[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:1304":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":16,"ima_formula":15,"elements":17,"sigelements":22,"key_elements":11,"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":35,"csystem":36,"cclass":37,"spacegroup":38,"spacegroupset":39,"a":40,"b":41,"c":42,"alpha":41,"beta":41,"gamma":41,"aerror":43,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":44,"csmetamict":14,"commentcrystal":11,"twinning":45,"tranglide":46,"parting":47,"epitaxidescription":48,"morphology":49,"tlform":11,"hmin":50,"hmax":51,"hardtype":44,"vhnmin":41,"vhnmax":41,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":52,"dmeas2":53,"dcalc":54,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":55,"lustretype":56,"commentluster":57,"diapheny":58,"streak":59,"colour":60,"commentcolor":11,"colors":61,"streak_colors":68,"luminescence":69,"uv":70,"cleavage":71,"cleavagetype":72,"fracturetype":73,"tenacity":74,"commentbreak":11,"opticaltype":75,"opticalsign":76,"opticalalpha":41,"opticalalpha2":41,"opticalalphaerror":11,"opticalbeta":41,"opticalbeta2":41,"opticalbetaerror":11,"opticalgamma":41,"opticalgamma2":41,"opticalgammaerror":11,"opticalomega":77,"opticalomega2":78,"opticalomegaerror":11,"opticalepsilon":79,"opticalepsilon2":80,"opticalepsilonerror":11,"opticaln":41,"opticaln2":41,"opticalnerror":11,"optical2vcalc":41,"optical2vcalc2":41,"optical2vcalcerror":11,"optical2vmeasured":41,"optical2vmeasured2":41,"optical2vmeasurederror":11,"rimin":81,"rimax":82,"opticaldispersion":11,"opticalpleochroism":11,"opticalpleochorismdesc":11,"opticalbirefringence":83,"opticalcomments":84,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":85,"opticalr":11,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":86,"industrial":87,"occurrence":11,"otheroccurrence":88,"type_specimen_store":11,"description_short":89,"aboutname":90,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":91,"reviewed_at":11,"variety_of":11,"varieties":92,"group_members":125,"associates":158,"confused_with":495,"type_localities":504,"occurrence_total":505,"citations":506,"images":734,"structures":1176,"synonyms":1204,"language_names":1241,"wikidata_qid":1598,"texts":1599},1304,"1:1:1304:4","7c373532-152c-4b15-80f0-df4832a3831f","Dolomite","Dol",0,"mineral",null,29288,122832,false,"CaMg(CO\u003Csub>3\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>","Ca can exist in excess of up to 0.25 apfu in non-stoichiometric dolomite (Nascimento dos Santos et al., 2017). See also Chai et al. (1995) and Drits et al. (2005).",[18,19,20,21],"Ca","Mg","O","C",[18,19,20,21],",Fe,Mn,Co,Pb,Zn,,","11.4.6",[26,27],"APPROVED","GRANDFATHERED","1791","5","A","B","10","14","2","1","Trigonal",10,80,"R-3","4.8012","0","16.002",1,3,"On {0001}, common with re-entrant angles around the middle edges; on \u003Cmi>{10_10}\u003C\u002Fmi> common; on \u003Cmi>{11_20}\u003C\u002Fmi>, common, as complementary twins simulating holohedral symmetry; also as double twins by combination of this law and twins on \u003Cmi>{10_10}\u003C\u002Fmi> or {0001}. On \u003Cmi>{10_11}\u003C\u002Fmi>, rare. On \u003Cmi>{02_21}\u003C\u002Fmi> as lamellae, especially in grains of dolomite marble.","translation gliding with T{0001}, t\u003Cmi>[10_10]\u003C\u002Fmi>.","Noted in lamellar twins on \u003Cmi>{02_21}\u003C\u002Fmi>. Twin gliding on \u003Cmi>{02_21}\u003C\u002Fmi>;","Growths of dolomite on calcite or vice versa, with parallel axes; also dolomite on rhodochrosite or siderite. Also occurs in oriented growths with antigorite (uncertain), and with chlorite [{0001} and {001} parallel].","Crystals typically rhombohedral with \u003Cmi>{10_11}\u003C\u002Fmi> or \u003Cmi>{40_41}\u003C\u002Fmi> dominant, may also be prismatic \u003Cmi>{11_20}\u003C\u002Fmi> terminated by rhombohedral faces; tabular {0001} with \u003Cmi>{11_20}\u003C\u002Fmi>; \u003Cmi>{10_11}\u003C\u002Fmi> often striated horizontally or curved - \"saddle\" or \"fingernail\" habit.  Also massive, coarse to fine granular, fibrous or pisolitic.",3.5,4,"2.84","2.86","2.876","Vitreous","Vitreous,Sub-Vitreous,Resinous,Waxy,Pearly","Usually not vitreous or sub-vitreous","Transparent,Translucent","White","Colourless, white, gray, reddish-white, brownish-white, green (rarely), or pink; colourless in transmitted light",[62,63,64,65,66,67],"colorless","white","gray","pink","brown","green",[63],"None","Some types fluoresce white, blue white, creamy yellow, etc. in either SW or LW UV. Manganoan varieties may fluoresce pale pink through intense red, but weaker in long wave.","On \u003Cmi>{10_11}\u003C\u002Fmi>.","Perfect","Sub-Conchoidal","brittle","Uniaxial","-","1.679","1.681","1.500","1.503",1.5,1.681,"0.179","Anomalously biaxial.","Parallel","Very slowly dissolved in cold acids. Powder readily dissolves in warm acids with effervescence.\r\n\r\nMay exhibit triboluminescence.\r\n\r\nDolomite and ferroan dolomite occur frequently as pseudomorphs after calcite and also after aragonite. Rarely pseudomorphic after cerussite, baryte and fluorite.\r\n\r\nSeveral species have been recognized as incrustation or substitution pseudomorphs after dolomite crystals. These include siderite, calcite, smithsonite, quartz, talc, limonite; and more rarely, hematite, pyrite, malachite, azurite, magnetite, cinnabar, sphalerite, pyrolusite, marcasite and serpentine.","A major source of magnesium, particularly for agricultural and pharmaceutical applications.","An important sedimentary and metamorphic mineral found as the principal mineral in dolostones and metadolostones, and as an important mineral in limestones and marbles where calcite is the principal mineral present.  Also found as a hydrothermal vein mineral, forming crystals in cavities; and found in serpentinites and similar rocks.","Dolomite Group. Ankerite-Dolomite Series.\r\n\r\nA common rock forming mineral, also common in veins. Usually, when crystallised, it is found as druzes or clusters of small rhombohedral crystals, typically with a somewhat \"saddle\"-like shape, white to tan ...","Named in 1791 by Nicolas Théodore de Saussure in honor of the French mineralogist and geologist, Déodat (Dieudonné) Guy Sylvain Tancrède Gratet de Dolomieu [June 23, 1750, Dolomieu, near Tour-du-Pin, Isère, France - November 28, 1801, Château-Neuf, Sâone-et-Loire, France]. de Dolomieu wrote numerous books on observations on geology, notably about the Alps and Pyrenees, in addition to theoretical books about the internal structure of the Earth. He discovered a specimen of what would eventually be called dolomite during his participation in Napoleon Bonaparte's expedition into Egypt in 1798.","2026-02-16 12:21:33",[93,99,104,108,112,116,120],{"id":94,"name":95,"entrytype":96,"csystem":11,"ima_formula":11,"mindat_formula":97,"hmin":11,"hmax":11,"dmeas":41,"dcalc":41,"primary_image_id":98},1105,"Cobalt-bearing Dolomite",2,"Ca(Mg,Co)(CO\u003Csub>3\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>",49881,{"id":100,"name":101,"entrytype":96,"csystem":11,"ima_formula":11,"mindat_formula":102,"hmin":11,"hmax":11,"dmeas":41,"dcalc":41,"primary_image_id":103},11125,"Iron-bearing Dolomite","Ca(Mg,Fe)(CO\u003Csub>3\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>",61109,{"id":105,"name":106,"entrytype":96,"csystem":11,"ima_formula":11,"mindat_formula":15,"hmin":11,"hmax":11,"dmeas":41,"dcalc":41,"primary_image_id":107},30570,"Manganese-bearing 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(1923) A Comprehensive Treatise on Inorganic and Theoretical Chemistry. 16 volumes, London: 4: 372.",{"id":609,"year":599,"html":610,"doi":11},16107842,"Mitchell (1923) Journal of the Chemical Society, London: 123: 1055.",{"id":612,"year":599,"html":613,"doi":11},16107843,"Ungemach (1923) Zeitschrift für Kristallographie, Mineralogie und Petrographie, Leipzig: 58: 161.",{"id":615,"year":616,"html":617,"doi":11},16107844,1924,"Bäckström (1924) Journal of the Chemical Society, London: 125: 430.",{"id":619,"year":616,"html":620,"doi":11},16107845,"Wyckoff and Merwin (1924) American Journal of Science: 8: 447.",{"id":622,"year":623,"html":624,"doi":11},16107846,1925,"de Klerk and Goldschmidt (1925) Mineralogische und petrographische Mitteilungen, Vienna: 38: 159.",{"id":626,"year":623,"html":627,"doi":11},16107847,"Eitel (1925) Jb. Min., Beil.-Bd.: 51: 477.",{"id":629,"year":630,"html":631,"doi":11},16100698,1926,"Rocza (1926) Zentralblatt Mineralien: 229.",{"id":633,"year":630,"html":634,"doi":11},16107848,"Garrabos, M. L. (1926) Symétrie et macles de la dolomite étudiées au moyen des rayons X. \u003Ci>Bulletin de la Société française de Minéralogie\u003C\u002Fi>,  49 (3-6). 110-127",{"id":636,"year":630,"html":637,"doi":11},16107849,"Strobentz (1926) Földtani Közlöny, Budapest (Magyarhone Földtani Torsulat): 55: 49.",{"id":639,"year":630,"html":640,"doi":11},16107850,"Zsivny (1926) Ann. Hist.-Nat. Mus. Nat. Hungar.: 24: 423.",{"id":642,"year":643,"html":644,"doi":11},16107851,1927,"Hintze, Carl (1927) Handbuch der Mineralogie. Berlin and Leipzig. 6 volumes: 1[3A]: 3333.",{"id":646,"year":643,"html":647,"doi":11},16107852,"Zsivny (1927) Zeitschrift für Kristallographie, Mineralogie und Petrographie, Leipzig: 65: 728.",{"id":649,"year":650,"html":651,"doi":11},16107853,1928,"Kani (1928) Journal of the Geological Society of Tokyo: 35: 279.",{"id":653,"year":654,"html":655,"doi":11},16107854,1930,"Halla (1930) Ak Wien, Sitzber.: 139: 683.",{"id":657,"year":654,"html":658,"doi":11},16107855,"Onorato E. (1930) Sulla natura della dolomite. Periodico di Mineralogia - Roma pp. 216-220.",{"id":660,"year":661,"html":662,"doi":11},16107856,1932,"Vavrinecz (1932) Magyar Chemiai Folyóirat, Budapest: 38: 140.",{"id":664,"year":665,"html":666,"doi":11},520112,1933,"Ulke, Titus (1933) Ankerite from Bethesda, Maryland. \u003Ci>American Mineralogist\u003C\u002Fi>,  18 (7) 312 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM18\u002FAM18_312.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":668,"year":669,"html":670,"doi":11},16107858,1934,"Koch and Zombory (1934) Földtani Közlöny, Budapest (Magyarhone Földtani Torsulat): 64: 160.",{"id":672,"year":669,"html":673,"doi":11},16107859,"Tokody (1934) Magyar Tudom. Akad. Mat. Termeszett. Ertisitö, Budapest: 50: 650.",{"id":675,"year":676,"html":677,"doi":11},16107860,1935,"Du Rietz (1935) Geologiska Föeningens I Stockholm. Förhandlinger, Stockholm: 57: 133.",{"id":679,"year":676,"html":680,"doi":11},16107861,"Hawkes and Smythe (1935) Mineralogical Magazine: 24: 65.",{"id":682,"year":676,"html":683,"doi":11},16107862,"Koiké (1935) Journal of the Japanese Association of Min. Petr. Ec. Geol.: 14: 216.",{"id":685,"year":676,"html":686,"doi":11},16107864,"Tertsch (1935) Zeitschrift für Kristallographie, Mineralogie und Petrographie, Leipzig: 92: 39.",{"id":688,"year":676,"html":689,"doi":690},105075,"Schoklitsch, Karl (1935) Beitrag zur Physiographie steirischer Karbonspäte. \u003Ci>Zeitschrift für Kristallographie, Mineralogie und Petrographies\u003C\u002Fi>,  90 (4). 433-445 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1935.90.1.433'>doi:10.1524\u002Fzkri.1935.90.1.433\u003C\u002Fa>","10.1524\u002Fzkri.1935.90.1.433",{"id":692,"year":693,"html":694,"doi":11},16107865,1936,"Royer (1936) Comptes rendus de l’Académie des sciences de Paris: 202: 429.",{"id":696,"year":693,"html":697,"doi":11},16107866,"Siegl (1936) Mineralogische und petrographische Mitteilungen, Vienna: 48: 288.",{"id":699,"year":700,"html":701,"doi":11},16107867,1940,"Koritnig, Ehrlich (1940) Zentralblatt Mineralien: 41.",{"id":703,"year":700,"html":704,"doi":705},1153554,"Rodgers, J. (1940) Distinction between calcite and dolomite on polished surfaces. \u003Ci>American Journal of Science\u003C\u002Fi>,  238 (11) 788-798 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2475\u002Fajs.238.11.788'>doi:10.2475\u002Fajs.238.11.788\u003C\u002Fa>","10.2475\u002Fajs.238.11.788",{"id":707,"year":708,"html":709,"doi":710},1153801,1941,"Fairbairn, H. W., Hawkes, H. E. (1941) Dolomite orientation in deformed rocks. \u003Ci>American Journal of Science\u003C\u002Fi>,  239 (9) 617-632 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2475\u002Fajs.239.9.617'>doi:10.2475\u002Fajs.239.9.617\u003C\u002Fa>","10.2475\u002Fajs.239.9.617",{"id":712,"year":713,"html":714,"doi":715},4241,1947,"Smythe, J. A., Dunham, K. C. (1947) Ankerites and chalybites from the northern Pennine orefield and the north-east coalfield. \u003Ci>Mineralogical Magazine and Journal of the Mineralogical Society\u003C\u002Fi>,  28 (197) 53-74 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1947.028.197.01'>doi:10.1180\u002Fminmag.1947.028.197.01\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_28\u002F28-197-53.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1947.028.197.01",{"id":717,"year":718,"html":719,"doi":720},439000,1948,"Wickman, F. E. (1948) From the notes of the late K. Johansson. I. \u003Ci>Geologiska Föreningen i Stockholm Förhandlingar\u003C\u002Fi>,  70 (2) 349-350 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1080\u002F11035894809454092'>doi:10.1080\u002F11035894809454092\u003C\u002Fa>","10.1080\u002F11035894809454092",{"id":722,"year":723,"html":724,"doi":11},521935,1949,"Faust, George T. (1949) Dedolomitization, and its relation to a possible derivation of a magnesium-rich hydrothermal solution. \u003Ci>American Mineralogist\u003C\u002Fi>,  34 (11-12) 789-823 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM34\u002FAM34_789.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":726,"year":727,"html":728,"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":730,"year":731,"html":732,"doi":733},168049,1962,"Goldsmith, Julian R., Graf, Donald L., Witters, Juanita, Northrop, David A. (1962) Studies in the System CaCO3-MgCO3-FeCO3: 1. Phase Relations; 2. A Method for Major-Element Spectrochemical Analysis; 3. Compositions of Some Ferroan Dolomites. \u003Ci>The Journal of Geology\u003C\u002Fi>,  70 (6) 659-688 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1086\u002F626865'>doi:10.1086\u002F626865\u003C\u002Fa>","10.1086\u002F626865",[735,745,755,764,772,781,790,799,804,812,822,831,836,842,852,860,867,874,882,889,897,906,914,923,932,939,944,951,959,969,977,986,996,1004,1012,1019,1027,1036,1042,1050,1058,1065,1074,1082,1090,1095,1103,1108,1115,1123,1130,1137,1146,1154,1162,1169],{"id":736,"source_url":737,"license_code":738,"credit_html":739,"title":740,"description":741,"author":742,"original_width":743,"original_height":744},5744,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=7185993","CC BY-SA 3.0","JJ Harrison (https:\u002F\u002Fwww.jjharrison.com.au\u002F), via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=7185993\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cinnabar on Dolomite.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCinnabar\" class=\"extiw\" title=\"en:Cinnabar\">Cinnabar\u003C\u002Fa> on \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDolomite\" class=\"extiw\" title=\"en:Dolomite\">Dolomite\u003C\u002Fa>","JJ Harrison (https:\u002F\u002Fwww.jjharrison.com.au\u002F)",1763,1254,{"id":746,"source_url":747,"license_code":748,"credit_html":749,"title":750,"description":751,"author":752,"original_width":753,"original_height":754},7310,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=8868415","CC BY-SA 4.0","Didier Descouens, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=8868415\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Dolomite-Magnésite- Navarre.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDolomite\" class=\"extiw\" title=\"w:Dolomite\">Dolomite\u003C\u002Fa> and \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002Fmagnesite\" class=\"extiw\" title=\"en:magnesite\">magnesite\u003C\u002Fa>\n\u003Cdd>Locality : Azcárate Quarry, Eugui, Esteribar, Navarre, Spain\u003C\u002Fdd>\n\u003Cdd>Size : 10.2x6.7cm.\u003C\u002Fdd>","Didier Descouens",3628,2821,{"id":756,"source_url":757,"license_code":738,"credit_html":758,"title":759,"description":760,"author":761,"original_width":762,"original_height":763},13530,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=26382092","Parent Géry, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=26382092\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cuprite, kolwezite, dolomite 1.JPG","crystals of cuprite, crystals of kolwezite, cristals of dolomite : Mashamba West Mine, Kolwezi Districy, Katanga Copper Crescent, Katanga (Shaba), Republic of Congo (Zaïre)","Parent Géry",4288,2848,{"id":765,"source_url":766,"license_code":748,"credit_html":767,"title":768,"description":769,"author":752,"original_width":770,"original_height":771},7311,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=8875036","Didier Descouens, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=8875036\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Dolomite Luzenac.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDolomite\" class=\"extiw\" title=\"en:Dolomite\">Dolomite\u003C\u002Fa> and \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FTalc\" class=\"extiw\" title=\"en:Talc\">Talc\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality : Trimouns Talc Mine, Luzenac, Ariège, Midi-Pyrénées, France\u003C\u002Fdd>\n\u003Cdd>Size 10x6.2cm\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",4345,2863,{"id":773,"source_url":774,"license_code":748,"credit_html":775,"title":776,"description":777,"author":778,"original_width":779,"original_height":780},7315,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=100616864","Elekes Andor, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=100616864\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Dolomite -.jpg","Dolomite. On the top of Schreiberberg (Budaörs, 258 m).","Elekes Andor",4000,3000,{"id":782,"source_url":783,"license_code":748,"credit_html":784,"title":785,"description":786,"author":787,"original_width":788,"original_height":789},732,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=50365140","Joan Rosell - Rosellminerals.com, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=50365140\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","RM746-Allanita-(Ce)-dolomita-calcita.jpg","Localidad: Cantera de talco de Trimouns, Luzenac, Ariège, Midi-Pyrénées, Francia.\n\u003Cp>Ejemplar que muestra un nutrido grupo de cristales de allanita-(Ce) dispuestos aleatóriamente sobre una cavidad tapizada de dolomita y calcita. Este mineral de Elementos de Tierras Raras es un clásico de esta localidad francesa. Se presenta como cristales prismáticos muy alargados, con transparencia y color marrón a miel tostada. \n\u003C\u002Fp>\u003Cp>Medidas: 9,2 x 6,5 x 5,5 cm.\nCristal principal: 6 x 1 mm.\n\u003C\u002Fp>\nEncontrado en ±2004.","Joan Rosell - Rosellminerals.com",872,1260,{"id":791,"source_url":792,"license_code":748,"credit_html":793,"title":794,"description":795,"author":796,"original_width":797,"original_height":798},5987,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=41267829","Géry PARENT, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=41267829\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Rosélite, cobaltaustinite, dolomite 1100.FS2015.jpg","roselite, cobaltaustinite, dolomite : Agoudal Centre Quarrys, Agoudal, Bou Azer District (Bou Azzer District), Tazenakht, Ouarzazate Province, Souss-Massa-Draâ Region, Morocco","Géry PARENT",1981,1319,{"id":800,"source_url":801,"license_code":748,"credit_html":802,"title":803,"description":795,"author":796,"original_width":797,"original_height":798},5988,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=41267831","Géry PARENT, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=41267831\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Rosélite, cobaltaustinite, dolomite 1100.FS2015 1.jpg",{"id":805,"source_url":806,"license_code":748,"credit_html":807,"title":808,"description":809,"author":796,"original_width":810,"original_height":811},5989,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=46954056","Géry PARENT, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=46954056\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Roselite-ß, cobaltocalcite, cobaltaustinite, dolomite 7100.3711.jpg","roselite-ß, cobaltocalcite, cobaltaustinite, dolomite : Agoudal Centre Quarry, Agoudal, Bou Azer District (Bou Azzer District), Tazenakht, Ouarzazate Province, Souss-Massa-Draâ Region, Morocco",1988,1325,{"id":813,"source_url":814,"license_code":815,"credit_html":816,"title":817,"description":818,"author":819,"original_width":820,"original_height":821},7339,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=17429312","Public domain","Modris Baum, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=17429312\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Riebeckite, Calcite, Dolomite, Donnayite group-262219.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FRiebeckite\" class=\"extiw\" title=\"en:Riebeckite\">Riebeckite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCalcite\" class=\"extiw\" title=\"en:Calcite\">Calcite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDolomite\" class=\"extiw\" title=\"en:Dolomite\">Dolomite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDonnayite\" class=\"extiw\" title=\"en:Donnayite\">Donnayite\u003C\u002Fa> Group (FOV ~ 4.5 cm wide)\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Poudrette quarry (Demix quarry; Uni-Mix quarry; Desourdy quarry), Mont Saint-Hilaire, Rouville RCM, Montérégie, Québec, Canada\u003C\u002Fdd>\n\u003Cdd>\u003Ci>Original description:\u003C\u002Fi> FOV ~ 4.5 cm wide. Found 1996. This is from hornfels and MSH collectors call it \"riebeckite\" - but it has not been analyzed.\u003C\u002Fdd>\n\u003Cdd>This material is found abundantly but infrequently. It may be \"under collected\" because it's rather ugly when wet and muddy - as if often the case. But when cleaned up, the blue color is quite attractive. There are some very small calcite \"cones\" and translucent dolomite rhombs (esp top). There are also quite a few gray donnayite group \"pagodas\" with white caps. Likely these are ewaldite with donnayite-(Y). In any case, they are too small to make out in the photo.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Modris Baum",1024,635,{"id":823,"source_url":824,"license_code":738,"credit_html":825,"title":826,"description":827,"author":828,"original_width":829,"original_height":830},13527,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10138687","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10138687\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Dolomite-Kolwezite-114258.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDolomite\" class=\"extiw\" title=\"en:Dolomite\">Dolomite\u003C\u002Fa> (Var.: Cobaltoan Dolomite), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FKolwezite\" class=\"extiw\" title=\"en:Kolwezite\">Kolwezite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Musonoi Mine, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FKolwezi\" class=\"extiw\" title=\"en:Kolwezi\">Kolwezi\u003C\u002Fa>, Western area, Katanga Copper Crescent, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FKatanga\" class=\"extiw\" title=\"en:Katanga\">Katanga (Shaba)\u003C\u002Fa>, Democratic Republic of Congo (Zaïre) (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-4322.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 2.2 x 1.7 x 1.7 cm.\u003C\u002Fdd>\n\u003Cdd>A beautifully bright pink thumbnail of cobaltoan dolomite rhombs on matrix from the famous Musonoi Mine of Zaire. The two tiny kolwezite balls really add character to this showy piece. Material of this quality is seldom available today.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Robert M. Lavinsky",500,380,{"id":832,"source_url":833,"license_code":738,"credit_html":834,"title":835,"description":760,"author":761,"original_width":762,"original_height":763},13531,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=26382093","Parent Géry, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=26382093\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cuprite, kolwezite, dolomite.JPG",{"id":837,"source_url":838,"license_code":738,"credit_html":839,"title":840,"description":841,"author":761,"original_width":762,"original_height":763},13532,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=26441340","Parent Géry, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=26441340\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cuprite, kolwezite, dolomite 2.JPG","crystals of cuprite, crystals of kolwezite, crystals of dolomite : Mashamba West Mine, Kolwezi Districy, Katanga Copper Crescent, Katanga (Shaba), Republic of Congo (Zaïre)",{"id":843,"source_url":844,"license_code":845,"credit_html":846,"title":847,"description":848,"author":849,"original_width":850,"original_height":851},13534,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=167127940","CC BY 4.0","Animalculum, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=167127940\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Kolwezite with Cuprite and Dolomite, Musee de Mineralogie, Paris, 2025.jpg","Kolwezite with Cuprite and Dolomite from Kakanda South Mine, Lualaba, DR Congo in Musee de Mineralogie, Paris","Animalculum",2796,3654,{"id":853,"source_url":854,"license_code":738,"credit_html":855,"title":856,"description":857,"author":828,"original_width":858,"original_height":859},15143,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=74299421","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=74299421\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Magnussonite, Allactite, Hausmannite, Dolomite-762319.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMagnussonite\" class=\"extiw\" title=\"en:Magnussonite\">Magnussonite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAllactite\" class=\"extiw\" title=\"en:Allactite\">Allactite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHausmannite\" class=\"extiw\" title=\"en:Hausmannite\">Hausmannite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDolomite\" class=\"extiw\" title=\"en:Dolomite\">Dolomite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FL%C3%A5ngban\" class=\"extiw\" title=\"en:Långban\">Långban\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FFilipstad\" class=\"extiw\" title=\"en:Filipstad\">Filipstad\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FV%C3%A4rmland\" class=\"extiw\" title=\"en:Värmland\">Värmland\u003C\u002Fa>, Sweden (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"https:\u002F\u002Fwww.mindat.org\u002Floc-3167.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Dimensions: 7.0 cm x 6.5 cm x 2.0 cm\u003C\u002Fdd>\n\u003Cdd>A very good specimen of hausmannite-dolomite ore exhibiting a fracture surface coated with relatively coarse, inter-grown blades of dark pink allactite and scattered patches of emerald-green magnussonite. Allactite is an uncommon manganese arsenate hydroxide. From Langban, Filipstad, Varmland, Sweden, the type locality for magnussonite, a manganese arsenite. Ex. Paulo Matioli and Swedish Natural History Museum collections with labels.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",1386,1134,{"id":861,"source_url":862,"license_code":738,"credit_html":863,"title":864,"description":857,"author":828,"original_width":865,"original_height":866},15144,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=74299423","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=74299423\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Magnussonite, Allactite, Hausmannite, Dolomite-762320.jpg",1500,1000,{"id":868,"source_url":869,"license_code":738,"credit_html":870,"title":871,"description":857,"author":828,"original_width":872,"original_height":873},15145,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=74299427","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=74299427\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Magnussonite, Allactite, Hausmannite, Dolomite-762321.jpg",1439,1172,{"id":875,"source_url":876,"license_code":845,"credit_html":877,"title":878,"description":879,"author":880,"original_width":881,"original_height":865},20026,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=131777693","София Угарова, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=131777693\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Камень доломит.jpg","dolomite stone","София Угарова",1478,{"id":883,"source_url":884,"license_code":845,"credit_html":885,"title":886,"description":879,"author":880,"original_width":887,"original_height":888},20027,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=131777694","София Угарова, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=131777694\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Камень доломит 01.jpg",2754,1822,{"id":890,"source_url":891,"license_code":815,"credit_html":892,"title":893,"description":894,"author":796,"original_width":895,"original_height":896},21735,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=11373587","Géry PARENT, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=11373587\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Scheelite, quartz, dolomite.jpg","scheelite, quartz, dolomite : Huya W-Sn-Be deposit (Pingwu beryl mine), Huya village, Mt Xuebaoding, Pingwu Co., Mianyang Prefecture, Sichuan Province, China",2765,3941,{"id":898,"source_url":899,"license_code":738,"credit_html":900,"title":901,"description":902,"author":903,"original_width":904,"original_height":905},23156,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146751239","HolDu, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146751239\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Chalkostibit, Fahlerz, Dolomit (OM1-082A).JPG","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FChalcostibite\" class=\"extiw\" title=\"en:Chalcostibite\">Chalcostibite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FFahlore\" class=\"extiw\" title=\"en:Fahlore\">Fahlore\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDolomite_(mineral)\" class=\"extiw\" title=\"en:Dolomite (mineral)\">Dolomite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Cavnik, Baia Mare, Transylvania, Romania\u003C\u002Fdd>\n\u003Cdd>Weight: 26.3 g\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","HolDu",3989,3313,{"id":907,"source_url":908,"license_code":738,"credit_html":909,"title":910,"description":911,"author":828,"original_width":912,"original_height":913},23346,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10120481","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10120481\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Svanbergite-Dolomite-21593.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSvanbergite\" class=\"extiw\" title=\"en:Svanbergite\">Svanbergite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDolomite\" class=\"extiw\" title=\"en:Dolomite\">Dolomite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Mount Brussilof mine (Bay Mag Mine), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FRadium_Hot_Springs,_British_Columbia\" class=\"extiw\" title=\"en:Radium Hot Springs, British Columbia\">Radium Hot Springs\u003C\u002Fa>, Golden Mining Division, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBritish_Columbia\" class=\"extiw\" title=\"en:British Columbia\">British Columbia\u003C\u002Fa>, Canada (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-485.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>A very pretty and richly crystallized specimen of this rare species, with sharp cubic 1mm-plus crystals on contrasting matrix of sparkling white dolomite! In person, this is a very colorful and showy piece, aside from the rarity, and is of display quality 3 x 2.5 x 2.1 cm\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",567,600,{"id":915,"source_url":916,"license_code":845,"credit_html":917,"title":918,"description":919,"author":920,"original_width":921,"original_height":922},24685,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=107310213","Kasatkin, A.V., Makovicky, E., Plášil, J., Škoda, R., Agakhanov, A.A, Karpenko, V.Y. and Nestola, F., via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=107310213\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Tsygankoite, Alabandite, Arsenic, Orpiment, Calcite, Dolomite.png","Black elongated grain of tsygankoite with metallic lustre and alabandite (in the center) in white dolomite-calcite matrix along with orpiment (yellow) and native arsenic (black rounded grain on the right). This grain of tsygankoite was extracted from the polished section and used for the structure data collection. Image obtained from: Kasatkin, A.V., Makovicky, E., Plášil, J., Škoda, R., Agakhanov, A.A, Karpenko, V.Y. and Nestola, F. (2018) Tsygankoite, Mn8Tl8Hg2(Sb21Pb2Tl)S24S48, a New Sulfosalt from the Vorontsovskoe Gold Deposit, Northern Urals, Russia. Minerals: 8(5): 218; doi.org\u002F10.3390\u002Fmin8050218 The article is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. (CC BY 4.0).","Kasatkin, A.V., Makovicky, E., Plášil, J., Škoda, R., Agakhanov, A.A, Karpenko, V.Y. and Nestola, F.",1246,933,{"id":924,"source_url":925,"license_code":748,"credit_html":926,"title":927,"description":928,"author":929,"original_width":930,"original_height":931},28825,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=153647466","J. Patrick Fischer, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=153647466\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","24844 Zinckenit-Dolomit 1.jpg","Zinckenit mit Dolomit, Saint-Pons, Südfrankreich. 302,6 g","J. Patrick Fischer",3156,2604,{"id":933,"source_url":934,"license_code":738,"credit_html":935,"title":936,"description":937,"author":761,"original_width":481,"original_height":938},33892,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=21243231","Parent Géry, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=21243231\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Wulfénite, vanadinite, dolomite.jpg","wulfenite, vanadinite var. endlichite, dolomite : Erupción Mine (Ahumada Mine ; Erupción-Ahumada Mine), Los Lamentos Mts (Sierra de Los Lamentos), Mun. de Ahumada, Chihuahua,  Mexico",2633,{"id":940,"source_url":941,"license_code":738,"credit_html":942,"title":943,"description":937,"author":761,"original_width":762,"original_height":763},33893,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=21243233","Parent Géry, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=21243233\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Wulfénite, vanadinite, dolomite 2.jpg",{"id":945,"source_url":946,"license_code":738,"credit_html":947,"title":948,"description":949,"author":828,"original_width":913,"original_height":950},37896,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10127315","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10127315\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Calcite-Dolomite-39571.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCalcite\" class=\"extiw\" title=\"en:Calcite\">Calcite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDolomite\" class=\"extiw\" title=\"en:Dolomite\">Dolomite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Sweetwater Mine (Milliken Mine; Frank R. Milliken; Blair Creek; Ozark Lead Company Mine; Adair Creek; Logan Creek), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FEllington\" class=\"extiw\" title=\"en:Ellington\">Ellington\u003C\u002Fa>, Viburnum Trend District, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FReynolds_County,_Missouri\" class=\"extiw\" title=\"en:Reynolds County, Missouri\">Reynolds County\u003C\u002Fa>, \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-3866.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Light golden, doubly terminated, and well formed calcite crystals, are aesthetically arranged on a matrix of dolomite along with minor iridescent chalcopyrite. The largest of the calcite crystals exceed 5. 75 cm in length. SUPERB example! 6.2 x 6 x 3.3 cm\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",479,{"id":952,"source_url":953,"license_code":845,"credit_html":954,"title":955,"description":956,"author":957,"original_width":958,"original_height":958},37900,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=182899709","Marie-Lan Taÿ Pamart, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=182899709\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Siderite calcite and dolomite Ibituruna Minéraux SU.jpg","Siderite, calcite and dolomite from Ibituruna peak, Governador Valadares, Minas Gerais, Brazil. Sorbonne University mineral collection.","Marie-Lan Taÿ Pamart",5537,{"id":960,"source_url":961,"license_code":962,"credit_html":963,"title":964,"description":965,"author":966,"original_width":967,"original_height":968},38535,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=73427880","CC BY 3.0","Ralph Bottrill, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=73427880\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Carrollite, Dolomite, Siderite, Malachite-792195.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCarrollite\" class=\"extiw\" title=\"en:Carrollite\">Carrollite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDolomite\" class=\"extiw\" title=\"en:Dolomite\">Dolomite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSiderite\" class=\"extiw\" title=\"en:Siderite\">Siderite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMalachite\" class=\"extiw\" title=\"en:Malachite\">Malachite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Dimensions: 45 mm; Field of view: 35 mm\u003C\u002Fdd>\n\u003Cdd>Locality: Kamoya South II Mine (Kamoya Sud Mine; Kamoya South Mine), Kamoya, Kambove District, Katanga (Shaba), Democratic Republic of the Congo\u003C\u002Fdd>\n\u003Cdd>\u003Ci>Original description:\u003C\u002Fi> Carrollite, white dolomite, yellow siderite and malachite\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Ralph Bottrill",2518,1872,{"id":970,"source_url":971,"license_code":738,"credit_html":972,"title":973,"description":974,"author":828,"original_width":975,"original_height":976},39317,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10161580","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10161580\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Chalcostibite-Sphalerite-Dolomite-216393.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FChalcostibite\" class=\"extiw\" title=\"en:Chalcostibite\">Chalcostibite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSphalerite\" class=\"extiw\" title=\"en:Sphalerite\">Sphalerite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDolomite\" class=\"extiw\" title=\"en:Dolomite\">Dolomite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGalena\" class=\"extiw\" title=\"en:Galena\">Galena\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Boldut Mine, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCavnic\" class=\"extiw\" title=\"en:Cavnic\">Cavnic (Kapnic; Kapnik)\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMaramure%C5%9F_County\" class=\"extiw\" title=\"en:Maramureş County\">Maramures County\u003C\u002Fa>, Romania (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-6861.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 11.3 x 6.7 x 6.5 cm.\u003C\u002Fdd>\n\u003Cdd>Chalcostibite is a rare copper, antimony sulfosalt. This excellent and very showy, 3-dimensional cabinet combination piece from Cavnic, Romania features shiny, gray metallic blades and needles of chalcostibite clusters richly scattered on lustrous sphalerite crystals and associated with a rich, preferential coating of sparkly, light gray dolomite rhombs and a bit of galena. Chalcostibite was never common at Cavnic and this major discovery was made in 1990.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",700,434,{"id":978,"source_url":979,"license_code":738,"credit_html":980,"title":981,"description":982,"author":983,"original_width":984,"original_height":985},49265,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=6607105","Ra'ike (see also: de:Benutzer:Ra'ike), via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=6607105\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Chrysotilasbest aus serpentiniertem Dolomit - Farm Rietfontein, Carolina, Transvaal.JPG","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FChrysotile\" class=\"extiw\" title=\"en:Chrysotile\">Chrysotil\u003C\u002Fa> asbestos out of serpentinized Dolomite - Locality: Farm Rietfontein, Carolina, Transvaal - Exposed in the Mineralogical Museum, Bonn, Germany","Ra'ike (see also: de:Benutzer:Ra'ike)",2800,2080,{"id":987,"source_url":988,"license_code":989,"credit_html":990,"title":991,"description":992,"author":993,"original_width":994,"original_height":995},50415,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=186819712","CC0 1.0","Slashme, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=186819712\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Konichalcit Dolomit 28142 01.jpg","Conichalcite and dolomite from Altenmiltlau, Spessart, Bavaria. 67g with mm scale","Slashme",3907,2987,{"id":997,"source_url":998,"license_code":989,"credit_html":999,"title":1000,"description":1001,"author":993,"original_width":1002,"original_height":1003},50416,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=186819714","Slashme, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=186819714\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Konichalcit Dolomit 28142 02.jpg","Conichalcite and dolomite from Altenmiltlau, Spessart, Bavaria. 67g",5710,4640,{"id":1005,"source_url":1006,"license_code":738,"credit_html":1007,"title":1008,"description":1009,"author":828,"original_width":1010,"original_height":1011},51267,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10142122","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10142122\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cubanite-Pyrrhotite-Dolomite-135185.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCubanite\" class=\"extiw\" title=\"en:Cubanite\">Cubanite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FPyrrhotite\" class=\"extiw\" title=\"en:Pyrrhotite\">Pyrrhotite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDolomite\" class=\"extiw\" title=\"en:Dolomite\">Dolomite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Morro Velho mine (incl. Mina Velha; Mina Grande), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FNova_Lima\" class=\"extiw\" title=\"en:Nova Lima\">Nova Lima\u003C\u002Fa>, Iron Quadrangle, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMinas_Gerais\" class=\"extiw\" title=\"en:Minas Gerais\">Minas Gerais\u003C\u002Fa>, Southeast Region, Brazil (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-415.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 13.5 x 8.5 x 4.8 cm.\u003C\u002Fdd>\n\u003Cdd>An AESTHETIC CABINET specimen of highly lustrous and translucent, light gray dolomite rhombs festooned with brassy, tabular crystals of cubanite and pyrrhotite from the 1960s find at the famous Morro Velho Gold Mine, Nova Lima, Brazil. The cubanites reach 9 mm. Dr. Gary Hansen got much of this find and this is from his personal collection. I found one more stashed away in the small lot from his collection. VERY DIFFICULT to obtain in this quality and size today.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",650,425,{"id":1013,"source_url":1014,"license_code":738,"credit_html":1015,"title":1016,"description":1017,"author":828,"original_width":1018,"original_height":913},51274,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10166456","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10166456\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cubanite-Siderite-Dolomite-246453.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCubanite\" class=\"extiw\" title=\"en:Cubanite\">Cubanite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSiderite\" class=\"extiw\" title=\"en:Siderite\">Siderite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDolomite\" class=\"extiw\" title=\"en:Dolomite\">Dolomite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Morro Velho mine (incl. Mina Velha; Mina Grande), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FNova_Lima\" class=\"extiw\" title=\"en:Nova Lima\">Nova Lima\u003C\u002Fa>, Iron Quadrangle, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMinas_Gerais\" class=\"extiw\" title=\"en:Minas Gerais\">Minas Gerais\u003C\u002Fa>, Southeast Region, Brazil (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-415.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 4.2 x 3.2 x 2.9 cm.\u003C\u002Fdd>\n\u003Cdd>A classic and fine combination specimen from the 1960s finds at the Morro Velho Mine of Brazil. Lustrous, brassy, tabular cubanite crystals are richly and aesthetically scattered on the mounded matrix of glassy, yellow-green siderite blades and translucent, light gray dolomite rhombs. Some of the cubanites are beautifully iridescent and the large siderite is 2.2 cm. A highly representative and showy, two-sided piece from this well-known find and locale. Ex. Scott Williams Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",586,{"id":1020,"source_url":1021,"license_code":815,"credit_html":1022,"title":1023,"description":1024,"author":819,"original_width":1025,"original_height":1026},53952,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=9572453","Modris Baum, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=9572453\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Eudidymite and Dolomite - Poudrette quarry, Mont Saint-Hilaire, Quebec, Canada.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FEudidymite\" class=\"extiw\" title=\"en:Eudidymite\">Eudidymite\u003C\u002Fa> and \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDolomite\" class=\"extiw\" title=\"en:Dolomite\">Dolomite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Poudrette quarry (Demix quarry; Uni-Mix quarry; Desourdy quarry), Mont Saint-Hilaire, Rouville RCM, Montérégie, Québec, Canada\u003C\u002Fdd>\n\u003Cdd>The main rosette is about 7 mm in diameter. Found May 1997\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",893,720,{"id":1028,"source_url":1029,"license_code":738,"credit_html":1030,"title":1031,"description":1032,"author":1033,"original_width":1034,"original_height":1035},56712,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=131978137","Michael C. Rygel, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=131978137\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","C GrosVentre 40X 2 PPL.jpg","Limestone with glauconite and dolomite in plane polarized light.  Specimen is stained for calcite.  Cambrian Grose Ventre Formation, WY.","Michael C. Rygel",1206,617,{"id":1037,"source_url":1038,"license_code":738,"credit_html":1039,"title":1040,"description":1041,"author":1033,"original_width":1034,"original_height":1035},56713,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=131978138","Michael C. Rygel, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=131978138\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","C GrosVentre 40X 1 PPL.jpg","Limestone with glauconite and dolomite in plane polarized light. Cambrian Grose Ventre Formation, WY.",{"id":1043,"source_url":1044,"license_code":748,"credit_html":1045,"title":1046,"description":1047,"author":1033,"original_width":1048,"original_height":1049},56714,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=132081181","Michael C. Rygel, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=132081181\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","C GrosVentre glauconite 20x PPL.jpg","Photomicrograph (plane polarized light) of glauconite, calcite, and dolomite in the Cambrian Gros Ventre Formation, WY.  Same image but with crossed polars provided under \"other versions\" below",2304,1728,{"id":1051,"source_url":1052,"license_code":738,"credit_html":1053,"title":1054,"description":1055,"author":828,"original_width":1056,"original_height":1057},64024,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10030244","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10030244\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Dolomite-Aragonite-173842.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDolomite\" class=\"extiw\" title=\"en:Dolomite\">Dolomite\u003C\u002Fa> (Var.: Cobaltoan Dolomite), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAragonite\" class=\"extiw\" title=\"en:Aragonite\">Aragonite\u003C\u002Fa> (Var.: Plumboan Aragonite)\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Tsumeb Mine (Tsumcorp Mine), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FTsumeb\" class=\"extiw\" title=\"en:Tsumeb\">Tsumeb\u003C\u002Fa>, Otjikoto (Oshikoto) Region, Namibia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2428.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 4 x 3.5 x 3 cm.\u003C\u002Fdd>\n\u003Cdd>An amazing pseudomorph and a very unusual Tsumeb specimen, from a small pocket. It is complete 360-degrees and undamaged all around! The color is a bright pink, and it has a sparkly lustre. Ex. Sussman Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",338,450,{"id":1059,"source_url":1060,"license_code":738,"credit_html":1061,"title":1062,"description":1063,"author":828,"original_width":1064,"original_height":913},64917,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10165882","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10165882\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Galena-Dolomite-Marcasite-243358.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGalena\" class=\"extiw\" title=\"en:Galena\">Galena\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDolomite\" class=\"extiw\" title=\"en:Dolomite\">Dolomite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMarcasite\" class=\"extiw\" title=\"en:Marcasite\">Marcasite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCalcite\" class=\"extiw\" title=\"en:Calcite\">Calcite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Buick Mine (Amax Buick Mine; Moloc Mine), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBixby\" class=\"extiw\" title=\"en:Bixby\">Bixby\u003C\u002Fa>, Viburnum Trend District, Iron 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-3871.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 7.2 x 4.6 x 2.5 cm.\u003C\u002Fdd>\n\u003Cdd>A rare and superb cluster of sharp, highly to moderately lustrous, lead-gray, parallel-growth, spinel-twinned galena crystals from the Buick Mine of Missouri’s Viburnum Trend. These large crystals and style are classic for a particular find there, in the 1990s. This excellent, complete-all-around crystal is richly and beautifully covered on the back and one edge with lustrous dolomite rhombs, sparkly, brassy marcasite crystals and a couple of well-placed, calcite scalenohedrons. The doubly terminated calcite on the end is 1.5 cm (one end is cleaved).\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",581,{"id":1066,"source_url":1067,"license_code":1068,"credit_html":1069,"title":1070,"description":1071,"author":1072,"original_width":779,"original_height":1073},67593,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=83169261","CC BY 2.0","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=83169261\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Dundee Limestone over Lucas Dolomite (Middle Devonian; Auglaize Quarry, near Junction, Ohio, USA) 4 (48889181752).jpg","\u003Cp>Limestones and dolostones in the Devonian of Ohio, USA.\n\u003C\u002Fp>\u003Cp>This is the active wall at a functioning quarry in far-northwestern Ohio.  We were forbidden from closely approaching the walls.  Large, loose blocks of rock were piled on the quarry floor for close examination and mineral collecting.\n\u003C\u002Fp>\u003Cp>The gray-colored rocks in the top third of the wall are the Dundee Limestone, a Middle Devonian unit equivalent to the upper Columbus Limestone and Delaware Limestone elsewhere in Ohio.  At this site, the Dundee is principally light gray to gray-brown micrite and dismicrite.  These lithologies are sometimes referred to as lithographic limestone and sublithographic limestone.  Stylolites are present, as are numerous patches of coarsely-crystalline calcite.\n\u003C\u002Fp>\u003Cp>The brownish-colored rocks in the middle and lower walls are the Lucas Dolomite of the upper Detroit River Group.  The Lucas appears to consist of dolostone and limestone.  Finely-laminated, brown dolostone is a common lithology in this unit.  Lack of stratigraphic control in the loose quarry blocks makes specific lithologic assessments difficult.  Stylolites are also present in the Lucas.\n\u003C\u002Fp>\u003Cp>Stratigraphy: Dundee Limestone over Lucas Dolomite, Middle Devonian\n\u003C\u002Fp>\nLocality: Auglaize Quarry (= Shelly Company, Stoneco's Auglaize Facility), southeast of the town of Junction, northeastern Paulding County, northwestern Ohio, USA (41° 10' 27.83\" North latitude, 84° 25' 19.75\" West longitude)","James St. John",2923,{"id":1075,"source_url":1076,"license_code":738,"credit_html":1077,"title":1078,"description":1079,"author":828,"original_width":1080,"original_height":1081},67763,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10141270","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10141270\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Millerite-Dolomite-130305.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMillerite\" class=\"extiw\" title=\"en:Millerite\">Millerite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDolomite\" class=\"extiw\" title=\"en:Dolomite\">Dolomite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Ronna Mine, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FKladno\" class=\"extiw\" title=\"en:Kladno\">Kladno\u003C\u002Fa>, Central Bohemia Region, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBohemia\" class=\"extiw\" title=\"en:Bohemia\">Bohemia (Böhmen; Boehmen)\u003C\u002Fa>, Czech Republic (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-18510.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 4.9 x 2.6 x 2.5 cm.\u003C\u002Fdd>\n\u003Cdd>An OUTSTANDING combination specimen from Kladno, Czech Republic of bright, brassy, millerite needles to 8 mm nicely scattered in a vug with lustrous, gray dolomite rhombs. Seldom available in this quality from this locality. Excellent material from the Richard Hauck Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",483,572,{"id":1083,"source_url":1084,"license_code":748,"credit_html":1085,"title":1086,"description":1087,"author":1088,"original_width":1089,"original_height":763},75470,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113744475","Koreller, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113744475\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Muséum de Nantes - 336 - Dolomite (Alpes-de-Haute-Provence).jpg","Dolomite, en provenance des Alpes-de-Haute-Provence, au Muséum de Nantes","Koreller",4272,{"id":1091,"source_url":1092,"license_code":748,"credit_html":1093,"title":1094,"description":1087,"author":1088,"original_width":1089,"original_height":763},75471,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113744476","Koreller, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113744476\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Muséum de Nantes - 337 - Dolomite (Alpes-de-Haute-Provence).jpg",{"id":1096,"source_url":1097,"license_code":748,"credit_html":1098,"title":1099,"description":1100,"author":1088,"original_width":1101,"original_height":1102},75472,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113744481","Koreller, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113744481\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Muséum de Nantes - 340 - Dolomite (Espagne).jpg","Dolomite, en provenance d'Espagne, au Muséum de Nantes",3212,2300,{"id":1104,"source_url":1105,"license_code":748,"credit_html":1106,"title":1107,"description":1100,"author":1088,"original_width":1089,"original_height":763},75473,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113744482","Koreller, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113744482\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Muséum de Nantes - 341 - Dolomite (Espagne).jpg",{"id":1109,"source_url":1110,"license_code":748,"credit_html":1111,"title":1112,"description":1100,"author":1088,"original_width":1113,"original_height":1114},75474,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113744483","Koreller, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113744483\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Muséum de Nantes - 342 - Dolomite (Espagne).jpg",3880,2452,{"id":1116,"source_url":1117,"license_code":748,"credit_html":1118,"title":1119,"description":1120,"author":796,"original_width":1121,"original_height":1122},77346,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=42798911","Géry PARENT, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=42798911\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Rosélite, dolomite 7100.2731.jpg","roselite, dolomite : Agoudal Centre Quarry, Agoudal, Bou Azer District (Bou Azzer District), Tazenakht, Ouarzazate Province, Souss-Massa-Draâ Region, Morocco",1992,1382,{"id":1124,"source_url":1125,"license_code":748,"credit_html":1126,"title":1127,"description":1120,"author":796,"original_width":1128,"original_height":1129},77347,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=42798914","Géry PARENT, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=42798914\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Rosélite, dolomite 7100.2606.jpg",2497,1749,{"id":1131,"source_url":1132,"license_code":748,"credit_html":1133,"title":1134,"description":1120,"author":796,"original_width":1135,"original_height":1136},77348,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=42798916","Géry PARENT, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=42798916\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Rosélite, dolomite 7100.2776.jpg",2000,1555,{"id":1138,"source_url":1139,"license_code":1140,"credit_html":1141,"title":1142,"description":1143,"author":1144,"original_width":779,"original_height":1145},78234,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118205478","CC BY-SA 2.0","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118205478\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Sartorite with Sugary Dolomite (47975580747).jpg","\u003Cp>Binnental\nSwitzerland\n\u003C\u002Fp>\nS-74-2029","Pacific Museum of Earth from Canada",6000,{"id":1147,"source_url":1148,"license_code":989,"credit_html":1149,"title":1150,"description":1151,"author":1152,"original_width":1153,"original_height":661},78236,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163482428","Darla Sondrol, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163482428\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Sartorite with pyrite in dolomite (GeoDIL number - 1191).jpg","This 5 cm across pecimen is mostly dolomite but is notable because it contains a few dark gray masses of sartorite, the most prominent of which is just left of center in this photo. It also contains some golden pyrite. Sartorite is a rare lead aresenic sulfide mineral with composition Pb3As4S9. It is usually steel gray with a metallic luster and striated acicular to prismatic crystals. Its best known occurrence is at Lengenbach in Switzerland.","Darla Sondrol",2746,{"id":1155,"source_url":1156,"license_code":738,"credit_html":1157,"title":1158,"description":1159,"author":828,"original_width":1160,"original_height":1161},79495,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10147909","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10147909\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Siegenite-Dolomite-162518.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSiegenite\" class=\"extiw\" title=\"en:Siegenite\">Siegenite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDolomite\" class=\"extiw\" title=\"en:Dolomite\">Dolomite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Sweetwater Mine (Milliken Mine; Frank R. Milliken; Blair Creek; Ozark Lead Company Mine; Adair Creek; Logan Creek), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FEllington\" class=\"extiw\" title=\"en:Ellington\">Ellington\u003C\u002Fa>, Viburnum Trend District, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FReynolds_County,_Missouri\" class=\"extiw\" title=\"en:Reynolds County, Missouri\">Reynolds County\u003C\u002Fa>, \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-3866.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 6.5 x 3.5 x 3.3 cm.\u003C\u002Fdd>\n\u003Cdd>Silvery and bright siegenite crystals richly cover sulfide matrix on this very fine combination specimen along with off-white dolomite rhombs from the famous Sweetwater Mine of Missouri’s Viburnum Trend. Scattered, golden chalcopyrite adds color. The siegenite \"ball\" perched atop siegenite and dolomite is very attractive. This is older material and is seldom available in this quality. Siegenite is an extremely rare mineral from these mines and is found at its most significant here. Rather, it was. No finds I am aware of came out since the 1980s. This is a superb example from the Gary Hansen dealer stock.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",550,387,{"id":1163,"source_url":1164,"license_code":738,"credit_html":1165,"title":1166,"description":1159,"author":828,"original_width":1167,"original_height":1168},79496,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10147912","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10147912\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Siegenite-Dolomite-162519.jpg",400,379,{"id":1170,"source_url":1171,"license_code":738,"credit_html":1172,"title":1173,"description":1174,"author":828,"original_width":1161,"original_height":1175},80394,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10172106","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10172106\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Stannite-Quartz-Dolomite-280296.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FStannite\" class=\"extiw\" title=\"en:Stannite\">Stannite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FQuartz\" class=\"extiw\" title=\"en:Quartz\">Quartz\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDolomite\" class=\"extiw\" title=\"en:Dolomite\">Dolomite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Yaogangxian Mine, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FYizhang_County\" class=\"extiw\" title=\"en:Yizhang County\">Yizhang County\u003C\u002Fa>, Chenzhou Prefecture, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHunan\" class=\"extiw\" title=\"en:Hunan\">Hunan Province\u003C\u002Fa>, China (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-4549.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 6.2 x 5.9 x 6.1 cm.\u003C\u002Fdd>\n\u003Cdd>This specimen of well-crystallized Stannite from the Yaogangxian mine in Hunan, China features numerous groups of well-defined, brassy-colored Stannite crystals in association with several sharp and very clear Quartz crystals and a sprinkling of white Dolomite and Muscovite Mica. There is a lot of Stannite on this specimen; in fact, half of the matrix is composed of Stannite. It is not quite pristine (just a little damage at the periphery edges of the cluster) but is close to it. There is even a Stannite-lined vug on the right side of the piece. The Quartz crystals all have perfect tips, and some of them even contain Dolomite-covered phantoms in their terminations. Not only is this a very rare species, but to find it in such an aesthetic composition with three other well-crystallized minerals is wonderful. The stannite has excellent luster, and crystals to 8mm.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",480,[1177,1184,1189,1194,1199],{"id":1178,"url":1179,"label":1180,"formula":1181,"spacegroup":1182,"year":1183},3851,"\u002Fcif\u002F3851.cif","Drits 2005 · Ca1.08 Mg.92 C2 O6","Ca1.08 Mg.92 C2 O6","R -3",2005,{"id":1185,"url":1186,"label":1187,"formula":1188,"spacegroup":1182,"year":1183},3852,"\u002Fcif\u002F3852.cif","Drits 2005 · Ca1.17 Mg.83 C2 O6","Ca1.17 Mg.83 C2 O6",{"id":1190,"url":1191,"label":1192,"formula":1193,"spacegroup":1182,"year":1183},3853,"\u002Fcif\u002F3853.cif","Drits 2005 · Ca1.07 Mg.93 C2 O6","Ca1.07 Mg.93 C2 O6",{"id":1195,"url":1196,"label":1197,"formula":1198,"spacegroup":1182,"year":1183},3854,"\u002Fcif\u002F3854.cif","Drits 2005 · Ca1.13 Mg.87 C2 O6","Ca1.13 Mg.87 C2 O6",{"id":1200,"url":1201,"label":1202,"formula":1203,"spacegroup":1182,"year":1183},3856,"\u002Fcif\u002F3856.cif","Drits 2005 · Ca1.14 Mg.86 C2 O6","Ca1.14 Mg.86 C2 O6",[1205,1206,1207,1208,1209,1210,1211,1212,1213,1214,1215,1216,1217,1218,1219,1220,1221,1222,1223,1224,1225,1226,1227,1228,1229,1230,1231,1232,1233,1234,1235,1236,1237,1238,1239,1240],"Bitterkalk","Bittersalzerde","Bitterspat (of Klaproth)","Chaux carbonatée aluminifère","Compound Spar","Dolomie","Kalktalkspath","Kohlensauere Kalkerde","Magnesio-Calcite","Magnesiocalcit","Magnesiodolomit","Magnesiodolomita","Magnesiodolomite","Miemit","Miemita","Miemite","Muricalcit","Muricalcita","Muricalcite","Paratomes Kalk-Haloid","Pearl Spar","Perlspath","Picrite (of Brogniart)","Rauhkalk","Rautenspath","Rhomb Spar","Rhombenspat","Rhomboidalspath","Ridolfit","Ridolphite","Spath magnésien","Spath perlé","Taraspit","Taraspita","Tharandite","Wandstein",[1242,1246,1250,1257,1261,1265,1269,1273,1277,1281,1285,1288,1291,1294,1297,1303,1307,1311,1314,1318,1322,1329,1333,1350,1354,1358,1362,1366,1369,1372,1376,1379,1383,1387,1390,1396,1400,1403,1407,1410,1413,1416,1420,1423,1427,1432,1436,1439,1442,1445,1449,1453,1457,1460,1464,1469,1473,1476,1480,1483,1486,1489,1493,1496,1499,1503,1507,1510,1514,1517,1520,1524,1527,1530,1533,1536,1539,1544,1548,1551,1557,1562,1566,1570,1573,1577,1580,1583,1586,1589,1592,1595],{"lang":1243,"names":1244},"af",[1245],"Dolomiet",{"lang":1247,"names":1248},"an",[1249],"dolomita",{"lang":1251,"names":1252},"ar",[1253,1254,1255,1256],"دولومايت","دولوميت","صخر الدولومايت","صخور الدولوميت",{"lang":1258,"names":1259},"az",[1260],"dolomit",{"lang":1262,"names":1263},"ba",[1264],"доломит",{"lang":1266,"names":1267},"bar",[1268],"Dolomit",{"lang":1270,"names":1271},"be",[1272],"даламіт",{"lang":1274,"names":1275},"be-tarask",[1276],"даляміт",{"lang":1278,"names":1279},"be-x-old",[1280],"Даляміт",{"lang":1282,"names":1283},"bg",[1284],"Доломит",{"lang":1286,"names":1287},"bs",[1268],{"lang":1289,"names":1290},"ca",[1249],{"lang":1292,"names":1293},"cs",[1260],{"lang":1295,"names":1296},"da",[1268],{"lang":1298,"names":1299},"de",[1268,1300,1301,1302],"Dolomitspat","Perlspat","Rautenspat",{"lang":1304,"names":1305},"el",[1306],"δολομίτης",{"lang":1308,"names":1309},"eo",[1310],"dolomito",{"lang":1312,"names":1313},"es",[1249],{"lang":1315,"names":1316},"et",[1317],"dolomiit",{"lang":1319,"names":1320},"eu",[1321,1249],"dolomia",{"lang":1323,"names":1324},"fa",[1325,1326,1327,1328],"دلمیت","دلومیت","دولمیت","دولومیت",{"lang":1330,"names":1331},"fi",[1332],"dolomiitti",{"lang":1334,"names":1335},"fr",[1336,1337,1338,1339,1340,1341,1342,1343,1344,1345,1346,1347,1348,1349],"brossite","CaMg(CO3)2","chaux carbonatée magnésifère","dolomite","dolomite zincifère","magnésiodolomite","manganodolomite","miémite","plumbodolomite","protodolomite","sidérocalcite","spath magnésien","spath perlé","tharandite",{"lang":1351,"names":1352},"ga",[1353],"dolaimít",{"lang":1355,"names":1356},"gl",[1357],"Dolomita",{"lang":1359,"names":1360},"he",[1361],"דולומיט",{"lang":1363,"names":1364},"hi",[1365],"डोलोमाइट",{"lang":1367,"names":1368},"hr",[1268],{"lang":1370,"names":1371},"hu",[1260],{"lang":1373,"names":1374},"hy",[1375],"Դոլոմիտ",{"lang":1377,"names":1378},"id",[1260],{"lang":1380,"names":1381},"io",[1382],"Dolomito",{"lang":1384,"names":1385},"is",[1386],"Dólómít",{"lang":1388,"names":1389},"it",[1339],{"lang":1391,"names":1392},"ja",[1393,1394,1395],"ドロマイト","白雲石","苦灰石",{"lang":1397,"names":1398},"ka",[1399],"დოლომიტი",{"lang":1401,"names":1402},"kk",[1264],{"lang":1404,"names":1405},"kk-arab",[1406],"دولومىيت",{"lang":1408,"names":1409},"kk-cn",[1406],{"lang":1411,"names":1412},"kk-cyrl",[1284],{"lang":1414,"names":1415},"kk-kz",[1284],{"lang":1417,"names":1418},"kk-latn",[1419],"Dolomït",{"lang":1421,"names":1422},"kk-tr",[1419],{"lang":1424,"names":1425},"kn",[1426],"ಡಾಲಮೈಟ್",{"lang":1428,"names":1429},"ko",[1430,1431],"돌로마이트","백운암",{"lang":1433,"names":1434},"ku-latn",[1435],"dolomît",{"lang":1437,"names":1438},"ky",[1264],{"lang":1440,"names":1441},"la",[1249],{"lang":1443,"names":1444},"lez",[1284],{"lang":1446,"names":1447},"lt",[1448],"dolomitas",{"lang":1450,"names":1451},"lv",[1452],"dolomīts",{"lang":1454,"names":1455},"mg",[1456],"Dôlômita",{"lang":1458,"names":1459},"mk",[1264],{"lang":1461,"names":1462},"ml",[1463],"ഡോളമൈറ്റ്",{"lang":1465,"names":1466},"nb",[1467,1468],"dolomitt","Dolomitt(stein)",{"lang":1470,"names":1471},"nl",[1472],"dolomiet",{"lang":1474,"names":1475},"nn",[1467],{"lang":1477,"names":1478},"no",[1479],"Dolomitt",{"lang":1481,"names":1482},"oc",[1357],{"lang":1484,"names":1485},"os",[1264],{"lang":1487,"names":1488},"pl",[1260],{"lang":1490,"names":1491},"ps",[1492],"ډولومیت",{"lang":1494,"names":1495},"pt",[1249,7],{"lang":1497,"names":1498},"pt-br",[1357,1339],{"lang":1500,"names":1501},"ro",[1260,1502],"dolomită",{"lang":1504,"names":1505},"ru",[1264,1506],"доломиты",{"lang":1508,"names":1509},"sco",[1339],{"lang":1511,"names":1512},"se",[1513],"dolomihtta",{"lang":1515,"names":1516},"sh",[1260],{"lang":1518,"names":1519},"sk",[1268],{"lang":1521,"names":1522},"sl",[1523,1260],"CaMg(CO₃)₂",{"lang":1525,"names":1526},"smn",[1317],{"lang":1528,"names":1529},"sms",[1467],{"lang":1531,"names":1532},"sr",[1264],{"lang":1534,"names":1535},"sr-ec",[1284],{"lang":1537,"names":1538},"sr-el",[1268],{"lang":1540,"names":1541},"sv",[1260,1542,1543],"Dolomitisk","Dolomitmarmor",{"lang":1545,"names":1546},"th",[7,1547],"โดโลไมต์",{"lang":1549,"names":1550},"tt",[1264],{"lang":1552,"names":1553},"uk",[1554,1555,1556],"вапняк гіркий","вапняк магніїстий","доломіт",{"lang":1558,"names":1559},"vec",[1560,1561],"dołomita","dołomite",{"lang":1563,"names":1564},"vi",[1268,1565],"Đôlômít",{"lang":1567,"names":1568},"wuu",[1569],"白云石",{"lang":1571,"names":1572},"yo",[7],{"lang":1574,"names":1575},"za",[1576],"bwzyinzsiz",{"lang":1578,"names":1579},"zh",[1569],{"lang":1581,"names":1582},"zh-cn",[1569],{"lang":1584,"names":1585},"zh-hans",[1569],{"lang":1587,"names":1588},"zh-hant",[1394],{"lang":1590,"names":1591},"zh-hk",[1394],{"lang":1593,"names":1594},"zh-sg",[1569],{"lang":1596,"names":1597},"zh-tw",[1394],"Q167741",{"history":1600,"applications":1605},{"markdown":1601,"model_version":1602,"prompt_version":1603,"reviewed_at":1604},"The mountains came after the mineral. The Dolomite Mountains in northern Italy take their name from a pale carbonate rock first described in 1791. The rock was named after the man who studied it: the French geologist Déodat de Dolomieu.\n\nA study of the Alps in 1789 and 1790[5] brought him to the carbonate stone that would carry his name. He had encountered it first in the buildings of old Rome, and later as samples collected in the Tyrolean Alps[6]. The Genevan chemist Nicolas-Théodore de Saussure formally named it dolomite the following year[7]. Some accounts place the formal naming a few months later, in March 1792[8].","claude-opus-4-7","1.7.0","2026-06-02 13:50:42",{"markdown":1606,"model_version":1602,"prompt_version":1603,"reviewed_at":1607},"In construction, dolomite is cut into ornamental stone and crushed into concrete aggregate[1]. Where calcite limestone is uncommon or too costly, dolomite is sometimes used in its place. It serves there as a flux — material that helps the metal melt cleanly — for the smelting of iron and steel[2].\n\nIndustrial chemistry takes dolomite for the magnesium inside it. Calcined — heated until its carbonates break down — dolomite yields magnesium oxide[3]. The same calcined ore feeds the Pidgeon process for the production of magnesium[4]. It is also a source of magnesium for pharmaceutical applications[5]. Large quantities of processed dolomite go into the production of float glass[6]. That is the smooth, planar window glass made by floating molten glass on a bath of tin.\n\nAgriculture and environmental care turn to dolomite for its slow release of magnesium and its buffering effect on acid soils. Dolomite and dolomitic limestone are added to soils and soilless potting mixes as a pH buffer and as a magnesium source[7]. Pastures can be limed with dolomitic lime to raise their pH and to remedy magnesium deficiency[8]. The same lime is used in environmental restoration and soil regeneration, raising pH in soils acidified by mining[9]. Marine aquaria use dolomite gravel as a substrate that buffers the water against pH swings[10].\n\nTwo more roles round the list out. As a host rock, dolomite is an important petroleum reservoir[11]. It also hosts the strata-bound Mississippi Valley-Type ore deposits — layered seams of lead, zinc, and copper inside carbonate rocks[12]. As a high-temperature catalyst, calcined dolomite destroys tar in the gasification of biomass[13]. That is the heating of wood, agricultural waste, or other plant matter to extract a fuel gas.","2026-06-02 13:59:27"]