[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:31587":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":16,"elements":17,"sigelements":23,"key_elements":24,"impurities":11,"cim":11,"ima_status":25,"ima_notes":11,"ima_history":11,"approval_year":27,"publication_year":28,"discovery_year":11,"strunz10ed1":29,"strunz10ed2":21,"strunz10ed3":30,"strunz10ed4":31,"dana8ed1":11,"dana8ed2":11,"dana8ed3":11,"dana8ed4":11,"csystem":32,"cclass":33,"spacegroup":34,"spacegroupset":35,"a":36,"b":37,"c":38,"alpha":39,"beta":40,"gamma":39,"aerror":41,"berror":42,"cerror":33,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":11,"csmetamict":14,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":43,"tlform":44,"hmin":45,"hmax":45,"hardtype":11,"vhnmin":39,"vhnmax":39,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":46,"dmeas2":46,"dcalc":47,"dmeaserror":48,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":49,"commentluster":11,"diapheny":50,"streak":51,"colour":52,"commentcolor":53,"colors":54,"streak_colors":59,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":60,"fracturetype":11,"tenacity":61,"commentbreak":11,"opticaltype":62,"opticalsign":63,"opticalalpha":64,"opticalalpha2":39,"opticalalphaerror":33,"opticalbeta":65,"opticalbeta2":39,"opticalbetaerror":33,"opticalgamma":66,"opticalgamma2":39,"opticalgammaerror":33,"opticalomega":39,"opticalomega2":39,"opticalomegaerror":11,"opticalepsilon":39,"opticalepsilon2":39,"opticalepsilonerror":11,"opticaln":39,"opticaln2":39,"opticalnerror":11,"optical2vcalc":39,"optical2vcalc2":39,"optical2vcalcerror":11,"optical2vmeasured":39,"optical2vmeasured2":39,"optical2vmeasurederror":11,"rimin":67,"rimax":68,"opticaldispersion":69,"opticalpleochroism":70,"opticalpleochorismdesc":71,"opticalbirefringence":11,"opticalcomments":72,"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":73,"industrial":11,"occurrence":74,"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":88,"confused_with":89,"type_localities":90,"occurrence_total":97,"citations":98,"images":112,"structures":131,"synonyms":144,"language_names":147,"wikidata_qid":168,"texts":169},31587,"1:1:31587:4","71a189bb-06d2-4efd-8ae8-bf30e4b61628","Lasalite","Las",0,"mineral",null,55047,361,false,"Na\u003Csub>2\u003C\u002Fsub>Mg\u003Csub>2\u003C\u002Fsub>(V\u003Csub>10\u003C\u002Fsub>O\u003Csub>28\u003C\u002Fsub>)·20H\u003Csub>2\u003C\u002Fsub>O","Na\u003Csub>2\u003C\u002Fsub>Mg\u003Csub>2\u003C\u002Fsub>V\u003Csub>10\u003C\u002Fsub>O\u003Csub>28\u003C\u002Fsub> · 20H\u003Csub>2\u003C\u002Fsub>O",[18,19,20,21,22],"Mg","Na","O","H","V",[18,19,20,21,22],[22],[26],"APPROVED",2007,2008,"4","C","05","Monoclinic",5,10,"C2\u002Fc ","23.9019","10.9993","17.0504","0","118.284",7,3,"The major forms are {100}, {010}, {001}, \u003Cmi>{_111}\u003C\u002Fmi>, and {111}.","Efflorescent crusts are commonly 1 to 3 mm thick. The surfaces of the crusts may be rounded owing to dissolution, but may also glisten from exposed crystal faces. Some sandstone surfaces are coated with isolated single crystals 1 to 2 mm in length.",1,"2.38","2.362",2,"Adamantine","Transparent","Yellow","Yellow to yellow-orange","Thin coatings on sandstone are brown.",[55,56,57,58],"yellow","orange","brown","green",[55],"None Observed","very brittle","Biaxial","-","1.743","1.773","1.780",1.743,1.78,"strong r> v dispersion.","Visible","X = light greenish yellow, Y = light yellow, Z = light brown","2V at 550 nm: 32(l), 589 nm: 43(l), and 650 nm: 53(l);","On prolonged exposure to conditions of low humidity, the crystals dehydrate to a yellow powder.","Lasalite occurs in efflorescences on the sandstone walls of the mine workings and along fractures in the sandstone. The mineral forms by oxidation of the primary vanadium oxide bronze phase (corvusite) by vadose water and reaction with dolomite and calcite cement of the host sandstone.","National Museum of Natural History (Smithsonian Institution), Washington, D.C., USA, catalog number NMNH-174744.","It is virtually identical in all respects to pascoite and other members of that group, and can only be distinguished by X-ray diffraction or chemical methods.","For the type locality.","2026-01-15 14:17:04",[],[81],{"id":82,"name":83,"entrytype":9,"csystem":32,"ima_formula":84,"mindat_formula":85,"hmin":45,"hmax":45,"dmeas":86,"dcalc":87,"primary_image_id":11},52841,"Ammoniolasalite","[(NH\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>Mg\u003Csub>2\u003C\u002Fsub>(H\u003Csub>2\u003C\u002Fsub>O)\u003Csub>20\u003C\u002Fsub>] · [V\u003Csub>10\u003C\u002Fsub>O\u003Csub>28\u003C\u002Fsub>]","[(NH\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>Mg\u003Csub>2\u003C\u002Fsub>(H\u003Csub>2\u003C\u002Fsub>O)\u003Csub>20\u003C\u002Fsub>] [V\u003Csub>10\u003C\u002Fsub>O\u003Csub>28\u003C\u002Fsub>]","2.28","2.278",[],[],[91],{"id":92,"txt":93,"latitude":94,"longitude":95,"country":96},30869,"Vanadium Queen Mine, La Sal Creek Mining District, San Juan County, Utah, USA",38.3359843,-109.0827638,"USA",8,[99,103,108],{"id":100,"year":28,"html":101,"doi":102},64593,"Hughes, J. M., Wise, W. S., Gunter, M. E., Morton, J. P., Rakovan, J. (2008) Lasalite, Na\u003Csub>2\u003C\u002Fsub>Mg\u003Csub>2\u003C\u002Fsub>[V\u003Csub>10\u003C\u002Fsub>O\u003Csub>28\u003C\u002Fsub>]·20H\u003Csub>2\u003C\u002Fsub>O, a new decavanadate mineral species from the Vanadium Queen mine, La Sal District, Utah: Description, atomic arrangement, and relationship to the pascoite group of minerals. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  46 (5) 1365-1372 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3749\u002Fcanmin.46.5.1365'>doi:10.3749\u002Fcanmin.46.5.1365\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fcm\u002Fvol46\u002FCM46_1365.pdf' class='refpdflink'>\u003C\u002Fa>","10.3749\u002Fcanmin.46.5.1365",{"id":104,"year":105,"html":106,"doi":107},64625,2009,"Hughes, J. M., Wise, W. S., Gunter, M. E., Morton, J. P., Rakovan, J. (2009) Lasalite, Na\u003Csub>2\u003C\u002Fsub>Mg\u003Csub>2\u003C\u002Fsub>[V\u003Csub>10\u003C\u002Fsub>O\u003Csub>28\u003C\u002Fsub>]·20H\u003Csub>2\u003C\u002Fsub>O, a new decavanadate mineral species from the Vanadium Queen mine, La Sal District, Utah: Description, atomic arrangement, and relationship to the pascoite group of minerals: Addendum. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  47 (1) 206 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3749\u002Fcanmin.47.1.206'>doi:10.3749\u002Fcanmin.47.1.206\u003C\u002Fa>","10.3749\u002Fcanmin.47.1.206",{"id":109,"year":110,"html":111,"doi":11},16965505,2011,"(2011) Lasalite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Flasalite.pdf' class='refpdflink'>\u003C\u002Fa>",[113,123],{"id":114,"source_url":115,"license_code":116,"credit_html":117,"title":118,"description":119,"author":120,"original_width":121,"original_height":122},14016,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14866790","CC BY-SA 3.0","Leon Hupperichs, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14866790\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Lasalite-116343.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FLasalite\" class=\"extiw\" title=\"en:Lasalite\">Lasalite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Vanadium Queen Mine, La Sal Creek Canyon, Paradox Valley District, Paradox Valley, San Juan Co., Utah, USA\u003C\u002Fdd>\n\u003Cdd>Bright orange crystalline crust of Lasalite. This nice specimen was acquired from Tom Loomis and was tested by Bob Jenkins at the University of Arizona using Raman spectroscopy. This specimen contains no Pascoite. Field of view 6 mm. Specimen and photo Leon Hupperichs.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Leon Hupperichs",777,588,{"id":124,"source_url":125,"license_code":116,"credit_html":126,"title":127,"description":128,"author":120,"original_width":129,"original_height":130},14017,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14866795","Leon Hupperichs, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14866795\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Lasalite-116346.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FLasalite\" class=\"extiw\" title=\"en:Lasalite\">Lasalite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Vanadium Queen Mine, La Sal Creek Canyon, Paradox Valley District, Paradox Valley, San Juan Co., Utah, USA\u003C\u002Fdd>\n\u003Cdd>Bright orange crystalline crust of Lasalite. This nice specimen was acquired from Tom Loomis and was tested by Bob Jenkins at the University of Arizona using Raman spectroscopy. This specimen contains no Pascoite. Field of view 9 mm. Specimen and photo Leon Hupperichs.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",754,572,[132,138],{"id":133,"url":134,"label":135,"formula":136,"spacegroup":137,"year":28},7456,"\u002Fcif\u002F7456.cif","Hughes 2008","Na Mg V5 O24 H20","C 1 2\u002Fc 1",{"id":139,"url":140,"label":141,"formula":142,"spacegroup":137,"year":143},7457,"\u002Fcif\u002F7457.cif","Iida 2004","Mg Na V5 O24 H20",2004,[145,146],"IMA2007-005","Lasaliet",[148,152,157,160,164],{"lang":149,"names":150},"ca",[151],"lasalita",{"lang":153,"names":154},"de",[155,156],"IMA 2007-005","Lasalit",{"lang":158,"names":159},"es",[151],{"lang":161,"names":162},"eu",[163],"Lasalita",{"lang":165,"names":166},"it",[167],"lasalite","Q19860935",{"history":11,"applications":11}]