[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:5981":3},{"id":4,"longid":5,"guid":6,"name":7,"shortcode_ima":8,"entrytype":9,"entrytype_text":10,"varietyof":11,"synid":8,"polytypeof":8,"groupid":8,"weighting":12,"nolocadd":13,"blacklisted":13,"mindat_formula":14,"mindat_formula_note":8,"ima_formula":8,"elements":15,"sigelements":19,"key_elements":8,"impurities":8,"cim":8,"ima_status":8,"ima_notes":8,"ima_history":8,"approval_year":8,"publication_year":8,"discovery_year":8,"strunz10ed1":20,"strunz10ed2":20,"strunz10ed3":20,"strunz10ed4":8,"dana8ed1":8,"dana8ed2":8,"dana8ed3":8,"dana8ed4":8,"csystem":8,"cclass":8,"spacegroup":8,"spacegroupset":20,"a":8,"b":8,"c":8,"alpha":8,"beta":8,"gamma":8,"aerror":8,"berror":8,"cerror":8,"alphaerror":8,"betaerror":8,"gammaerror":8,"va3":8,"z":8,"csmetamict":13,"commentcrystal":8,"twinning":8,"tranglide":8,"parting":8,"epitaxidescription":8,"morphology":8,"tlform":8,"hmin":8,"hmax":8,"hardtype":8,"vhnmin":8,"vhnmax":8,"vhnerror":8,"vhng":8,"vhns":8,"commenthard":8,"dmeas":8,"dmeas2":8,"dcalc":8,"dmeaserror":8,"dcalcerror":8,"commentdense":8,"lustre":8,"lustretype":8,"commentluster":8,"diapheny":8,"streak":8,"colour":8,"commentcolor":8,"colors":8,"streak_colors":8,"luminescence":8,"uv":8,"cleavage":8,"cleavagetype":8,"fracturetype":8,"tenacity":8,"commentbreak":8,"opticaltype":8,"opticalsign":8,"opticalalpha":8,"opticalalpha2":20,"opticalalphaerror":8,"opticalbeta":8,"opticalbeta2":20,"opticalbetaerror":8,"opticalgamma":8,"opticalgamma2":20,"opticalgammaerror":8,"opticalomega":8,"opticalomega2":20,"opticalomegaerror":8,"opticalepsilon":8,"opticalepsilon2":20,"opticalepsilonerror":8,"opticaln":8,"opticaln2":8,"opticalnerror":8,"optical2vcalc":8,"optical2vcalc2":8,"optical2vcalcerror":8,"optical2vmeasured":8,"optical2vmeasured2":8,"optical2vmeasurederror":8,"rimin":8,"rimax":8,"opticaldispersion":8,"opticalpleochroism":8,"opticalpleochorismdesc":8,"opticalbirefringence":8,"opticalcomments":8,"opticalcolour":8,"opticalinternal":8,"opticaltropic":8,"opticalanisotropism":8,"opticalbireflectance":8,"opticalextinction":8,"opticalr":8,"specdispm":8,"ir":8,"electrical":8,"magnetism":8,"thermalbehaviour":8,"other":8,"industrial":8,"occurrence":8,"otheroccurrence":8,"type_specimen_store":8,"description_short":8,"aboutname":8,"rock_parent":8,"rock_parent2":8,"rock_root":21,"rock_bgs_code":8,"meteoritical_code":8,"updttime":22,"reviewed_at":8,"variety_of":23,"varieties":31,"group_members":32,"associates":33,"confused_with":34,"type_localities":35,"occurrence_total":36,"citations":37,"images":59,"structures":78,"synonyms":79,"language_names":80,"wikidata_qid":8,"texts":81},5981,"1:1:5981:3","164ddd84-ddf9-4298-8f9a-4f428e999704","Common Opal",null,2,"variety",3004,472,false,"SiO\u003Csub>2\u003C\u002Fsub>·nH\u003Csub>2\u003C\u002Fsub>O",[16,17,18],"Si","O","H",[16,17,18],"0",0,"2025-08-11 12:14:26",{"id":11,"name":24,"entrytype":21,"csystem":8,"ima_formula":25,"mindat_formula":14,"hmin":26,"hmax":27,"dmeas":28,"dcalc":20,"strunz10ed1":29,"primary_image_id":30},"Opal","SiO\u003Csub>2\u003C\u002Fsub> · nH\u003Csub>2\u003C\u002Fsub>O",5.5,6.5,"1.9","4",18161,[],[],[],[],[],42,[38,43,48,52,56],{"id":39,"year":40,"html":41,"doi":42},565312,1971,"Jones, J. B., Segnit, E. R. (1971) The nature of opal I. nomenclature and constituent phases. \u003Ci>Journal of the Geological Society of Australia\u003C\u002Fi>,  18 (1) 57-68 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1080\u002F00167617108728743'>doi:10.1080\u002F00167617108728743\u003C\u002Fa>","10.1080\u002F00167617108728743",{"id":44,"year":45,"html":46,"doi":47},3235954,1994,"Elzea, J.M., Odom, I.E., Miles, W.J. (1994) Distinguishing well ordered opal-CT and opal-C from high temperature cristobalite by x-ray diffraction. \u003Ci>Analytica Chimica Acta\u003C\u002Fi>, 286 (1). 107-116 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1016\u002F0003-2670(94)80182-7'>doi:10.1016\u002F0003-2670(94)80182-7\u003C\u002Fa>","10.1016\u002F0003-2670(94)80182-7",{"id":49,"year":50,"html":51,"doi":8},16129728,1996,"Lapis Extra No. 10, Opal (1996).",{"id":53,"year":54,"html":55,"doi":8},17515363,2015,"Newman, Renée (2015) Not-So-Common Common Opal. \u003Ci>13th Sinkankas Symposium\u003C\u002Fi>,  13. Pala International. 48-58",{"id":57,"year":54,"html":58,"doi":8},17515364,"Serras-Herman, Helen (2015) Exotic Common Opals. \u003Ci>13th Sinkankas Symposium\u003C\u002Fi>,  13. Pala International. 58-80",[60,70],{"id":61,"source_url":62,"license_code":63,"credit_html":64,"title":65,"description":66,"author":67,"original_width":68,"original_height":69},50342,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=154048813","CC BY 2.0","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=154048813\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Opalite point 1.jpg","Knapper: Jason Green\n\u003Chr>\nThis point is composed of \"opalite\", an artificial material.  In geology, \"opalite\" refers to opal-bearing rocks (a rock name, not a mineral name) and can refer to \"common opal\" that lacks a play of color.  \"Opalite\" is also a term used in the rock-n-mineral market for manmade opalescent glass.  Some varieties are reportedly made of plastic.","James St. John",1518,3190,{"id":71,"source_url":72,"license_code":63,"credit_html":73,"title":74,"description":75,"author":67,"original_width":76,"original_height":77},50335,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=85906080","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=85906080\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Opal in hydrothermally-altered rhyolitic obsidian (Tertiary; mine at Opal Mountain, Clark County, Idaho, USA) 7.jpg","Opal in rhyolitic obsidian from the Tertiary of Idaho, USA.\n\u003Cp>This rock is on display at a precious opal pay site in the town of Spencer, located on the eastern side of Interstate 15, eastern Idaho.  Rocks are quarried at a nearby mountain and dumped here.  The material is composed of Early Pliocene rhyolitic volcanics that were erupted from the Heise Volcanic Center.  Observed lithologies range from rhyolite to rhyolitic obsidian to hydrothermally altered versions.  The obsidian varies: black spherulitic obsidian, brown spherulitic obsidian, flow-banded spherulitic obsidian.  Opal (= SiO2·nH2O - hydrous silica) occurs in these rocks - it is secondary (early secondary?) and hydrothermal in origin.  The opal fills cavities and lithophysae in the host rocks.  Observed opal varieties here include common opal (milky opal; = opalite, which is opal rock), hyalite opal, and precious opal.  Also noted were turgite on hyalite and drusy quartz.\n\u003C\u002Fp>\u003Cp>Stratigraphy: possibly derived from a lava flow called the Opal Mountain Rhyolite, Kilgore Tuff, upper Heise Group, Lower Pliocene, 4.45 Ma\n\u003C\u002Fp>\nLocality: derived from an opal mine on the southern side of Opal Mountain between Rattlesnake Creek & Three Mile Creek, ENE of Spencer, north-central Clark County, north of the eastern Snake River Plain, Idaho, USA (44° 22’ 43.94” North latitude, 112° 05’ 38.13” West longitude)",3008,2000,[],[],[],{"history":8,"applications":8}]