Funda konke Okuvela Kanjani Ukumemezela Ngayo Uma Kuphazamiseka
I-Eyjafjallajökull yi-volcano evelele yase-Iceland enegama elide elingase libe nzima kakhulu ukulibiza. Itholakala ngasogwini oluseningizimu phakathi kweMt. I-Hekla noMt. I-Katla, izintaba-mlilo ezimbili ezisebenzayo. Futhi i-volcano esebenzayo, i-Eyjafjallajökull ihlanganiswe ngokuphelele kwi-cap cap edla ama-glaciers amaningi. Esimweni sayo esiphakeme, intaba-mlilo inamamitha amahlanu ubude, futhi i-ice cap ihlanganisa amakhilomitha angama-40 square.
I-crater isingamakhilomitha amabili ububanzi, ivulekile enyakatho, futhi inezilinganiso ezintathu eceleni kwesigubhu sekhanda. U-Eyjafjallajökull uye waqhuma njalo, umsebenzi wamuva kakhulu ngo-2010.
Okushoyo nokubizwa ngegama
Igama elithi Eyjafjallajökull lingase lizwakale liyinkimbinkimbi, kodwa incazelo yalo ilula futhi ingadilizwa zibe izingxenye ezintathu: "Eyja" kusho isiqhingi, "fjalla" kusho izintaba, futhi "jökull" okusho ukuthi i-glacier. Ngakho lapho kuhlanganiswa u-Eyjafjallajökull kusho "i-glacier ezintabeni zezintaba."
Nakuba ukuhumusha akuyona leyo inselele, ukubiza igama le-volcano kuyinto-isi-Iceland kungaba ulimi olulukhuni kakhulu ukuze lukwazi kahle. Kodwa ngokuphindaphinda ama-syllables wezwi, kufanele kuthathe imizuzu embalwa ukubiza u-Eyjafjallajökull kangcono kunokuningi. Yisho i- AY-yah-fyad-layer-kuh-tel ukuze ufunde ama-syllables e-"Eyjafjallajökull" bese uphinda izikhathi eziningana uze uhlele phansi.
U-Eruption of Volcanic ka-2010
Kungakhathaliseki ukuthi uqobo noma awukho embikweni wezindaba ezenziwa ngo-Eyijafjallajökull phakathi kuka-Mashi no-Agasti ka-2010, kulula ukucabanga ukuthi izintatheli zezindaba zakwamanye amazwe ziqamba igama lika-volcano lase-Iceland.
Kodwa kungakhathaliseki ukuthi kwakhulunywa kanjani, le ndaba yayifanayo-emva kokuhlala isikhathi eside iminyaka engaphezu kwengu-180, u-Eyjafjallajökull waqala ukukhipha indawo engasetshenziswanga eningizimu-ntshonalanga ye-Iceland, ngokubonga. Ngemva kwenyanga engasebenzi, i-volcano yaqhuma futhi, okwamanje kusukela phakathi kwe-glacier ebangela ukukhukhula nokudinga abantu abangu-800.
Lokhu kuqhuma kwandisa umlotha emkhathini obangela ukuphazanyiswa kwe-air-travel cishe isonto enyakatho-ntshonalanga yeYurophu, lapho amazwe angu-20 ayevale khona umoya wezokuhamba ngezindiza, okwenza abantu abangaba ngu-10 million abahambahamba-okuyiwona omkhulu ukuphazamiseka kokuhamba emoyeni kusukela eWWII. Umlotha waqhubeka waba yinkinga endaweni yomoya ngenyanga ezayo, eqhubeka nokuphazamisa izinhlelo zezindiza.
Ngasekuqaleni kukaJune, kwavulwa elinye ukuvulwa komgodla futhi laqala ukuchitha umcibisholo omncane womswakama-volcanic. I-Eyjafjallajökull yayiqashwe izinyanga ezimbalwa ezilandelayo futhi ngo-Agasti kwakubhekwa njengesiqhwa. Ukuqhuma kwe-Eyjafjallajökull okwedlule kwakuneminyaka engu-920, 1612, 1821 no-1823.
Uhlobo lwe-Volcano
I-Eyjafjallajökull iyi-stratovolcano, uhlobo oluvame kakhulu lwe-volcano. I-stratovolcano yakhiwe yizingxenye zelava elinzima, i-tephra, i-pumice, nomlotha wokushisa i-volcanic. I-glacier phezulu eyenza ukuqhuma kwe-Eyjafjallajökull kuqhuma futhi kugcwele umlotha. I-Eyjafjallajökull iyingxenye yochungechunge lwezintaba-mlilo ezibhekene ne-Iceland futhi likholelwa ukuthi lixhunywe neKatla, intaba-mlilo emikhulu futhi enamandla kakhulu kulolu hlobo-lapho i-Eyjafjallajökull iqhuma, ukuqhuma kwe-Katla kulandela. A