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Farkawa ta hudu

Tun daga 2005 ƙasan Campi Flegrei ya tashi da 0.4 zuwa inci takwas a kowace shekara. Wannan hauhawan farashin ya yi kasa fiye da yadda aka yi tashe-tashen hankula a cikin shekaru uku da suka gabata, amma kusan shekaru ashirin kenan da faruwar hakan. Masana ilimin volcano sun fara mamakin abin da zai faru idan ɓawon burodi ya miƙe ya ​​wuce wurin da ya karye. Hentai Sex Doll

Haka kuma an yi ta tsalle-tsalle da yawan girgizar kasa a yankin tun lokacin bazara. Adadin ya ragu a cikin 'yan makonnin da suka gabata, amma har yanzu abubuwa masu ƙarfi suna girgiza yankin, gami da wani abin girma-4.0 a ranar 2 ga Oktoba. Menene zai iya bayyana wannan aiki mai ban tsoro?Fucking A Sex Doll

A watan Yuni ne wasu gungun masana kimiyya suka buga wata takarda da ta yi ƙoƙarin tantance halayen dutsen mai aman wuta a cikin shekaru 70 da suka gabata. Idan fassarar wannan binciken daidai ne, zai iya bayyana abin da ke faruwa a yau.

Ga abin da suke tunanin yana faruwa: A zurfin mil biyar zuwa shida, akwai tafkin magma mai tsayi wanda ke ci gaba da sako iskar gas mai guba. Wasu daga cikin wannan iskar suna makale ne a wani shingen dutse mai nisan mil biyu kasa da kasa, wasu kuma suna tserewa daga kananan tudu masu aman wuta a wurare kamar magudanar ruwa na Solfatara.

Masu binciken sun yi hasashen cewa, a cikin shekarun 1950, wani rukunin magma ya kutsa kusa da wannan shingen dutsen, ya dan karye shi kadan kuma ya daga ɓawon burodi. Da zarar magma ya huce kuma ƙarin iskar gas ɗin ya tsere zuwa sama, ɗagawa ya tsaya kuma ƙasa ta lafa—ko da yake bai taɓa komawa matakan da aka auna kafin dagawa ba.

Ƙungiyar ta yi imanin cewa wannan tsari ya sake faruwa a cikin 1970s da 1980s. A lokacin tashin hankali na 1980s, maimaita fashewar ɓawon burodi ya haifar da sababbin hanyoyi don samun iskar gas don tserewa, wanda ya haifar da wani muhimmin lokaci na raguwa daga baya. Elden Ring Sex Doll

Yawancin waɗancan karaya tun daga lokacin sun warke. Alluran magma guda uku da suka gabata sun sanyaya kuma sun daskare, suna haifar da "tambarin magma, wanda kuma ke zama shinge ga tserewar iskar gas," in ji marubucin binciken Nicola Alessandro Pino, babban jami'in bincike a INGV's Vesuvius Observatory a Naples. Amma iskar gas ya ci gaba da fitowa daga cikin ma'adanar magma mai zurfi, kuma yawancinsa ya sake tarawa a shingen dutse mai nisan mil biyu ƙasa, wanda ya sa ƙasa ta hauhawa.

Gas na Magmatic da ke tashi daga zurfin ƙasa kuma ya makale ya isa ya bayyana haɓakar da ke faruwa tun 2005-kuma girgizar ƙasa na baya-bayan nan da na lokaci-lokaci na iya fitowa daga mummunan haɗuwar sabbin karaya.