[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:905":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":22,"key_elements":23,"impurities":11,"cim":24,"ima_status":25,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":28,"discovery_year":29,"strunz10ed1":30,"strunz10ed2":31,"strunz10ed3":21,"strunz10ed4":32,"dana8ed1":33,"dana8ed2":34,"dana8ed3":35,"dana8ed4":36,"csystem":37,"cclass":38,"spacegroup":39,"spacegroupset":40,"a":41,"b":42,"c":43,"alpha":40,"beta":40,"gamma":40,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":38,"csmetamict":14,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":44,"tlform":11,"hmin":45,"hmax":45,"hardtype":11,"vhnmin":40,"vhnmax":40,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":46,"dmeas2":47,"dcalc":48,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":49,"commentluster":50,"diapheny":51,"streak":52,"colour":53,"commentcolor":11,"colors":54,"streak_colors":58,"luminescence":11,"uv":11,"cleavage":59,"cleavagetype":60,"fracturetype":11,"tenacity":61,"commentbreak":11,"opticaltype":62,"opticalsign":63,"opticalalpha":64,"opticalalpha2":65,"opticalalphaerror":11,"opticalbeta":64,"opticalbeta2":65,"opticalbetaerror":11,"opticalgamma":66,"opticalgamma2":67,"opticalgammaerror":11,"opticalomega":40,"opticalomega2":40,"opticalomegaerror":11,"opticalepsilon":40,"opticalepsilon2":40,"opticalepsilonerror":11,"opticaln":40,"opticaln2":40,"opticalnerror":11,"optical2vcalc":40,"optical2vcalc2":40,"optical2vcalcerror":11,"optical2vmeasured":40,"optical2vmeasured2":40,"optical2vmeasurederror":11,"rimin":68,"rimax":69,"opticaldispersion":70,"opticalpleochroism":71,"opticalpleochorismdesc":72,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":73,"opticalr":11,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":74,"industrial":11,"occurrence":11,"otheroccurrence":11,"type_specimen_store":75,"description_short":76,"aboutname":77,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":78,"reviewed_at":11,"variety_of":11,"varieties":79,"group_members":80,"associates":91,"confused_with":187,"type_localities":193,"occurrence_total":200,"citations":201,"images":261,"structures":358,"synonyms":375,"language_names":381,"wikidata_qid":427,"texts":428},905,"1:1:905:2","62267a57-dc1b-4c57-bf52-654c15b32f09","Carminite","Cmt",0,"mineral",null,46587,10811,false,"PbFe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>(AsO\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>",[17,18,19,20,21],"As","Fe","Pb","O","H",[17,18,19,20,21],[17,19],"20.5.12",[26,27],"APPROVED","GRANDFATHERED",1850,"1850","8","B","30","41","10","6","1","Orthorhombic",8,48,"0","16.591","7.58","12.285","Crystals lath-like, flattened on {010}, elongated [001] and exhibiting {010}, {110}, {011} plus other forms. As needle-like crystals; tufted or spherical aggregates; fibrous, drusy, massive.",3.5,"5.03","5.18","5.405","Vitreous,Pearly","Lustre pearly on cleavages.","Translucent","Reddish yellow","Carmine-red, terra cotta-red, reddish brown; red in transmitted light.",[55,56,57],"red","brown","yellow",[55,57],"On {110}, distinct.","Distinct\u002FGood","brittle","Biaxial","+","2.05","2.07","2.06","2.08",2.05,2.08,"r \u003C v strong","Visible","X = Light yellowish red\r\nY = Dark carmine-red\r\nZ = Dark carmine-red","X = c; Y = a; Z = b.","Slowly soluble in HCl with the separation of PbCl2 and totally soluble in HNO3.","No defined type material.","The lead analogue of Sewardite. The orthorhombic dimorph of Mawbyite.\r\n\r\nA rare secondary mineral formed as an alteration product of (mainly) arsenopyrite in the oxidized zones of lead-bearing deposits.\r\nStructurally related to palermoite.\r\n\r\nMay be co...","First description by F. Sandberger (1850, in German), in which he named the mineral \"Carminspath\", after its carmine-red color. \r\nThe German name was anglicised to \"carminite\" by J. Dana in his 4th System of Mineralogy (1854).\r\n","2025-08-11 12:14:19",[],[81,86],{"id":82,"name":83,"entrytype":9,"csystem":37,"ima_formula":84,"mindat_formula":84,"hmin":45,"hmax":45,"dmeas":11,"dcalc":85,"primary_image_id":11},46570,"Crimsonite","PbFe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>","5.180 ",{"id":87,"name":88,"entrytype":9,"csystem":37,"ima_formula":89,"mindat_formula":89,"hmin":45,"hmax":45,"dmeas":40,"dcalc":90,"primary_image_id":11},11128,"Sewardite","CaFe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>(AsO\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>","4.156",[92,102,112,120,128,136,143,152,161,170,178],{"id":93,"name":94,"entrytype":9,"csystem":37,"ima_formula":95,"mindat_formula":96,"hmin":97,"hmax":98,"dmeas":99,"dcalc":100,"primary_image_id":101},233,"Anglesite","Pb(SO\u003Csub>4\u003C\u002Fsub>)","PbSO\u003Csub>4\u003C\u002Fsub>",2.5,3,"6.37","6.36",1430,{"id":103,"name":104,"entrytype":9,"csystem":105,"ima_formula":106,"mindat_formula":107,"hmin":108,"hmax":108,"dmeas":109,"dcalc":110,"primary_image_id":111},360,"Arseniosiderite","Monoclinic","Ca\u003Csub>2\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>O\u003Csub>2\u003C\u002Fsub>(AsO\u003Csub>4\u003C\u002Fsub>)\u003Csub>3\u003C\u002Fsub> · 3H\u003Csub>2\u003C\u002Fsub>O","Ca\u003Csub>2\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>(AsO\u003Csub>4\u003C\u002Fsub>)\u003Csub>3\u003C\u002Fsub>O\u003Csub>2\u003C\u002Fsub>·3H\u003Csub>2\u003C\u002Fsub>O",4.5,"3.58","3.78",2032,{"id":113,"name":114,"entrytype":9,"csystem":105,"ima_formula":115,"mindat_formula":116,"hmin":108,"hmax":108,"dmeas":117,"dcalc":118,"primary_image_id":119},581,"Bayldonite","Cu\u003Csub>3\u003C\u002Fsub>PbO(AsO\u003Csub>3\u003C\u002Fsub>OH)\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>","PbCu\u003Csub>3\u003C\u002Fsub>(AsO\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>","5.24","5.707",2902,{"id":121,"name":122,"entrytype":9,"csystem":123,"ima_formula":124,"mindat_formula":124,"hmin":45,"hmax":108,"dmeas":125,"dcalc":126,"primary_image_id":127},652,"Beudantite","Trigonal","PbFe\u003Csup>3+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>(AsO\u003Csub>4\u003C\u002Fsub>)(SO\u003Csub>4\u003C\u002Fsub>)(OH)\u003Csub>6\u003C\u002Fsub>","4.48","4.49",3210,{"id":129,"name":130,"entrytype":9,"csystem":37,"ima_formula":131,"mindat_formula":132,"hmin":98,"hmax":45,"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":123,"ima_formula":139,"mindat_formula":139,"hmin":45,"hmax":45,"dmeas":140,"dcalc":141,"primary_image_id":142},1334,"Dussertite","BaFe\u003Csup>3+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>(AsO\u003Csub>4\u003C\u002Fsub>)(AsO\u003Csub>3\u003C\u002Fsub>OH)(OH)\u003Csub>6\u003C\u002Fsub>","3.75","4.09",7514,{"id":144,"name":145,"entrytype":9,"csystem":146,"ima_formula":147,"mindat_formula":147,"hmin":45,"hmax":148,"dmeas":149,"dcalc":150,"primary_image_id":151},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":153,"name":154,"entrytype":9,"csystem":155,"ima_formula":156,"mindat_formula":157,"hmin":97,"hmax":97,"dmeas":158,"dcalc":159,"primary_image_id":160},3185,"Pharmacosiderite","Isometric","KFe\u003Csup>3+\u003C\u002Fsup>\u003Csub>4\u003C\u002Fsub>(AsO\u003Csub>4\u003C\u002Fsub>)\u003Csub>3\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub> · 6-7H\u003Csub>2\u003C\u002Fsub>O","KFe\u003Csup>3+\u003C\u002Fsup>\u003Csub>4\u003C\u002Fsub>(AsO\u003Csub>4\u003C\u002Fsub>)\u003Csub>3\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub>·6-7H\u003Csub>2\u003C\u002Fsub>O","2.797","2.90",19220,{"id":162,"name":163,"entrytype":9,"csystem":123,"ima_formula":164,"mindat_formula":164,"hmin":165,"hmax":166,"dmeas":167,"dcalc":168,"primary_image_id":169},3248,"Plumbojarosite","Pb\u003Csub>0.5\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>6\u003C\u002Fsub>",1.5,2,"3.665","3.71",19645,{"id":171,"name":172,"entrytype":9,"csystem":37,"ima_formula":173,"mindat_formula":174,"hmin":45,"hmax":148,"dmeas":175,"dcalc":176,"primary_image_id":177},3595,"Scorodite","Fe\u003Csup>3+\u003C\u002Fsup>(AsO\u003Csub>4\u003C\u002Fsub>) · 2H\u003Csub>2\u003C\u002Fsub>O","Fe\u003Csup>3+\u003C\u002Fsup>AsO\u003Csub>4\u003C\u002Fsub>·2H\u003Csub>2\u003C\u002Fsub>O","3.27","3.276",21915,{"id":179,"name":180,"entrytype":9,"csystem":181,"ima_formula":182,"mindat_formula":183,"hmin":97,"hmax":98,"dmeas":184,"dcalc":185,"primary_image_id":186},4322,"Wulfenite","Tetragonal","PbMoO\u003Csub>4\u003C\u002Fsub>","Pb(MoO\u003Csub>4\u003C\u002Fsub>)","6.5","6.88",30992,[188],{"id":189,"name":190,"entrytype":9,"csystem":105,"ima_formula":15,"mindat_formula":15,"hmin":148,"hmax":148,"dmeas":40,"dcalc":191,"primary_image_id":192},2603,"Mawbyite","5.365",15661,[194],{"id":195,"txt":196,"latitude":197,"longitude":198,"country":199},1869,"Louise Mine, Bürdenbach, Altenkirchen-Flammersfeld, Altenkirchen, Rhineland-Palatinate, Germany",50.6053511,7.5105925,"Germany",198,[202,205,209,213,218,223,227,231,235,239,244,248,252,257],{"id":203,"year":28,"html":204,"doi":11},16104724,"von Sandberger (1850) Carminspath, ein neues mineral aus der Ordnung der Arseniate. Annalen der Physik und Chemie (Poggendorff), Halle, Leipzig: 80: 391-392 (as Carminspath).",{"id":206,"year":207,"html":208,"doi":11},1118641,1854,"Dana, James D. (1854) \u003Ci>A System of Mineralogy\u003C\u002Fi> (4th ed.). p.1-849.",{"id":210,"year":211,"html":212,"doi":11},15933555,1858,"von Sandberger (1858) Ueber den Carminspath. Annalen der Physik und Chemie (Poggendorff), Halle, Leipzig: 103: 345 (as Carminspath).",{"id":214,"year":215,"html":216,"doi":217},4804,1910,"Russell, Arthur (1910) On the occurrence of the rare mineral Carminite in Cornwall. \u003Ci>Mineralogical Magazine and Journal of the Mineralogical Society\u003C\u002Fi>,  15 (71) 285-287 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1910.015.71.03'>doi:10.1180\u002Fminmag.1910.015.71.03\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_15\u002F15-71-285.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1910.015.71.03",{"id":219,"year":220,"html":221,"doi":222},653692,1934,"Larsen, E.S.; Berman, H. (1934) The microscopic determination of the nonopaque minerals. \u003Ci>Bulletin of the US Geological Survey\u003C\u002Fi> Vol. 848. US Geological Survey p.1-266. \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3133\u002Fb848'>doi:10.3133\u002Fb848\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fpubs.usgs.gov\u002Fbul\u002F0848\u002Freport.pdf?reftype=.pdf' class='refpdflink'>\u003C\u002Fa>","10.3133\u002Fb848",{"id":224,"year":225,"html":226,"doi":11},520604,1937,"Foshag, W. F. (1937) Carminite and associated minerals from Mapimi, Mexico. \u003Ci>American Mineralogist\u003C\u002Fi>,  22 (5) 479-484 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM22\u002FAM22_479.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":228,"year":229,"html":230,"doi":11},16103221,1939,"Le Mesurier (1939) Journal of the Royal Society of Western Australia: 25: 137.",{"id":232,"year":233,"html":234,"doi":11},1118652,1951,"Palache, Charles; Berman, Harry; Frondel, Clifford (1951) \u003Ci>The System of Mineralogy\u003C\u002Fi> (7th ed.) Vol. 2 - Halides, Nitrates, Borates, Carbonates, Sulfates, Phosphates, Arsenates, Tungstates, Molybdates, Etc. John Wiley and Sons.",{"id":236,"year":237,"html":238,"doi":11},523221,1959,"Rosenzweig, Abraham, Finney, Joseph J. (1959) Unit cell of carminite. \u003Ci>American Mineralogist\u003C\u002Fi>,  44 (5-6) 663-665 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM44\u002FAM44_663.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":240,"year":241,"html":242,"doi":243},5561,1960,"Kingsbury, Arthur W. G., Hartley, J. (1960) Carminite and beudantite from the northern part of the Lake District and from Cornwall. \u003Ci>Mineralogical Magazine and Journal of the Mineralogical Society\u003C\u002Fi>,  32 (249) 423-432 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1960.032.249.01'>doi:10.1180\u002Fminmag.1960.032.249.01\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_32\u002F32-249-423.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1960.032.249.01",{"id":245,"year":246,"html":247,"doi":11},526470,1975,"Moore, Paul B., Araki, Takaharu (1975) Palermoite, SrLi\u003Csub>2\u003C\u002Fsub>[Al\u003Csub>4\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>4\u003C\u002Fsub>]: Its atomic arrangement and relationship to carminite, Pb\u003Csub>2\u003C\u002Fsub>[Fe\u003Csub>4\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub>(AsO\u003Csub>4\u003C\u002Fsub>)\u003Csub>4\u003C\u002Fsub>]. \u003Ci>American Mineralogist\u003C\u002Fi>,  60 (5-6) 460-465 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM60\u002FAM60_460.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":249,"year":250,"html":251,"doi":11},16104732,1995,"Olmi, F. and Sabelli, C. (1995) Carminite from three localities of Sardinia (Italy). Crystal structure refinements. Neues Jahrb. Mineral., Monatsh., 553–562.",{"id":253,"year":254,"html":255,"doi":256},99,1996,"Kharisun, Taylor, Max R., Bevan, D. J. M, Pring, Allan (1996) The crystal structure of carminite: refinement and bond valence calculations. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  60 (402). 805-811 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1996.060.402.11'>doi:10.1180\u002Fminmag.1996.060.402.11\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_60\u002F60-402-805.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1996.060.402.11",{"id":258,"year":259,"html":260,"doi":11},16963534,2005,"(2005) Carminite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fcarminite.pdf' class='refpdflink'>\u003C\u002Fa>",[262,269,279,284,291,295,302,312,320,326,331,338,348],{"id":263,"source_url":264,"license_code":265,"credit_html":266,"title":7,"description":11,"author":11,"original_width":267,"original_height":268},29377,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F167328","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\u002F167328\" rel=\"noopener\">University of Tartu, Natural History Museum\u003C\u002Fa> via Europeana",1000,750,{"id":270,"source_url":271,"license_code":272,"credit_html":273,"title":274,"description":275,"author":276,"original_width":277,"original_height":278},4751,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14865785","CC BY-SA 3.0","Christian Rewitzer, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14865785\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Carminite-170209.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCarminite\" class=\"extiw\" title=\"en:Carminite\">Carminite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Alto das Quelhas do Gestoso Mines, Gestoso, Manhouce, São Pedro do Sul, Viseu District, Portugal\u003C\u002Fdd>\n\u003Cdd>Picture width 1.5 mm. Collection and photograph Christian Rewitzer\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Christian Rewitzer",800,727,{"id":280,"source_url":281,"license_code":265,"credit_html":282,"title":7,"description":11,"author":11,"original_width":283,"original_height":267},29378,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F167331","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby-sa\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F167331\" rel=\"noopener\">University of Tartu, Natural History Museum\u003C\u002Fa> via Europeana",984,{"id":285,"source_url":286,"license_code":272,"credit_html":287,"title":288,"description":289,"author":276,"original_width":277,"original_height":290},4752,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14865787","Christian Rewitzer, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14865787\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Carminite-170210.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCarminite\" class=\"extiw\" title=\"en:Carminite\">Carminite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Alto das Quelhas do Gestoso Mines, Gestoso, Manhouce, São Pedro do Sul, Viseu District, Portugal\u003C\u002Fdd>\n\u003Cdd>Picture width 8 mm. Collection and photograph Christian Rewitzer  This Photo was Mindat.org Photo of the Day - 30th Oct 2008\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",669,{"id":292,"source_url":293,"license_code":265,"credit_html":294,"title":7,"description":11,"author":11,"original_width":267,"original_height":268},29379,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F167274","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby-sa\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F167274\" rel=\"noopener\">University of Tartu, Natural History Museum\u003C\u002Fa> via Europeana",{"id":296,"source_url":297,"license_code":272,"credit_html":298,"title":299,"description":300,"author":276,"original_width":277,"original_height":301},4753,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14865788","Christian Rewitzer, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14865788\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Carminite-170211.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCarminite\" class=\"extiw\" title=\"en:Carminite\">Carminite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Alto das Quelhas do Gestoso Mines, Gestoso, Manhouce, São Pedro do Sul, Viseu District, Portugal\u003C\u002Fdd>\n\u003Cdd>Picture width 1.5 mm. Collection and photograph Christian Rewitzer  This Photo was Mindat.org Photo of the Day - 26th Apr 2009\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",753,{"id":303,"source_url":304,"license_code":305,"credit_html":306,"title":307,"description":308,"author":309,"original_width":310,"original_height":311},4756,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118189935","CC BY-SA 2.0","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118189935\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Carminite (48293952937).jpg","\u003Cp>Ojuela Mine - Mapimi\n\u003C\u002Fp>\nDurango, Mexico","Pacific Museum of Earth from Canada",4000,6000,{"id":313,"source_url":314,"license_code":315,"credit_html":316,"title":317,"description":318,"author":319,"original_width":277,"original_height":277},1818,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=1955909","Public domain","Dave Dyet http:\u002F\u002Fwww.shutterstone.com http:\u002F\u002Fwww.dyet.com, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=1955909\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Argentojarosite 2 w- carminite arseniosiderite and quartz Basic silver iron sulfate Santa Ana Sonora Mexico 2030.jpg","These mineral images are free to use how you wish.","Dave Dyet http:\u002F\u002Fwww.shutterstone.com http:\u002F\u002Fwww.dyet.com",{"id":321,"source_url":322,"license_code":315,"credit_html":323,"title":324,"description":318,"author":319,"original_width":325,"original_height":325},2029,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=1955916","Dave Dyet http:\u002F\u002Fwww.shutterstone.com http:\u002F\u002Fwww.dyet.com, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=1955916\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Arseniosiderite w- carminite Hydrous basic calcium arsenate Mina Ojuela Mapimi Durango Mexico 2096.jpg",700,{"id":327,"source_url":328,"license_code":315,"credit_html":329,"title":330,"description":318,"author":319,"original_width":277,"original_height":277},1819,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=1955910","Dave Dyet http:\u002F\u002Fwww.shutterstone.com http:\u002F\u002Fwww.dyet.com, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=1955910\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Argentojarosite w- carminite arseniosiderite and quartz Basic silver iron sulfate Santa Ana Sonora Mexico 2030.jpg",{"id":332,"source_url":333,"license_code":272,"credit_html":334,"title":335,"description":336,"author":276,"original_width":277,"original_height":337},4754,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14865807","Christian Rewitzer, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14865807\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Scorodite-Carminite-170220.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FScorodite\" class=\"extiw\" title=\"en:Scorodite\">Scorodite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCarminite\" class=\"extiw\" title=\"en:Carminite\">Carminite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Alto das Quelhas do Gestoso Mines, Gestoso, Manhouce, São Pedro do Sul, Viseu District, Portugal\u003C\u002Fdd>\n\u003Cdd>Picture width 3 mm. Collection and photograph Christian Rewitzer Blue Scorodite xls on redbrown Carminite.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",919,{"id":339,"source_url":340,"license_code":341,"credit_html":342,"title":343,"description":344,"author":345,"original_width":346,"original_height":347},4755,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=27539060","CC BY 3.0","Juan Manuel Garriga, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=27539060\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Carminite, Mimetite-191240.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCarminite\" class=\"extiw\" title=\"en:Carminite\">Carminite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMimetite\" class=\"extiw\" title=\"en:Mimetite\">Mimetite\u003C\u002Fa> (View size: 5x5 mm) \n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Le Mazet vein, Échassières, Ébreuil, Allier, Auvergne, France\u003C\u002Fdd>\n\u003Cdd>A little vug with yellow mimetite and red-brownish acicular Carminite\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Juan Manuel Garriga",1024,683,{"id":349,"source_url":350,"license_code":351,"credit_html":352,"title":353,"description":354,"author":355,"original_width":356,"original_height":357},4757,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163484450","CC0 1.0","Nessa Eull, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163484450\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Carminite with corkite (GeoDIL number - 1598).jpg","Carminite, PbFe3+2(AsO4)2(OH)2 (lead iron hydroxy arsenate), was only recognized as a separate mineral in the last fifty years. Before that it was often seen in lead mining wastes around the Luise Mining plant in Nassau, but there was never enough material for unambiguous identification. However, some years later it was “re-discovered” in much greater quantities in the form of crystalline deposits in Mexico that enabled more in-depth analysis. The name was given because of vivid red coloration of the crystals.","Nessa Eull",2662,1735,[359,365,369],{"id":360,"url":361,"label":362,"formula":363,"spacegroup":364,"year":254},2301,"\u002Fcif\u002F2301.cif","Kharisun 1996","Pb Fe2 As2 O10 H2","C c c m",{"id":366,"url":367,"label":368,"formula":363,"spacegroup":364,"year":250},2302,"\u002Fcif\u002F2302.cif","Olmi 1995",{"id":370,"url":371,"label":372,"formula":373,"spacegroup":364,"year":374},2305,"\u002Fcif\u002F2305.cif","Finney 1963","Pb As2 Fe2 O10 H2",1963,[376,377,378,379,380],"Carmine Spar","Carminiet","Carminit","Carminspath","Karminspat",[382,386,390,394,398,402,405,408,412,416,419,423],{"lang":383,"names":384},"ca",[385],"carminita",{"lang":387,"names":388},"de",[389],"Karminit",{"lang":391,"names":392},"el",[393],"Καρμινίτης",{"lang":395,"names":396},"es",[397],"Carminita",{"lang":399,"names":400},"et",[401],"karminiit",{"lang":403,"names":404},"eu",[397],{"lang":406,"names":407},"fr",[7],{"lang":409,"names":410},"it",[411],"carminite",{"lang":413,"names":414},"mn",[415],"Карминят",{"lang":417,"names":418},"pl",[389],{"lang":420,"names":421},"ru",[422],"Карминит",{"lang":424,"names":425},"uk",[426],"Кармініт","Q3660390",{"history":429,"applications":433},{"markdown":430,"model_version":431,"prompt_version":432,"reviewed_at":11},"The name says exactly what the eye sees. Carminite is a deep carmine red — the rich crimson of the cochineal dye called *carmine* — and it was the colour, not a person, that earned the mineral its name.\n\nThe German mineralogist Fritz Sandberger first described it in 1850. He called it *Carminspath*, joining the colour word *carmine* to *spath*, the old German term for a crystalline, easily split mineral[1]. The crystals he studied formed clusters of fine needles, carmine to tile red, and stay red even when light passes through them[2].\n\nA few years later the name crossed into English. The American mineralogist James Dwight Dana anglicised *Carminspath* to *carminite* in the fourth edition of his *System of Mineralogy*, published in 1854[3]. The shortened, Latin-suffixed form is the one still in use.\n\nCarminite is a rare secondary mineral — one that forms not when rock first crystallises but later, as earlier minerals break down near the surface. It appears where arsenopyrite, an iron arsenic sulfide, weathers in the oxidised upper zones of some lead-bearing ore deposits[4]. The original specimens came from the Louise Mine at Bürdenbach, in the Rhineland-Palatinate region of Germany, the locality that defines the species[5].","claude-opus-4-8","1.7.0",{"markdown":434,"model_version":431,"prompt_version":432,"reviewed_at":11},"Carminite has no industrial use. It is far too rare to mine, and its mix of lead, iron, and arsenic offers nothing that cheaper, more abundant minerals do not supply better.\n\nWhat value it has is to people who study and collect minerals. Its deep carmine-red needles make it a prized specimen, and as a rare secondary arsenate it draws interest from researchers describing the minerals that form when arsenic-bearing ores weather[1]."]