125cm karamin jima'i mini yar tsana lebur lebur sexy dols

Na hudu farkawa

Tun daga 2005 gonar na Camsi Fergrei ya tashi daga 0.4 zuwa inci takwas a kowace shekara. Wannan adadin hauhawar farashin kaya yana da ƙasa da abin da aka lura da abin da aka lura a cikin lokutan rikitarwa uku na baya, amma yana faruwa kusan shekaru 20 a yanzu. Masana ilimin dabbobi sun fara mamakin abin da ke faruwa idan an shimfiɗa ɓoyayyiyar da dicess

Hakanan akwai tsalle-tsalle a cikin mita da kuma m na girgizar a cikin yankin tun lokacin bazara. Lambar ta sauka a cikin 'yan makonnin da suka gabata, amma pillent Temblors suna har yanzu suna robing yankin, gami da babban taron da aka kirkira?

A watan Yuni rukuni na masana kimiyya sun buga takarda wanda ya yi kokarin lalata halayen Volcano a cikin shekaru 70 da suka gabata. Idan wannan fassarar wannan binciken daidai ne, hakanan zai iya bayanin abin da ke faruwa a yau.

Ga abin da suke tsammanin yana ci gaba: a zurfin mil biyar zuwa shida, akwai m magma da ke koyaushe yana bin iskar gas. Wasu daga cikin wannan gas an kama shi a wani shinge na dutsen kusan mil biyu a ƙasa, kuma wasu suna tserewa daga kananan Maws na wutar lantarki a wurare kamar Mododorooro mai zurfi Solfatara Craker.

Masu binciken sun hango hakan, a cikin shekarun 1950, Magma tsari na magma, Magma magmai in kusa da waccan shingen dutsen, wanda ya cire shi kadan da ɗaukakewa da ɓawon burodi. Da zarar Magma ya sanyaya ƙasa kuma karin iskar gas ya tsaya a farfajiya, mai saukar ungulu ya tsaya da ƙasa - duk da cewa ba zai iya komawa matakan da aka auna ba kafin a yi amfani da shi.

Teamungiyar tayi imani da wannan tsari ya sake faruwa a cikin 1970s da 1980s. A lokacin tashin hankalin 1980s, maimaita watsi da ɓawon burodi ya kirkiro don tserewa, wanda ya haifar da wani muhimmin yanayi na subgingtence daga baya.elden zobe jima'i

Da yawa daga cikin wadancan rauni tun daga warke. Wadancan allurar magma uku na magma sun sanyaya da daskararru, samar da babban mai binciken Magma, wanda kuma shi ne wani shamaki a cikin Vesuvius a Naples. Amma gas ya ci gaba da zo daga zurfin magma, kuma yawancinsu ya sake yawaita a kan shingen dutsen kusan mil mil biyu, suna haifar da ƙasa don ɗauka.

Magmin gas yana tashi daga zurfin ƙasa kuma ya zama mai yiwuwa ya isa ya bayyana uplift ɗin da ke faruwa tun 200 da lokaci-lokaci da kuma lokaci-lokaci da kuma lokaci-lokaci da kuma lokaci-lokaci da kuma lokaci-lokaci da kuma lokaci-lokaci samun rauni da aka kafa.