ir":81,"electrical":82,"magnetism":11,"thermalbehaviour":83,"other":84,"industrial":85,"occurrence":11,"otheroccurrence":86,"type_specimen_store":11,"description_short":87,"aboutname":88,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":89,"reviewed_at":11,"variety_of":11,"varieties":90,"group_members":91,"associates":92,"confused_with":238,"type_localities":239,"occurrence_total":246,"citations":247,"images":354,"structures":731,"synonyms":753,"language_names":770,"wikidata_qid":901,"texts":902},1860,"1:1:1860:5","4b8c331d-af71-4f81-bee6-60cb37dcd798","Hemimorphite","Hmp",0,"mineral",null,55235,false,"Zn\u003Csub>4\u003C\u002Fsub>Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>·H\u003Csub>2\u003C\u002Fsub>O","Zn\u003Csub>4\u003C\u002Fsub>(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>)(OH)\u003Csub>2\u003C\u002Fsub> · H\u003Csub>2\u003C\u002Fsub>O",[17,18,19,20],"Si","Zn","O","H",[17,18,19,20],[18],",Cu,Fe,,","14.7.12",[26,27],"APPROVED","GRANDFATHERED","1853","9","B","D","10","56","1","2","Orthorhombic",6,27,"Imm2","8.367","10.730","5.155","0",5,3,2,"On {101} rare","Thin tabular crystals, sheaf-like or fan-like aggregates, stalactitic, mammillary, botryoidal.",4.5,"3.475","3.484","Sub-Adamantine,Vitreous,Sub-Vitreous,Greasy,Silky,Pearly","Transparent,Translucent","White","Colorless, white, pale blue, pale green, gray, brown",[57,58,59,60,61,62],"colorless","white","blue","green","gray","brown",[58],"May be bluish under SW UV.","Perfect on {110}, poor on {101}, {001} rare","Perfect","Irregular\u002FUneven,Sub-Conchoidal","brittle","Biaxial","+","1.614","1.617","1.636","44","46",1.614,1.636,"strong r > v","0.022","X = b; Y = a; Z = c.","May fluoresce and phosphoresce white to pale yellow in SW, MW, LW UV (Sterling Mine, NJ).","Pyroelectric.","Heated in a closed tube, it decrepitates, whitens, and gives off water. Before the blowpipe, almost infusible  (F = 6).","Gelatinizes with acids even when previously ignited. Decomposed by acetic acid with gelatinization. Soluble in a strong solution of KOH.","Ore of zinc.","Secondary mineral in the weathered portions of zinc deposits.","Fake Blue Hemimorphite Crystals\r\nCoated hemimorphite\r\nIn 2020 a number of electric-blue crystals of hemimorphite crystals came to market, from the Ojuela mine, Mapimi, Mexico. These have been proven to be deceptively stained using the artificial compou...","Named in 1853 by Adolph Kenngott in allusion to the hemimorphic morphology of the crystals. Many names were previously assigned to this species, including calamine.  Hemimorphite was chosen by the International Mineralogical Association, over calamine, in 1962.","2025-09-23 16:29:47",[],[],[93,101,110,119,128,136,143,151,159,166,175,182,190,198,206,213,221,229],{"id":94,"name":95,"entrytype":9,"csystem":36,"ima_formula":96,"mindat_formula":96,"hmin":97,"hmax":97,"dmeas":98,"dcalc":99,"primary_image_id":100},21,"Adamite","Zn\u003Csub>2\u003C\u002Fsub>(AsO\u003Csub>4\u003C\u002Fsub>)(OH)",3.5,"4.32","4.435",174,{"id":102,"name":103,"entrytype":9,"csystem":36,"ima_formula":104,"mindat_formula":105,"hmin":106,"hmax":45,"dmeas":107,"dcalc":108,"primary_image_id":109},233,"Anglesite","Pb(SO\u003Csub>4\u003C\u002Fsub>)","PbSO\u003Csub>4\u003C\u002Fsub>",2.5,"6.37","6.36",1430,{"id":111,"name":112,"entrytype":9,"csystem":113,"ima_formula":114,"mindat_formula":114,"hmin":115,"hmax":46,"dmeas":116,"dcalc":117,"primary_image_id":118},422,"Aurichalcite","Monoclinic","(Zn,Cu)\u003Csub>5\u003C\u002Fsub>(CO\u003Csub>3\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>6\u003C\u002Fsub>",1,"3.96","3.93",2314,{"id":120,"name":121,"entrytype":9,"csystem":122,"ima_formula":123,"mindat_formula":124,"hmin":45,"hmax":45,"dmeas":125,"dcalc":126,"primary_image_id":127},859,"Calcite","Trigonal","Ca(CO\u003Csub>3\u003C\u002Fsub>)","CaCO\u003Csub>3\u003C\u002Fsub>","2.7102","2.711",4401,{"id":129,"name":130,"entrytype":9,"csystem":36,"ima_formula":131,"mindat_formula":132,"hmin":45,"hmax":97,"dmeas":133,"dcalc":134,"primary_image_id":135},934,"Cerussite","Pb(CO\u003Csub>3\u003C\u002Fsub>)","PbCO\u003Csub>3\u003C\u002Fsub>","6.53","6.558",5045,{"id":137,"name":138,"entrytype":9,"csystem":36,"ima_formula":139,"mindat_formula":140,"hmin":106,"hmax":97,"dmeas":141,"dcalc":43,"primary_image_id":142},1040,"Chrysocolla","(Cu\u003Csub>2-x\u003C\u002Fsub>Al\u003Csub>x\u003C\u002Fsub>)H\u003Csub>2-x\u003C\u002Fsub>Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>5\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub> · nH\u003Csub>2\u003C\u002Fsub>O","Cu\u003Csub>2-x\u003C\u002Fsub>Al\u003Csub>x\u003C\u002Fsub>(H\u003Csub>2-x\u003C\u002Fsub>Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>5\u003C\u002Fsub>)(OH)\u003Csub>4\u003C\u002Fsub>·nH\u003Csub>2\u003C\u002Fsub>O, x \u003C 1","1.93",5675,{"id":144,"name":145,"entrytype":9,"csystem":113,"ima_formula":146,"mindat_formula":147,"hmin":46,"hmax":45,"dmeas":148,"dcalc":149,"primary_image_id":150},1583,"Fornacite","CuPb\u003Csub>2\u003C\u002Fsub>(CrO\u003Csub>4\u003C\u002Fsub>)(AsO\u003Csub>4\u003C\u002Fsub>)(OH)","Pb\u003Csub>2\u003C\u002Fsub>Cu(CrO\u003Csub>4\u003C\u002Fsub>)(AsO\u003Csub>4\u003C\u002Fsub>)(OH)","6.27","6.30",9296,{"id":152,"name":153,"entrytype":9,"csystem":154,"ima_formula":155,"mindat_formula":155,"hmin":106,"hmax":106,"dmeas":156,"dcalc":157,"primary_image_id":158},1641,"Galena","Isometric","PbS","7.60","7.57",9582,{"id":160,"name":161,"entrytype":9,"csystem":113,"ima_formula":162,"mindat_formula":162,"hmin":46,"hmax":106,"dmeas":163,"dcalc":164,"primary_image_id":165},1993,"Hydrozincite","Zn\u003Csub>5\u003C\u002Fsub>(CO\u003Csub>3\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>6\u003C\u002Fsub>","3.5","3.97",12029,{"id":167,"name":168,"entrytype":9,"csystem":169,"ima_formula":170,"mindat_formula":170,"hmin":97,"hmax":171,"dmeas":172,"dcalc":173,"primary_image_id":174},2714,"Mimetite","Hexagonal","Pb\u003Csub>5\u003C\u002Fsub>(AsO\u003Csub>4\u003C\u002Fsub>)\u003Csub>3\u003C\u002Fsub>Cl",4,"7.24","7.26",30195,{"id":176,"name":177,"entrytype":9,"csystem":154,"ima_formula":178,"mindat_formula":178,"hmin":171,"hmax":171,"dmeas":179,"dcalc":180,"primary_image_id":181},2812,"Murdochite","Cu\u003Csub>12\u003C\u002Fsub>Pb\u003Csub>2\u003C\u002Fsub>O\u003Csub>15\u003C\u002Fsub>Cl\u003Csub>2\u003C\u002Fsub>","5.9","6.06",16875,{"id":183,"name":184,"entrytype":9,"csystem":113,"ima_formula":185,"mindat_formula":186,"hmin":49,"hmax":49,"dmeas":187,"dcalc":188,"primary_image_id":189},3447,"Rosasite","CuZn(CO\u003Csub>3\u003C\u002Fsub>)(OH)\u003Csub>2\u003C\u002Fsub>","(Cu,Zn)\u003Csub>2\u003C\u002Fsub>(CO\u003Csub>3\u003C\u002Fsub>)(OH)\u003Csub>2\u003C\u002Fsub>","4","4.15",21115,{"id":191,"name":192,"entrytype":9,"csystem":122,"ima_formula":193,"mindat_formula":194,"hmin":171,"hmax":49,"dmeas":195,"dcalc":196,"primary_image_id":197},3688,"Smithsonite","Zn(CO\u003Csub>3\u003C\u002Fsub>)","ZnCO\u003Csub>3\u003C\u002Fsub>","4.42","4.43",30707,{"id":199,"name":200,"entrytype":9,"csystem":113,"ima_formula":201,"mindat_formula":202,"hmin":45,"hmax":45,"dmeas":203,"dcalc":204,"primary_image_id":205},3722,"Spencerite","Zn\u003Csub>4\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub> · 3H\u003Csub>2\u003C\u002Fsub>O","Zn\u003Csub>4\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>·3H\u003Csub>2\u003C\u002Fsub>O","3.123","3.282",22621,{"id":207,"name":208,"entrytype":9,"csystem":154,"ima_formula":209,"mindat_formula":209,"hmin":97,"hmax":171,"dmeas":210,"dcalc":211,"primary_image_id":212},3727,"Sphalerite","ZnS","3.9","4.096",66200,{"id":214,"name":215,"entrytype":9,"csystem":113,"ima_formula":216,"mindat_formula":217,"hmin":97,"hmax":171,"dmeas":218,"dcalc":219,"primary_image_id":220},4176,"Veszelyite","(Cu,Zn)\u003Csub>2\u003C\u002Fsub>Zn(PO\u003Csub>4\u003C\u002Fsub>)(OH)\u003Csub>3\u003C\u002Fsub> · 2H\u003Csub>2\u003C\u002Fsub>O","(Cu,Zn)\u003Csub>2\u003C\u002Fsub>Zn(PO\u003Csub>4\u003C\u002Fsub>)(OH)\u003Csub>3\u003C\u002Fsub>·2H\u003Csub>2\u003C\u002Fsub>O","3.4","3.42",27429,{"id":222,"name":223,"entrytype":9,"csystem":122,"ima_formula":224,"mindat_formula":224,"hmin":225,"hmax":225,"dmeas":226,"dcalc":227,"primary_image_id":228},4292,"Willemite","Zn\u003Csub>2\u003C\u002Fsub>SiO\u003Csub>4\u003C\u002Fsub>",5.5,"3.89","4.224",30976,{"id":230,"name":231,"entrytype":9,"csystem":232,"ima_formula":233,"mindat_formula":234,"hmin":106,"hmax":45,"dmeas":235,"dcalc":236,"primary_image_id":237},4322,"Wulfenite","Tetragonal","PbMoO\u003Csub>4\u003C\u002Fsub>","Pb(MoO\u003Csub>4\u003C\u002Fsub>)","6.5","6.88",30992,[],[240],{"id":241,"txt":242,"latitude":243,"longitude":244,"country":245},1981,"Băiţa mining district, Nucet, Bihor County, Romania",46.4818397,22.580562,"Romania",1669,[248,252,257,261,265,269,273,278,283,288,293,298,303,307,311,316,320,325,330,335,339,344,349],{"id":249,"year":250,"html":251,"doi":11},16111730,1853,"Kenngott, A. (1853) Hemimorphit. in Das Mohs’sche Mineralsystem, Verlag und Druck (Wien): 67-68.",{"id":253,"year":254,"html":255,"doi":256},5282,1884,"Thomson, J. Stuart (1884) Note on Crystals of Calamine from Wanlockhead, Dumfries-shire. \u003Ci>Mineralogical Magazine and Journal of the Mineralogical Society\u003C\u002Fi>,  5 (26) 332 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1884.005.26.04'>doi:10.1180\u002Fminmag.1884.005.26.04\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_5\u002F5-26-332.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1884.005.26.04",{"id":258,"year":259,"html":260,"doi":11},16111732,1894,"Pratt, J.H. (1894) Mineralogical Notes on Cerussite, Calamine and Zircon. American Journal of Science: 48(285): 212.",{"id":262,"year":263,"html":264,"doi":11},16111733,1899,"Clarke, F.W., Steiger, G. (1899) Experiments relative to the Constitution of Pectolite, Pyrophyllite, Calamine, and Analcite. American Journal of Science: 8(46): 245.",{"id":266,"year":267,"html":268,"doi":11},16111734,1911,"Pogue, J.E. (1911) On calamine crystals from Mexico, rutile-mica intergrowths from Canada, and pseudomorphs of marcasite arfter pyrrhotite from Russia. Proceedings U.S. National Museum: 39(1801): 571-579.",{"id":270,"year":271,"html":272,"doi":11},518765,1919,"Poitevin, Eugene (1919) Crystallography of some Canadian minerals: stephanite, epidote, and calamine. \u003Ci>American Mineralogist\u003C\u002Fi>,  4 (3) 22-25 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM4\u002FAM4_22.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":274,"year":275,"html":276,"doi":277},104654,1932,"Ito, T., West, J. (1932) The Structure of Hemimorphite (H\u003Csub>2\u003C\u002Fsub>Zn\u003Csub>2\u003C\u002Fsub>SiO\u003Csub>5\u003C\u002Fsub>) \u003Ci>Zeitschrift für Kristallographie - Crystalline Materials\u003C\u002Fi>,  83 (1) 1-8 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1932.83.1.1'>doi:10.1524\u002Fzkri.1932.83.1.1\u003C\u002Fa>","10.1524\u002Fzkri.1932.83.1.1",{"id":279,"year":280,"html":281,"doi":282},232758,1956,"Roy, Della Martin, Mumpton, Frederick Albert (1956) Stability of minerals in the system ZnO-SiO2-H2O. \u003Ci>Economic Geology\u003C\u002Fi>,  51 (5). 432-443 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2113\u002Fgsecongeo.51.5.432'>doi:10.2113\u002Fgsecongeo.51.5.432\u003C\u002Fa>","10.2113\u002Fgsecongeo.51.5.432",{"id":284,"year":285,"html":286,"doi":287},106426,1960,"Barclay, G. A., Cox, E. G. (1960) The structure of hemimorphite. \u003Ci>Zeitschrift für Kristallographie - Crystalline Materials\u003C\u002Fi>,  113 (1) 23-29 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1960.113.1-6.23'>doi:10.1524\u002Fzkri.1960.113.1-6.23\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fzk\u002Fvol113\u002FZK113_23.pdf' class='refpdflink'>\u003C\u002Fa>","10.1524\u002Fzkri.1960.113.1-6.23",{"id":289,"year":290,"html":291,"doi":292},5696,1962,"(1962) International Mineralogical Association: Commission on New Minerals and Mineral Names. \u003Ci>Mineralogical Magazine and Journal of the Mineralogical Society\u003C\u002Fi>,  33 (258) 260-263 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1962.033.258.09'>doi:10.1180\u002Fminmag.1962.033.258.09\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_33\u002F33-258-260.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1962.033.258.09",{"id":294,"year":295,"html":296,"doi":297},107409,1967,"McDonald, W. S., Cruickshank, D. W. J. (1967) Refinement of the structure of hemimorphite. \u003Ci>Zeitschrift für Kristallographie - Crystalline Materials\u003C\u002Fi>,  124 (3) 180-191 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1967.124.3.180'>doi:10.1524\u002Fzkri.1967.124.3.180\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fzk\u002Fvol124\u002FZK124_180.pdf' class='refpdflink'>\u003C\u002Fa>","10.1524\u002Fzkri.1967.124.3.180",{"id":299,"year":300,"html":301,"doi":302},109271,1978,"Hill, Roderick J., Gibbs, Gerald V., Craig, James R., Ross, Fred K., Williams, Jack M. (1978) A neutron-diffraction study of hemimorphite. \u003Ci>Zeitschrift für Kristallographie - Crystalline Materials\u003C\u002Fi>,  146 (1-6) 241-259 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1978.146.16.241'>doi:10.1524\u002Fzkri.1978.146.16.241\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fzk\u002Fvol146\u002FZK146_241.pdf' class='refpdflink'>\u003C\u002Fa>","10.1524\u002Fzkri.1978.146.16.241",{"id":304,"year":241,"html":305,"doi":306},109936,"Cooper, B. J., Gibbs, G. V. (1981) The effects of heating and dehydration on the crystal structure of hemimorphite up to 600 °C. \u003Ci>Zeitschrift für Kristallographie - Crystalline Materials\u003C\u002Fi>,  156 (14) 305-321 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1981.156.14.305'>doi:10.1524\u002Fzkri.1981.156.14.305\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fzk\u002Fvol156\u002FZK156_305.pdf' class='refpdflink'>\u003C\u002Fa>","10.1524\u002Fzkri.1981.156.14.305",{"id":308,"year":309,"html":310,"doi":11},16111741,1982,"Fischer, K.F., Schäfer, G. (1982) Umgehung des Phasenproblems durch Intensitätsmessung bei zwei Wellenlängen. Beispiel: Struktur des Hemimorphit mittels Lambda-Methode. Zeitschrift für Kristallographie: 159: 47-48. (Abstract.) https:\u002F\u002Frruff.info\u002Fuploads\u002FZK159_47.pdf",{"id":312,"year":313,"html":314,"doi":315},127573,1997,"Libowitzky, Eugen, Kohler, Thomas, Armbruster, Thomas, Rossman, George R. (1997) Proton disorder in dehydrated hemimorphite – IR spectroscopy and X-ray structure refinement at low and ambient temperatures. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  9 (4) 803-810 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1127\u002Fejm\u002F9\u002F4\u002F0803'>doi:10.1127\u002Fejm\u002F9\u002F4\u002F0803\u003C\u002Fa>","10.1127\u002Fejm\u002F9\u002F4\u002F0803",{"id":317,"year":318,"html":319,"doi":11},16964793,2001,"(2001) Hemimorphite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fhemimorphite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":321,"year":322,"html":323,"doi":324},395607,2006,"Kolesov, B. (2006) Raman investigation of H2O molecule and hydroxyl groups in the channels of hemimorphite. \u003Ci>American Mineralogist\u003C\u002Fi>,  91 (8) 1355-1362 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam.2006.2179'>doi:10.2138\u002Fam.2006.2179\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fam\u002Fvol91\u002FAM91_1355.pdf' class='refpdflink'>\u003C\u002Fa>","10.2138\u002Fam.2006.2179",{"id":326,"year":327,"html":328,"doi":329},16111745,2007,"Frost, Ray L., Bouzaid, Jocelyn M., Jagannadha Reddy, B. (2007) Vibrational spectroscopy of the sorosilicate mineral hemimorphite Zn4(OH)2Si2O7·H2O. \u003Ci>Polyhedron\u003C\u002Fi>,  26 (12). 2405-2412 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.poly.2006.12.008'>doi:10.1016\u002Fj.poly.2006.12.008\u003C\u002Fa>","10.1016\u002Fj.poly.2006.12.008",{"id":331,"year":332,"html":333,"doi":334},396248,2009,"Geiger, C. A., Dachs, E. (2009) Quasi-ice-like CP behavior of molecular H2O in hemimorphite Zn4Si2O7(OH)2·H2O: CP and entropy of confined H2O in microporous silicates. \u003Ci>American Mineralogist\u003C\u002Fi>,  94 (4) 634-637 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam.2009.3138'>doi:10.2138\u002Fam.2009.3138\u003C\u002Fa>","10.2138\u002Fam.2009.3138",{"id":336,"year":332,"html":337,"doi":338},128889,"Dachs, Edgar, Geiger, Charles A. (2009) Heat-capacity behaviour of hemimorphite, Zn4Si2O7(OH)2H2O, and its dehydrated analogue Zn4Si2O7(OH)2: a calorimetric and thermodynamic investigation of their phase transitions. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  21 (5) 971-983 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1127\u002F0935-1221\u002F2009\u002F0021-1975'>doi:10.1127\u002F0935-1221\u002F2009\u002F0021-1975\u003C\u002Fa>","10.1127\u002F0935-1221\u002F2009\u002F0021-1975",{"id":340,"year":341,"html":342,"doi":343},398581,2018,"Medas, Daniela, Meneghini, Carlo, Podda, Francesca, Floris, Costantino, Casu, Mariano, Casu, Maria Antonietta, Musu, Elodia, de Giudici, Giovanni (2018) Structure of low-order hemimorphite produced in a Zn-rich environment by cyanobacterium Leptolingbya frigida. \u003Ci>American Mineralogist\u003C\u002Fi>,  103 (5) 711-719 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-2018-6128'>doi:10.2138\u002Fam-2018-6128\u003C\u002Fa>","10.2138\u002Fam-2018-6128",{"id":345,"year":346,"html":347,"doi":348},13423393,2020,"Li, Yingzhe, Bass, Jay D. (2020) Single Crystal Elastic Properties of Hemimorphite, a Novel Hydrous Silicate. \u003Ci>Minerals\u003C\u002Fi>, 10 (5) 425 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3390\u002Fmin10050425'>doi:10.3390\u002Fmin10050425\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fwww.mdpi.com\u002F2075-163X\u002F10\u002F5\u002F425\u002Fpdf?version=1589120064' class='refpdflink'>\u003C\u002Fa>","10.3390\u002Fmin10050425",{"id":350,"year":351,"html":352,"doi":353},17734931,2025,"Gajda, Roman; Sławiński, Wojciech; Poręba, Tomasz; Parafiniuk, Jan; Mezouar, Mohamed; Dera, Przemysław; Woźniak, Krzysztof (2025) Incommensurately modulated structure of Zn\u003Csub>4\u003C\u002Fsub>Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>·H\u003Csub>2\u003C\u002Fsub>O at high pressure. \u003Ci>IUCrJ\u003C\u002Fi>,  12 (1). 62-73 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1107\u002Fs2052252524011060'>doi:10.1107\u002Fs2052252524011060\u003C\u002Fa>","10.1107\u002Fs2052252524011060",[355,364,370,380,385,394,403,412,417,425,432,439,448,453,458,468,477,486,492,497,506,514,522,530,538,547,555,563,569,575,581,589,597,606,616,623,629,636,642,649,656,662,668,677,686,694,701,708,716,722],{"id":356,"source_url":357,"license_code":358,"credit_html":359,"title":360,"description":361,"author":362,"original_width":363,"original_height":363},11125,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=98624550","CC BY-SA 4.0","Ivar Leidus, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=98624550\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphite - Mapimi, Durango, Mexico.jpg","Colorless prismatic crystals of hemimorphite on matrix (4.5 × 4.0 × 2.0 cm) with calcite. Found from Ojuela mine, Mapimí, Durango, Mexico.","Ivar Leidus",6000,{"id":365,"source_url":366,"license_code":358,"credit_html":367,"title":7,"description":11,"author":11,"original_width":368,"original_height":369},29864,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F128785","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby-sa\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F128785\" rel=\"noopener\">University of Tartu, Natural History Museum\u003C\u002Fa> via Europeana",712,1000,{"id":371,"source_url":372,"license_code":373,"credit_html":374,"title":375,"description":376,"author":377,"original_width":378,"original_height":379},58652,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=7739326","CC BY-SA 3.0","Didier Descouenss, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=7739326\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","HemimorphiteMexiqueFrome11.jpg","\u003Ca href=\"\u002F\u002Fcommons.wikimedia.org\u002Fwiki\u002FHemimorphite\" class=\"mw-redirect\" title=\"Hemimorphite\">hemimorphite\u003C\u002Fa> - Ojuela Mine, Mapimí, Mun. de Mapimí, Durango, \u003Ca href=\"\u002F\u002Fcommons.wikimedia.org\u002Fwiki\u002FMexico\" class=\"mw-redirect\" title=\"Mexico\">Mexico\u003C\u002Fa> - (21 × 12 cm)","Didier Descouenss",4089,4912,{"id":381,"source_url":382,"license_code":358,"credit_html":383,"title":7,"description":11,"author":11,"original_width":369,"original_height":384},29865,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F65434","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby-sa\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F65434\" rel=\"noopener\">The Estonian Museum of Natural History\u003C\u002Fa> via Europeana",666,{"id":386,"source_url":387,"license_code":358,"credit_html":388,"title":389,"description":390,"author":391,"original_width":392,"original_height":393},58655,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=38224197","Sosnowski, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=38224197\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphite from china.JPG","Hemimorfit","Sosnowski",4825,3217,{"id":395,"source_url":396,"license_code":358,"credit_html":397,"title":398,"description":399,"author":400,"original_width":401,"original_height":402},11126,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146497041","Kritzolina, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146497041\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphite from Sardinia 01.jpg","Hemimorphite from Sardinia - place of discovery is given as Minera Malfidana","Kritzolina",5472,3648,{"id":404,"source_url":405,"license_code":358,"credit_html":406,"title":407,"description":408,"author":409,"original_width":410,"original_height":411},58656,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=38414569","Photo by and (c)2015 Derek Ramsey (Ram-Man), via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=38414569\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphite Specimen 9.JPG","Photo of Hemimorphite. It was taken at the Delaware Museum of Natural History and is listed as specimen #9.","Photo by and (c)2015 Derek Ramsey (Ram-Man)",4608,3036,{"id":413,"source_url":414,"license_code":358,"credit_html":415,"title":416,"description":399,"author":400,"original_width":401,"original_height":402},11127,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146497042","Kritzolina, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146497042\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphite from Sardinia 02.jpg",{"id":418,"source_url":419,"license_code":358,"credit_html":420,"title":421,"description":422,"author":400,"original_width":423,"original_height":424},11128,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146792963","Kritzolina, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146792963\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphite from Italy 02.jpg","Hemimorphite from Monte Poni, Sardinia, Italy",4935,3290,{"id":426,"source_url":427,"license_code":358,"credit_html":428,"title":429,"description":422,"author":400,"original_width":430,"original_height":431},11129,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146792964","Kritzolina, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146792964\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphite from Italy 03.jpg",4800,3200,{"id":433,"source_url":434,"license_code":358,"credit_html":435,"title":436,"description":422,"author":400,"original_width":437,"original_height":438},11130,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146792965","Kritzolina, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146792965\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphite from Italy 01.jpg",4850,3233,{"id":440,"source_url":441,"license_code":358,"credit_html":442,"title":443,"description":444,"author":445,"original_width":446,"original_height":447},58659,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113720760","Koreller, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113720760\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Muséum de Nantes - 239 - Hémimorphite (Mexique).jpg","Hémimorphite, en provenance du Mexique, au Muséum de Nantes","Koreller",4272,2848,{"id":449,"source_url":450,"license_code":358,"credit_html":451,"title":452,"description":444,"author":445,"original_width":446,"original_height":447},58660,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113720761","Koreller, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113720761\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Muséum de Nantes - 240 - Hémimorphite (Mexique).jpg",{"id":454,"source_url":455,"license_code":358,"credit_html":456,"title":457,"description":444,"author":445,"original_width":446,"original_height":447},58661,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113720762","Koreller, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113720762\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Muséum de Nantes - 241 - Hémimorphite (Mexique).jpg",{"id":459,"source_url":460,"license_code":461,"credit_html":462,"title":463,"description":464,"author":465,"original_width":466,"original_height":467},58664,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=167117935","CC BY 4.0","Animalculum, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=167117935\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphite, Musee de Mineralogie, Paris, 2025.jpg","Hemimorphite from Seras, Germs-sur-l’Oussouet, Hautes-Pyrenees, France in Musee de Mineralogie, Paris","Animalculum",4096,2305,{"id":469,"source_url":470,"license_code":461,"credit_html":471,"title":472,"description":473,"author":474,"original_width":475,"original_height":476},58666,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=182899722","Marie-Lan Taÿ Pamart, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=182899722\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphite Mapimí Minéraux SU.jpg","Hemimorphite from from Mapimí, Durango, Mexico. Sorbonne University mineral collection.","Marie-Lan Taÿ Pamart",4567,6090,{"id":478,"source_url":479,"license_code":373,"credit_html":480,"title":481,"description":482,"author":483,"original_width":484,"original_height":485},39195,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=7738835","Didier Descouens, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=7738835\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","HemimorphiteMexique.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHemimorphite\" class=\"extiw\" title=\"en:Hemimorphite\">Hemimorphite\u003C\u002Fa> - Ojuela Mine, Mapimí, Mun. de Mapimí, Durango, \u003Ca href=\"\u002F\u002Fcommons.wikimedia.org\u002Fwiki\u002FMexico\" class=\"mw-redirect\" title=\"Mexico\">Mexico\u003C\u002Fa> (XX1mm)","Didier Descouens",1053,1153,{"id":487,"source_url":488,"license_code":358,"credit_html":489,"title":490,"description":491,"author":400,"original_width":401,"original_height":402},9586,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146495388","Kritzolina, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146495388\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphite and Galena 01.jpg","Hemimorphite and Galena found in Bleiberg, Austria",{"id":493,"source_url":494,"license_code":358,"credit_html":495,"title":496,"description":491,"author":400,"original_width":401,"original_height":402},9587,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146495389","Kritzolina, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146495389\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphite and Galena 02.jpg",{"id":498,"source_url":499,"license_code":461,"credit_html":500,"title":501,"description":502,"author":503,"original_width":504,"original_height":505},56052,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146468893","Slashme, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146468893\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphit Galenit 1.jpg","Hemimorphite and Galenite from Bleiberg, Carinthia, Austria","Slashme",5198,3462,{"id":507,"source_url":508,"license_code":461,"credit_html":509,"title":510,"description":511,"author":503,"original_width":512,"original_height":513},56053,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146468894","Slashme, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146468894\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphit Galenit 2.jpg","Hemimorphite and galenite from Bleiberg, Carinthia, Austria",4981,3349,{"id":515,"source_url":516,"license_code":461,"credit_html":517,"title":518,"description":519,"author":503,"original_width":520,"original_height":521},58662,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146468913","Slashme, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146468913\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphit Galenit 11.jpg","Hemimorphite and galenite from Bleiberg, Kärnten, Austria",4424,2961,{"id":523,"source_url":524,"license_code":373,"credit_html":525,"title":526,"description":527,"author":528,"original_width":529,"original_height":447},4028,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=13304297","Parent Géry, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=13304297\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hémimorphite, mimétite sur limonite (Mexique).JPG","crystals of hemimorphite, crystals of mimetite, crystals of goethite, crystals of limonite : Ojuela Mine, Mapimi, Municipio de Mapimi, Durango, Mexico","Parent Géry",3792,{"id":531,"source_url":532,"license_code":358,"credit_html":533,"title":534,"description":535,"author":483,"original_width":536,"original_height":537},5067,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=7747311","Didier Descouens, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=7747311\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphite-cesarolite.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHemimorphite\" class=\"extiw\" title=\"en:Hemimorphite\">Hemimorphite\u003C\u002Fa> with \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCes%C3%A0rolite\" class=\"extiw\" title=\"en:Cesàrolite\">Cesàrolite\u003C\u002Fa>\n\u003Cdd>Locality : Germs sur Oussouet, Lourdes, Hautes-Pyrénées, Midi-Pyrénées, France\u003C\u002Fdd>\n\u003Cdd>Size : view 1.5cm\u003C\u002Fdd>",4592,3056,{"id":539,"source_url":540,"license_code":373,"credit_html":541,"title":542,"description":543,"author":544,"original_width":545,"original_height":546},5196,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10163886","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10163886\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Willemite-Chalcophanite-Hemimorphite-230619.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FWillemite\" class=\"extiw\" title=\"en:Willemite\">Willemite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FChalcophanite\" class=\"extiw\" title=\"en:Chalcophanite\">Chalcophanite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHemimorphite\" class=\"extiw\" title=\"en:Hemimorphite\">Hemimorphite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Potosí Mine, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAquiles_Serd%C3%A1n\" class=\"extiw\" title=\"en:Aquiles Serdán\">Aquiles Serdán\u003C\u002Fa>, West Camp, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSanta_Eulalia_District\" class=\"extiw\" title=\"en:Santa Eulalia District\">Santa Eulalia District\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAquiles_Serd%C3%A1n,_Chihuahua\" class=\"extiw\" title=\"en:Aquiles Serdán, Chihuahua\">Municipio de Aquiles Serdán\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FChihuahua\" class=\"extiw\" title=\"en:Chihuahua\">Chihuahua\u003C\u002Fa>, Mexico (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-18927.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 15.8 x 10.0 x 6.2 cm.\u003C\u002Fdd>\n\u003Cdd>A fine, rare, large cabinet combination specimen from Santa Eulalia and the Dave Stoudt Collection. Both sides of the vuggy, 3-dimensional, very sturdy, sintered gossan matrix are richly covered with lustrous, translucent, gray willemite botryoids. The scattering of glassy hemimorphite blades to 1.5 cm is an elegant accent to the botryoidal willemite. Chalcophanite is an uncommon zinc, iron, manganese oxide, but is very rare at Santa Eulalia. The large \"V\" of sparkly, grape-like clusters of botryoidal chalcophanite on the front of the piece is very noteworthy. This Santa Eulalia specimen comes with a label with concise mine locality information, indicating that this is, indeed, a significant, large and rare specimen.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Robert M. Lavinsky",600,431,{"id":548,"source_url":549,"license_code":373,"credit_html":550,"title":551,"description":552,"author":544,"original_width":553,"original_height":554},9137,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10175327","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10175327\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Ellestadite-(F)-Hemimorphite-48321.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FEllestadite-(F)\" class=\"extiw\" title=\"en:Ellestadite-(F)\">Ellestadite-(F)\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHemimorphite\" class=\"extiw\" title=\"en:Hemimorphite\">Hemimorphite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMapim%C3%AD_(municipality)\" class=\"extiw\" title=\"en:Mapimí (municipality)\">Municipio de Mapimí\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDurango\" class=\"extiw\" title=\"en:Durango\">Durango\u003C\u002Fa>, Mexico (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-14161.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>A truly amazing pseudomorph with SHARP blades up to .7 cm. Although small overall, this is the best example I have yet seen of this classic replacement which used to be called by the name of wilkeite. The pics say it all. 2.7 x 2.7 x 1.7 cm\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",800,768,{"id":556,"source_url":557,"license_code":373,"credit_html":558,"title":559,"description":560,"author":544,"original_width":561,"original_height":562},9140,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10442998","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10442998\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fluorellestadite-Hemimorphite-3d11b.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FFluorellestadite\" class=\"extiw\" title=\"en:Fluorellestadite\">Fluorellestadite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHemimorphite\" class=\"extiw\" title=\"en:Hemimorphite\">Hemimorphite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMapim%C3%AD\" class=\"extiw\" title=\"en:Mapimí\">Mapimí\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMapim%C3%AD_(municipality)\" class=\"extiw\" title=\"en:Mapimí (municipality)\">Municipio de Mapimí\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDurango\" class=\"extiw\" title=\"en:Durango\">Durango\u003C\u002Fa>, Mexico (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-22316.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: thumbnail, 2.7 x 2.7 x 1.7 cm\n\u003Cdl>\u003Cdt>Fluorellestadite ps. Hemimorphite (wilkeite)\u003C\u002Fdt>\u003C\u002Fdl>\u003C\u002Fdd>\n\u003Cdd>A truly amazing pseudomorph with SHARP blades up to .7 cm. Although small overall, this is the best example I have yet seen of this classic replacement which used to be called by the name of wilkeite. The pics say it all.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",331,400,{"id":564,"source_url":565,"license_code":373,"credit_html":566,"title":567,"description":560,"author":544,"original_width":568,"original_height":562},9141,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10442999","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10442999\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fluorellestadite-Hemimorphite-3d11c.jpg",376,{"id":570,"source_url":571,"license_code":373,"credit_html":572,"title":573,"description":560,"author":544,"original_width":562,"original_height":574},9142,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10443000","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10443000\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fluorellestadite-Hemimorphite-3d11a.jpg",384,{"id":576,"source_url":577,"license_code":373,"credit_html":578,"title":579,"description":560,"author":544,"original_width":562,"original_height":580},9143,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10443001","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10443001\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fluorellestadite-Hemimorphite-3d11d.jpg",391,{"id":582,"source_url":583,"license_code":461,"credit_html":584,"title":585,"description":586,"author":465,"original_width":587,"original_height":588},13358,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=167129263","Animalculum, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=167129263\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Veszelyite with Hemimorphite and Kipushite, Musee de Mineralogie, Paris, 2025.jpg","Veszelyite with Hemimorphite and Kipushite from M'fouti, Bouenza, Republic of Congo in Musee de Mineralogie, Paris",3096,4128,{"id":590,"source_url":591,"license_code":373,"credit_html":592,"title":593,"description":594,"author":544,"original_width":595,"original_height":596},28078,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10119963","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10119963\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphite-Willemite-20547.jpg","\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\u002FWillemite\" class=\"extiw\" title=\"en:Willemite\">Willemite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Potosí Mine (El Potosí Mine), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FFrancisco_Portillo\" class=\"extiw\" title=\"en:Francisco Portillo\">Francisco Portillo\u003C\u002Fa>, West Camp, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSanta_Eulalia_District\" class=\"extiw\" title=\"en:Santa Eulalia District\">Santa Eulalia District\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAquiles_Serd%C3%A1n,_Chihuahua\" class=\"extiw\" title=\"en:Aquiles Serdán, Chihuahua\">Municipio de Aquiles Serdán\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FChihuahua\" class=\"extiw\" title=\"en:Chihuahua\">Chihuahua\u003C\u002Fa>, Mexico (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2312.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>A VERY CHOICE and VERY RARE specimen from the Potosi Mine at Santa Eulalia, Mexico of lustrous transparent to translucent hemimorphite crystals to 3.2 cm aesthetically set on a crust of very sparkly botryoidal hematite-tinted willemite. A few trivially broken hemimorphite crystals, but basically near-pristine despite its age (this IS an old specimen at least 1960s if not much earlier) and I have not seen a piece with this combination for sale before. 7.5 x 5.5 x 3.2 cm\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",650,521,{"id":598,"source_url":599,"license_code":600,"credit_html":601,"title":602,"description":603,"author":604,"original_width":605,"original_height":447},34304,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=6048306","Public domain","Géry PARENT, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=6048306\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Auricalcite, hemimorphite, goethite.jpg","aurichalcite, hemimorphite, goethite : San Antonio Mine (San Antonio el Grande Mine), East Camp, Santa Eulalia District, Mun. de Aquiles Serdán, Chihuahua, Mexico","Géry PARENT",4288,{"id":607,"source_url":608,"license_code":609,"credit_html":610,"title":611,"description":612,"author":613,"original_width":614,"original_height":615},34307,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=9989754","CC BY 3.0","Corie Mattar, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=9989754\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Aurichalcite and Hemimorphite - Blue Bell claims, Baker, San Bernardino County, California, USA.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAurichalcite\" class=\"extiw\" title=\"en:Aurichalcite\">Aurichalcite\u003C\u002Fa> (pale blue) and \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHemimorphite\" class=\"extiw\" title=\"en:Hemimorphite\">Hemimorphite\u003C\u002Fa> (colorless)\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Blue Bell claims (Hard Luck claims), Baker, San Bernardino Co., California, USA\u003C\u002Fdd>\n\u003Cdd>Original description: Beautifully colored aurichalcite crystals nestled in among varied hemimorphite crystals - FOV approx 2.5cm wide and 4 cm tall\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Corie Mattar",798,1024,{"id":617,"source_url":618,"license_code":373,"credit_html":619,"title":620,"description":621,"author":544,"original_width":545,"original_height":622},34310,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10153484","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10153484\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Aurichalcite-Hemimorphite-181575.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAurichalcite\" class=\"extiw\" title=\"en:Aurichalcite\">Aurichalcite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHemimorphite\" class=\"extiw\" title=\"en:Hemimorphite\">Hemimorphite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: 79 Mine (79th Mine; Seventy-Nine Mine; Seventy-Nine property; McHur prospect), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FZantigo\" class=\"extiw\" title=\"en:Zantigo\">Chilito\u003C\u002Fa>, Hayden area, Banner District, Dripping Spring Mts, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGila_County,_Arizona\" class=\"extiw\" title=\"en:Gila County, Arizona\">Gila County\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FArizona\" class=\"extiw\" title=\"en:Arizona\">Arizona\u003C\u002Fa>, USA (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-3322.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 4.9 x 2.7 x 1.4 cm.\u003C\u002Fdd>\n\u003Cdd>A fine specimen of velvety balls of aurichalcite on a field of sparkly hemimorphite - old classic 79 Mine material. Ex. Stoudt Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",370,{"id":624,"source_url":625,"license_code":373,"credit_html":626,"title":627,"description":621,"author":544,"original_width":562,"original_height":628},34311,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10153486","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10153486\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Aurichalcite-Hemimorphite-181576.jpg",366,{"id":630,"source_url":631,"license_code":373,"credit_html":632,"title":633,"description":634,"author":544,"original_width":545,"original_height":635},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":637,"source_url":638,"license_code":373,"credit_html":639,"title":640,"description":634,"author":544,"original_width":641,"original_height":545},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":643,"source_url":644,"license_code":373,"credit_html":645,"title":646,"description":647,"author":544,"original_width":648,"original_height":545},59553,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10152593","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10152593\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hopeite-Hemimorphite-179854.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHopeite\" class=\"extiw\" title=\"en:Hopeite\">Hopeite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHemimorphite\" class=\"extiw\" title=\"en:Hemimorphite\">Hemimorphite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Kabwe Mine (Broken Hill Mine), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FKabwe\" class=\"extiw\" title=\"en:Kabwe\">Kabwe (Broken Hill)\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCentral_Province\" class=\"extiw\" title=\"en:Central Province\">Central Province\u003C\u002Fa>, Zambia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-4341.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 3.5 x 3 x 2 cm.\u003C\u002Fdd>\n\u003Cdd>This pseudomorph of hopeite after hemimorphite is spectacular and it is very rare. Diverging blades clearly exhibiting parallel growth of hemimorphite, to 2.5 cm in length and of an umber color have been replaced by hopeite, the much rarer zinc phosphate. Ex. Martin Zinn Collection.   This Photo was Mindat.org Photo of the Day - 1st Sep 2008\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",566,{"id":650,"source_url":651,"license_code":373,"credit_html":652,"title":653,"description":654,"author":544,"original_width":562,"original_height":655},59555,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10453558","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10453558\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphite-Hopeite-mrz338b.jpg","\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\u002FHopeite\" class=\"extiw\" title=\"en:Hopeite\">Hopeite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBroken_Hill,_New_South_Wales\" class=\"extiw\" title=\"en:Broken Hill, New South Wales\">Broken Hill\u003C\u002Fa>, Yancowinna County, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FNew_South_Wales\" class=\"extiw\" title=\"en:New South Wales\">New South Wales\u003C\u002Fa>, Australia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-72.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: miniature, 3.5 x 3 x 2 cm\n\u003Cdl>\u003Cdt>Hopeite ps. Hemimorphite\u003C\u002Fdt>\u003C\u002Fdl>\u003C\u002Fdd>\n\u003Cdd>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>\nWith out question this pseudomorph of hopeite after hemimorphite is not only spectacular, it is very rare. Diverging blades clearly exhibiting parallel growth of hemimorphite, to 2.5 cm in length and of an umber color have been replaced by hopeite, the much rarer zinc phosphate. Awesome!",369,{"id":657,"source_url":658,"license_code":373,"credit_html":659,"title":660,"description":654,"author":544,"original_width":562,"original_height":661},59556,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10453559","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10453559\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphite-Hopeite-mrz338c.jpg",311,{"id":663,"source_url":664,"license_code":373,"credit_html":665,"title":666,"description":654,"author":544,"original_width":562,"original_height":667},59557,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10453560","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10453560\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphite-Hopeite-mrz338d.jpg",338,{"id":669,"source_url":670,"license_code":373,"credit_html":671,"title":672,"description":673,"author":674,"original_width":675,"original_height":676},60418,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=6554940","Ra'ike (see also: de:Benutzer:Ra'ike), via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=6554940\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hydrozinkit (Zinkblüte) mit Hemimorphit - Bleiberg, Kärnten.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHydrozincite\" class=\"extiw\" title=\"en:Hydrozincite\">Hydrozincite\u003C\u002Fa> with \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHemimorphite\" class=\"extiw\" title=\"en:Hemimorphite\">Hemimorphite\u003C\u002Fa> - Locality: Bleiberg, Carinthia (Germany) - Exposed in the Mineralogical Museum, Bonn, Germany","Ra'ike (see also: de:Benutzer:Ra'ike)",1800,1400,{"id":678,"source_url":679,"license_code":609,"credit_html":680,"title":681,"description":682,"author":683,"original_width":684,"original_height":685},78516,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=128748298","Stephen E. Fritz, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=128748298\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Scholzite, Hemimorphite-235257.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FScholzite\" class=\"extiw\" title=\"en:Scholzite\">Scholzite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHemimorphite\" class=\"extiw\" title=\"en:Hemimorphite\">Hemimorphite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Reaphook Hill, Martins Well station, South Flinders Ranges, Flinders Ranges, South Australia, Australia\u003C\u002Fdd>\n\u003Cdd>\u003Ci>Original description:\u003C\u002Fi> Total specimen size approximately 8.5 cm with 1 cm - 1.5 cm scholzite needles\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Stephen E. Fritz",2397,1839,{"id":687,"source_url":688,"license_code":373,"credit_html":689,"title":690,"description":691,"author":544,"original_width":692,"original_height":693},85186,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10149120","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10149120\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphite-Veszelyite-168068.jpg","\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\u002FVeszelyite\" class=\"extiw\" title=\"en:Veszelyite\">Veszelyite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Laochang ore field (Laochang Mine), Eastern Sub-district, Gejiu Sn-polymetallic deposit, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGejiu_City\" class=\"extiw\" title=\"en:Gejiu City\">Gejiu County\u003C\u002Fa>, Honghe Autonomous Prefecture, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FYunnan\" class=\"extiw\" title=\"en:Yunnan\">Yunnan Province\u003C\u002Fa>, China (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-155491.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 5.5 x 3.6 x 1.8 cm.\u003C\u002Fdd>\n\u003Cdd>An exceptional and lovely specimen of beautiful lustrous robin's-egg blue Hemimorphite, overlaying a layer of vitreous deep blue Veszelyite. The Veszelyite is notable in its own right, but to have it in such an aesthetic combination with the Hemimorphite is quite remarkable. Small find of a few years ago. Ex. Charlie Key.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",499,330,{"id":695,"source_url":696,"license_code":373,"credit_html":697,"title":698,"description":691,"author":544,"original_width":699,"original_height":700},85187,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10149121","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10149121\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphite-Veszelyite-168070.jpg",500,340,{"id":702,"source_url":703,"license_code":373,"credit_html":704,"title":705,"description":706,"author":544,"original_width":545,"original_height":707},85188,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10157349","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10157349\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphite-Veszelyite-196857.jpg","\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\u002FVeszelyite\" class=\"extiw\" title=\"en:Veszelyite\">Veszelyite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Laochang ore field (Laochang Mine), Eastern Sub-district, Gejiu Sn-polymetallic deposit, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGejiu_City\" class=\"extiw\" title=\"en:Gejiu City\">Gejiu County\u003C\u002Fa>, Honghe Autonomous Prefecture, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FYunnan\" class=\"extiw\" title=\"en:Yunnan\">Yunnan Province\u003C\u002Fa>, China (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-155491.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 13.4 x 8.4 x 3.4 cm.\u003C\u002Fdd>\n\u003Cdd>This Wenshan hemimorphite is really special. The plate of botryoidal hemimorphite itself is a pretty shade of sky blue. But what makes it unique is that you can see on it a sprinkling of crystals of the rare hydrated copper zinc phosphate veszelyite (zinc is a component of both hemimorphite and veszelyite; veszelyite also has a copper component).\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",381,{"id":709,"source_url":710,"license_code":373,"credit_html":711,"title":712,"description":713,"author":544,"original_width":714,"original_height":715},85191,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10164204","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10164204\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hemimorphite-Veszelyite-233177.jpg","\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\u002FVeszelyite\" class=\"extiw\" title=\"en:Veszelyite\">Veszelyite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Laochang ore field (Laochang Mine), Eastern Sub-district, Gejiu Sn-polymetallic deposit, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGejiu_City\" class=\"extiw\" title=\"en:Gejiu City\">Gejiu County\u003C\u002Fa>, Honghe Autonomous Prefecture, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FYunnan\" class=\"extiw\" title=\"en:Yunnan\">Yunnan Province\u003C\u002Fa>, China (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-155491.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 12.5 x 9.8 x 3.2 cm.\u003C\u002Fdd>\n\u003Cdd>A unique and beautiful new find from China of vivid, powder-blue hemimorphite botryoids highlighted or outlined by preferential bands of blue veszelyite. The hemimorphite is translucent. Veszelyite is a rare phosphate. This find was recovered in 2008 and appeared at the 2008 Munich Show.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",714,750,{"id":717,"source_url":718,"license_code":373,"credit_html":719,"title":720,"description":721,"author":544,"original_width":715,"original_height":545},85192,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10165582","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10165582\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Veszelyite-Hemimorphite-240710.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FVeszelyite\" class=\"extiw\" title=\"en:Veszelyite\">Veszelyite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHemimorphite\" class=\"extiw\" title=\"en:Hemimorphite\">Hemimorphite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Laochang ore field (Laochang Mine), Eastern Sub-district, Gejiu Sn-polymetallic deposit, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGejiu_City\" class=\"extiw\" title=\"en:Gejiu City\">Gejiu County\u003C\u002Fa>, Honghe Autonomous Prefecture, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FYunnan\" class=\"extiw\" title=\"en:Yunnan\">Yunnan Province\u003C\u002Fa>, China (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-155491.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 6.5 x 4.7 x 3.3 cm.\u003C\u002Fdd>\n\u003Cdd>Veszelyite is a rare phosphate and this beautiful, multi-hued blue specimen of botryoidal hemimorphite is richly sprinkled with sharp, dark blue veszelyite crystals. The hemimorphite ranges from powder-blue to cobalt-blue and the isolated, powder-blue botryoid on the cobalt-blue is indeed, striking. These were very popular at the 2008 Munich Show.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",{"id":723,"source_url":724,"license_code":609,"credit_html":725,"title":726,"description":727,"author":728,"original_width":729,"original_height":730},85204,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=35708516","John Sobolewski (JSS), via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=35708516\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Veszelyite, Hemimorphite-171526.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FVeszelyite\" class=\"extiw\" title=\"en:Veszelyite\">Veszelyite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHemimorphite\" class=\"extiw\" title=\"en:Hemimorphite\">Hemimorphite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Laochang ore field (Laochang Mine), Gejiu Sn-polymetallic ore field, Gejiu Co., Honghe Autonomous Prefecture, Yunnan Province, China\u003C\u002Fdd>\n\u003Cdd>\u003Ci>Original description:\u003C\u002Fi> A 3.7 by 2.4 cms specimen with one small dark blue Veszelyite crystal on the surface with many others included in but barely visible in the translucent lighter blue Hemimorphite. JSS specimen and photograph.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","John Sobolewski (JSS)",640,480,[732,738,744,748],{"id":733,"url":734,"label":735,"formula":736,"spacegroup":737,"year":313},6058,"\u002Fcif\u002F6058.cif","Libowitzky 1997","Zn4 Si2 O9 H2","I m m 2",{"id":739,"url":740,"label":741,"formula":742,"spacegroup":737,"year":743},6060,"\u002Fcif\u002F6060.cif","Hill 1977","Zn2 Si O5 H2",1977,{"id":745,"url":746,"label":747,"formula":742,"spacegroup":737,"year":295},6061,"\u002Fcif\u002F6061.cif","McDonald 1967",{"id":749,"url":750,"label":751,"formula":752,"spacegroup":737,"year":275},6063,"\u002Fcif\u002F6063.cif","Ito 1932","Si Zn2 O5",[754,755,756,757,758,759,760,761,762,763,764,765,766,767,768,769],"Calamina","Daviesit","Daviesita","Electric Calamine","Gemeiner Galmei","Hemimorphita","Kieselgalmei","Kieselgalmey","Kieselzinkerz","Kieselzinkspat","Smithsonite (of Brooke and Miller)","Wagit","Wagita","Wagite","Zinkglas","Zinkkieselerz",[771,775,779,783,787,791,795,799,802,806,809,813,817,825,829,835,839,844,848,852,855,859,863,868,871,875,879,883,887,890,895,898],{"lang":772,"names":773},"af",[774],"Hemimorfiet",{"lang":776,"names":777},"ar",[778],"هيميمورفيت",{"lang":780,"names":781},"be",[782],"Гемімарфіт",{"lang":784,"names":785},"bs",[786],"hemimorfit",{"lang":788,"names":789},"ca",[790],"hemimorfita",{"lang":792,"names":793},"de",[794,762],"Hemimorphit",{"lang":796,"names":797},"el",[798],"Ημιμορφίτης",{"lang":800,"names":801},"es",[790],{"lang":803,"names":804},"et",[805],"hemimorfiit",{"lang":807,"names":808},"eu",[790],{"lang":810,"names":811},"fa",[812],"همی مورفیت",{"lang":814,"names":815},"fi",[816],"Hemimorfiitti",{"lang":818,"names":819},"fr",[820,821,822,823,767,824],"E557","hémimorphite","Oxyde de zinc silicifère","Silicate de zinc","Zinc oxydé silicifère",{"lang":826,"names":827},"gl",[828],"Hemimorfita",{"lang":830,"names":831},"he",[832,833,820,834],"E 557","E-557","המימורפיט",{"lang":836,"names":837},"it",[838],"emimorfite",{"lang":840,"names":841},"ja",[842,843],"ヘミモルファイト","異極鉱",{"lang":845,"names":846},"nb",[847],"hemimorfitt",{"lang":849,"names":850},"nl",[851],"hemimorfiet",{"lang":853,"names":854},"nn",[847],{"lang":856,"names":857},"pl",[390,858],"Kalamin",{"lang":860,"names":861},"pt",[790,862],"Hemimorfite",{"lang":864,"names":865},"ru",[866,867],"Гемиморфит","Каламин",{"lang":869,"names":870},"sl",[786],{"lang":872,"names":873},"sr",[390,874],"хемиморфит",{"lang":876,"names":877},"sv",[786,878],"kiselgalmeja",{"lang":880,"names":881},"uk",[882],"Геміморфіт",{"lang":884,"names":885},"uz",[886],"Gemimorfit",{"lang":888,"names":889},"vi",[794],{"lang":891,"names":892},"zh",[893,894],"异极矿","異極礦",{"lang":896,"names":897},"zh-cn",[893],{"lang":899,"names":900},"zh-hant",[894],"Q408008",{"history":903,"applications":907},{"markdown":904,"model_version":905,"prompt_version":906,"reviewed_at":11},"For most of mineralogy's history, hemimorphite did not have its own name. It hid inside an older word: **calamine**.\n\nCalamine came from the Latin *lapis calaminaris*, itself a corruption of the Greek *kadmia* — the ancient catch-all term for zinc ores[1]. Miners and metalworkers had used the word for centuries to describe the pale, often botryoidal masses they smelted for zinc and brass. The trouble was that two different minerals answered to the name. Both formed in the weathered upper levels of zinc deposits. Both looked, in hand specimen, much the same. One worked beautifully as a zinc ore. The other did not[2].\n\nThe puzzle was settled in 1803, when the British chemist and mineralogist James Smithson took the question into the laboratory[3]. He showed that calamine was in fact a mixture of two distinct compounds — a zinc carbonate, which yielded zinc readily, and a zinc silicate, which did not[3]. The carbonate would later be named **smithsonite** in his honour, after his death in 1829[3].\n\nThe silicate — what we now call hemimorphite — kept the old calamine name for another fifty years.\n\nIt received its modern name in 1853, from the mineralogist Adolph Kenngott[4]. He coined **hemimorphite** from the Greek *hēmi* (half) and *morphē* (form), in reference to a quirk of the mineral's crystal symmetry[5]. The crystals are *hemimorphic* — meaning the two ends of a crystal develop differently, one terminated by a blunt face, the other by a sharp pyramid. Only a handful of mineral species do this, and the asymmetry is the species' defining structural feature[5].\n\nFor more than a century after Kenngott's paper, English and European literature kept using **calamine** and **hemimorphite** interchangeably. The International Mineralogical Association finally settled the matter in 1962, formally choosing *hemimorphite* over *calamine* as the species name[4]. *Calamine* survives today only in pharmacy — the pink **calamine lotion** sold for skin irritations is a mixture of zinc oxide and iron oxide[1].","claude-opus-4-7","1.7.0",{"markdown":908,"model_version":905,"prompt_version":906,"reviewed_at":11},"Hemimorphite is, first and foremost, a secondary ore of zinc — a supplemental source, not a primary one[1]. Roughly half its weight is zinc; published figures put the metal content at up to 54%[2]. The mineral forms where primary zinc sulfide ore — chiefly **sphalerite** (ZnS) — has been weathered or chemically altered near the surface[2][3]. That alteration leaves a band of oxidised zinc minerals capping the unweathered sulfide body below. Most modern zinc comes from sphalerite at depth; hemimorphite is mined where the oxidised upper layer is rich enough to recover[4].\n\nThe other practical use is lapidary. The blue-to-blue-green **botryoidal** variety — bunched, grape-cluster aggregates with a milky pastel colour reminiscent of turquoise — is cut into cabochons, beads, pendants, and earrings[5]. The best of this material has come from the **Wenshan Mine** in Yunnan, China, and from the **Ojuela Mine** in Durango, Mexico[5]. Working it is delicate. The mineral has perfect cleavage and a Mohs hardness of only 4½ to 5[5]. Jewellers therefore reserve it for pieces that will not see hard knocks — pendants and earrings, rarely rings.\n\nBeyond zinc recovery and ornament, the mineral has no significant industrial role. It is sought by collectors for well-formed transparent crystals and for the blue botryoidal pieces, and otherwise lives in the secondary literature on oxidised zinc deposits."]