Umlilo ozayo

Uma ukuphakamisa kuqhubeka, ekugcineni kukhona okuzokunikeza. Uma ukuphuka okukhulu ngokwanele (noma ukuphuka) kufinyelela phezulu, kunemiphumela emithathu engenzeka. Esokuqala, futhi okungenzeka kakhulu, ukuthi igesi yentaba-mlilo ixoshwa endaweni enkulu, ingenzi monakalo. Kungenjalo, “kungase kuphume endaweni egxilile, lapho kungase kube khona ukuqhuma okuthile, endaweni,” kusho uChristopher Kilburn, isazi sentaba-mlilo kanye nomcwaningi wezingozi ze-geophysical e-University College London, kanye nomlobi-ndawonye wocwaningo lwakamuva.Inflatable. Unodoli Wocansi

Isimo esingase sibe khona yisona esithinta kakhulu: ukungena okungajulile kwe-magma kuxhuma kulokho kuphuka futhi kuqhume ngokushesha phezulu, mhlawumbe ngesixwayiso esincane ngaphambili. Kuphakanyiswe ukuthi ukuphakama nokuzamazama kwamanje kungase kubangelwe imijovo yakamuva ye-magma ekujuleni okungashoni, kodwa izilinganiso zendawo yamandla adonsela phansi yentaba-mlilo ziphakamisa ukuthi akukho kuhlasela okukhulu okunamandla okwenzeke ezinyangeni ezedlule, kusho u-Pino.Robert Crimo Sex Doll.

Njengawo wonke amamodeli, eyakamuva ye-Campi Flegrei ingase ingalungile ngokuphelele. “Asinawo amamodeli aphelele,” kusho uMike Burton, isazi sentabamlilo e-University of Manchester, ngoba “asinalo ulwazi oluphelele.” Unodoli Wocansi Wabesilisa.

I-Campi Flegrei ingenye yezintaba-mlilo eziqashwe ngokucophelela kakhulu emhlabeni. Ukuguquguquka kwayo komhlabathi, ukuphuma kwegesi, ukufunda okushisayo, indawo yamandla adonsela phansi, nokundindizela kwayo kucutshungulwa ngokucophelela nangokuqhubekayo. Ukuziphatha kwezinye izintaba-mlilo kungasiza ososayensi bachaze le datha, kodwa izincazelo azinanazi neze—ikakhulukazi intaba-mlilo engenakho ukuqhuma kwamanje.

Njengoba i-INGV iphetha muva nje: “Amathuba okuqhuma kwentaba-mlilo mancane kakhulu, njengoba abukho ubufakazi bokuthi i-magma ikhuphukela phezulu.” Kodwa iyanezela ukuthi “intaba-mlilo inokuvela kwayo okungokwemvelo okungenakuvinjelwa, futhi, ngokushesha, izophinde iqhume.”