[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:46504":3},{"id":4,"longid":5,"guid":6,"name":7,"shortcode_ima":8,"entrytype":9,"entrytype_text":10,"varietyof":11,"synid":11,"polytypeof":11,"groupid":11,"weighting":12,"nolocadd":13,"blacklisted":13,"mindat_formula":14,"mindat_formula_note":11,"ima_formula":15,"elements":16,"sigelements":22,"key_elements":23,"impurities":11,"cim":11,"ima_status":24,"ima_notes":11,"ima_history":11,"approval_year":26,"publication_year":27,"discovery_year":11,"strunz10ed1":28,"strunz10ed2":29,"strunz10ed3":30,"strunz10ed4":11,"dana8ed1":31,"dana8ed2":31,"dana8ed3":31,"dana8ed4":31,"csystem":32,"cclass":33,"spacegroup":33,"spacegroupset":31,"a":34,"b":35,"c":36,"alpha":37,"beta":38,"gamma":39,"aerror":33,"berror":40,"cerror":41,"alphaerror":42,"betaerror":42,"gammaerror":43,"va3":44,"z":33,"csmetamict":13,"commentcrystal":11,"twinning":45,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":46,"tlform":47,"hmin":33,"hmax":33,"hardtype":11,"vhnmin":11,"vhnmax":11,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":11,"dmeas2":11,"dcalc":48,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":49,"commentluster":11,"diapheny":50,"streak":51,"colour":52,"commentcolor":11,"colors":53,"streak_colors":57,"luminescence":11,"uv":58,"cleavage":59,"cleavagetype":60,"fracturetype":61,"tenacity":62,"commentbreak":11,"opticaltype":63,"opticalsign":64,"opticalalpha":65,"opticalalpha2":11,"opticalalphaerror":66,"opticalbeta":67,"opticalbeta2":11,"opticalbetaerror":66,"opticalgamma":68,"opticalgamma2":11,"opticalgammaerror":66,"opticalomega":11,"opticalomega2":11,"opticalomegaerror":11,"opticalepsilon":11,"opticalepsilon2":11,"opticalepsilonerror":11,"opticaln":11,"opticaln2":11,"opticalnerror":11,"optical2vcalc":69,"optical2vcalc2":11,"optical2vcalcerror":11,"optical2vmeasured":70,"optical2vmeasured2":11,"optical2vmeasurederror":66,"rimin":71,"rimax":72,"opticaldispersion":73,"opticalpleochroism":11,"opticalpleochorismdesc":74,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":11,"opticalr":11,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":75,"industrial":11,"occurrence":76,"otheroccurrence":11,"type_specimen_store":77,"description_short":78,"aboutname":79,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":80,"reviewed_at":11,"variety_of":11,"varieties":81,"group_members":82,"associates":83,"confused_with":84,"type_localities":85,"occurrence_total":40,"citations":92,"images":120,"structures":121,"synonyms":122,"language_names":125,"wikidata_qid":143,"texts":144},46504,"1:1:46504:5","6349fdcd-3697-431b-bb62-89bb28734098","Carlsonite","Csn",0,"mineral",null,12,false,"(NH\u003Csub>4\u003C\u002Fsub>)\u003Csub>5\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>O(SO\u003Csub>4\u003C\u002Fsub>)\u003Csub>6\u003C\u002Fsub>&middot;7H\u003Csub>2\u003C\u002Fsub>O","(NH\u003Csub>4\u003C\u002Fsub>)\u003Csub>5\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>O(SO\u003Csub>4\u003C\u002Fsub>)\u003Csub>6\u003C\u002Fsub> &middot; 7H\u003Csub>2\u003C\u002Fsub>O",[17,18,19,20,21],"Fe","N","O","S","H",[17,18,19,20,21],[18],[25],"APPROVED",2014,2016,"7","D","F","0","Triclinic",2,"9.5927","9.7679","18.3995"," 93.250","95.258","117.993",3,13,7,8,1506.15,"cross-hatched, rare","Forms observed: {100}, {001}, \u003Cmi>{1_10}\u003C\u002Fmi>, {111}, \u003Cmi>{1_1_1}\u003C\u002Fmi>, \u003Cmi>{01_2}\u003C\u002Fmi>","It occurs in crystal form as thin to thick tablets up to about 0.5 mm but often much smaller; the tablets are flattened on {001); at this scale, the yellow to orange-brown crystals are best viewed through a high-powered microscope; also as stout prisms el","2.167","Vitreous","Transparent","tan","yellow to orange-brown",[54,55,56],"yellow","orange","brown",[56],"not observed","{001}","Perfect","Irregular\u002FUneven","brittle","Biaxial","-","1.576",1,"1.585","1.591","78","80",1.576,1.591,"strong (r > v)","yellow (X), orange (Y & Z); X \u003C Y ~ Z","easily soluble in RT water; Lewis basicity: (1) structural unit: 0.23-0.11 valence units (vu); (2) interstitial unit: 0.13\r\n\r\nRaman bands [cm\u003Csup>-1\u003C\u002Fsup>]: 245, 275, 436, 478, 514, 552, 576, 617, 629, 670, 1015, 1066, 1104, 1140, 1160, 1188, 1219","Carlsonite was produced by the condensation of gases in the oil-shale fire. The shale fire occurred in a rock outcrop of the Late Devonian Huron Shale Member of the Ohio Shale along River Road, northeast of the town of Monroeville in Ridgefield Township, Huron County. At the time of inspection, geologists were uncertain of the cause. The current hypothesis suggests the fire started in September 2009 as the result of spontaneous combustion. The shale fire burned until March 2011 and created a variety of exotic mineral species, such as boussinggaulite and lonecreekite, as well as the never-before-observed carlsonite.\r\n","Type and cotype material is deposited in the collections of the Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, California 90007, USA, catalogue numbers 65544 and 65545, respectively","Chemically related especially to clairite and lonecreekite; Unnamed (Fe analogue of huizingite-(Al)); also somewhat to mohrite. The first NH4-Fe oxysulphate mineral. Probably has a narrow stability range.\r\n\r\nThe bipartite structure (related to that of ...","Named in honor of Dr. Ernest H. Carlson (1933–2010) professor of mineralogy at Kent State University, Ohio from 1966 to 2009. At the time of his death, he had completed and submitted a revision of his popular Minerals of Ohio, originally published in 1991 by the Ohio Geological Survey, and was engaged in a study of the Huron River shale fire.","2025-08-11 12:15:13",[],[],[],[],[86],{"id":87,"txt":88,"latitude":89,"longitude":90,"country":91},23702,"Huron Shale burn site, Huron River, Huron County, Ohio, USA",41.2780556,-82.6741667,"USA",[93,97,100,104,108,112,116],{"id":94,"year":95,"html":96,"doi":11},16140247,2010,"Larsen, G. (2010) Survey inspects a rare Ohio geohazard. Ohio Geology: 1: 7.",{"id":98,"year":95,"html":99,"doi":11},16140248,"Carlson, E. (2010) Analysis of Huron River shale fire minerals reveals two specimens new to Ohio. Ohio Geology: 2: 7.",{"id":101,"year":26,"html":102,"doi":103},397582,"Kampf, A. R., Richards, R. P., Nash, B. P. (2014) The 2H and 3R polytypes of sabieite, NH\u003Csub>4\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>(SO\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>, from a natural fire in an oil-bearing shale near Milan, Ohio. \u003Ci>American Mineralogist\u003C\u002Fi>,  99 (7) 1500-1506 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam.2014.4884'>doi:10.2138\u002Fam.2014.4884\u003C\u002Fa>","10.2138\u002Fam.2014.4884",{"id":105,"year":106,"html":107,"doi":11},16140250,2015,"Blake, D. (2015) Carlsonite: New mineral species discovered in northern Ohio. Ohio Department of Natural Resources, Ohio Geology Extra, http:\u002F\u002Fgeosurvey.ohiodnr.gov\u002Fextra-news-archives\u002F2015-articles\u002Fcarlsonite.",{"id":109,"year":106,"html":110,"doi":111},244613,"Williams, P. A., Hatert, F., Pasero, M., Mills, S. J. (2015) New minerals and nomenclature modifications approved in 2014 and 2015. Newsletter No 23. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  79 (1) 51-58 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.2015.079.1.05'>doi:10.1180\u002Fminmag.2015.079.1.05\u003C\u002Fa>","10.1180\u002Fminmag.2015.079.1.05",{"id":113,"year":27,"html":114,"doi":115},398198,"Kampf, Anthony R., Richards, R. Peter, Nash, Barbara P., Murowchick, James B., Rakovan, John F. (2016) Carlsonite, (NH\u003Csub>4\u003C\u002Fsub>)\u003Csub>5\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>O(SO\u003Csub>4\u003C\u002Fsub>)\u003Csub>6\u003C\u002Fsub>·7H\u003Csub>2\u003C\u002Fsub>O, and huizingite-(Al), (NH\u003Csub>4\u003C\u002Fsub>)\u003Csub>9\u003C\u002Fsub>Al\u003Csub>3\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)\u003Csub>8\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>·4H\u003Csub>2\u003C\u002Fsub>O, two new minerals from a natural fire in an oil-bearing shale near Milan, Ohio. \u003Ci>American Mineralogist\u003C\u002Fi>,  101 (9) 2095-2107 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-2016-5680'>doi:10.2138\u002Fam-2016-5680\u003C\u002Fa>","10.2138\u002Fam-2016-5680",{"id":117,"year":118,"html":119,"doi":11},16963531,2017,"(2017) Carlsonite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fcarlsonite.pdf' class='refpdflink'>\u003C\u002Fa>",[],[],[123,124],"Carlsoniet","IMA2014-067",[126,130,135,139],{"lang":127,"names":128},"ca",[129],"carlsonita",{"lang":131,"names":132},"de",[133,134],"Carlsonit","IMA 2014-067",{"lang":136,"names":137},"eu",[138],"Carlsonita",{"lang":140,"names":141},"it",[142],"carlsonite","Q19862340",{"history":11,"applications":11}]