UkubunjwaIsayensi

Ziqhume. The main Ukuhlelwa

Mlilo ebizwa induli, yaxobuka phezu imiphantsi kunye neentanda kolu qweqwe lomhlaba, eboniswe phezu kwamagumbi daka iimveliso mlilo enzulu. Bona babe imilo ikhowuni kunye wentaba phezulu. Umlomo-mlilo - ijelo lebhokisi iziko phantsi.

Products, apho bafika ngaphantsi komhlaba, azilingani ngobukhulu kunye nokwakheka. Ngaphaya koko, i-dubulo unokuthatha indawo ngamandla ezahlukeneyo kunye nexesha. Ngenxa yezi mpawu yenziwa yeyona ixhaphakileyo umsebenzi yokuhlela iintlobo. Kufuneka kuqatshelwe ukuba enye dubulo ukuze uthathe omnye okanye omnye umlinganiswa.

uhlobo Plinian ogama emva UPliny Omdala. umphengululi waseRoma wafa ngexesha kuqhambuko kwiNtaba iVesuvius ngowama-79 AD. e. uhlobo Plinian ke ngamandla ethile. Kuqhuma kwi efanayo ixesha sikhatshwe kwakhululwa isixa esikhulu ash ukuya ubude neekhilomitha malunga namashumi amabini ukuya amahlanu, yaye unokuthatha iiyure eziliqela okanye ngezinye iintsuku. iimveliso mhlobo zisasazwa ngaphezulu indawo enkulu, kwaye umthamo wazo ukusuka 0.1 ukuya km anga-50 nangaphezulu. Mlilo sohlobo Plinian kungabangela ukuwa yenduli kwaye ukuyilwa lo mgodi. Kwezinye iimeko, amafu ingqatsini bayazibhijabhija, kodwa udaka kwenzeka ngaso. Kule hlobo mlilo St Heles (US) ngo-1980.

uhlobo Peleysky luphawulwa bubukho mlilo viscous. Eqina ukuba ukuyekelela, ngaloo ndlela eyakha okanye ngaphezulu uphahla extrusive. Ngoko kwaduma mlilo Pelée (kwi kwisiqithi Martinique) ngo-1902.

Vulcan uhlobo lomsebenzi elifutshane. Enigcoba dubulo kungathatha imizuzu okanye iiyure eziliqela. Noko ke, ukuba lihlaziywe iinyanga eziliqela emva eziliqela iintsuku okanye iiveki. Iqhuma luphawulwa phambi olu hlobo iziqina fluid wokusungula udaka. Izakhiwo akheke pyroclastic kunye udaka. Umthamo stratovolcanoes kukuba ukusuka kwishumi ukuya kwikhulu kwiikhilomitha cubic. amajukujuku nothuthu ezikhutshwayo Extrusive waphawula njalo. Ngokutsho uhlobo Vulcan oko batsho e Guatemala Fuego mlilo.

uhlobo Strombolian ibizwa imbeko isiqithi esikwiMeditera mboli. Ngokuba lo hlobo dubulo luphawulwa okuqhubekayo eruptive iinyanga ezimbalwa (ngamanye amaxesha iminyaka). Kulo mzekelo, kwikholam eruptive kunqabile liphuma ngaphezu km ezilishumi. Ezinye mlilo ifomu izixhobo kwento. Ziqulethe abangelwe (ikakhulu) andesite okanye (ngamaxesha ambalwa) le zeBlack. Cone akholisa kwasekwa ukujaduka enye, ngoxa bona ngokwabo ngokuba mlilo monogenic.

Ukukhutshwa uhlobo Hawaiian olwenze isivuno lwentaba. Imithombo lweempazamo kunye Ukophuka besukelana mnye, maxa wambi amawaka amabini eemitha ubude. Xa kukho ofaka umoya mnye kuphela, lava zohlukana radially. Ngoko ke bakha ezisezintabeni isihlangu ne amathambeka ngobunono kakhulu (ukuya izinyuko ezilishumi). ukuphakama ezinjalo kumiswa maleko kwaye ziqulathe nothuthu. Shield yeyona mlilo inkulu ehlabathini Manua Loa (Hawaii). ukuphakama kwawo - 4103 m. Le ephezulu linobude ikhulu elinamanci mabini, ububanzi baba ngeekhilomitha mahlanu. Ahla udaka wayaneka kwindawo kwisiqithi kweekhilomitha ngaphezulu kwezigidi ezihlanu square. Of iikhilomitha ezingamashumi amane anesibini amawaka anamakhulu amahlanu cubic of umthamo ngaphezu asibhozo ekhulwini ngaphantsi komphakamo wolwandle.

Kukho ezinye iintlobo ze kuqhume. Noko ke, kwenzeka kunqabile kakhulu. Umzekelo, esuke ngwenya ngo-1965 e-Iceland mlilo Surtsey Island kwasekwa.

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