Ngokuqinisekile wake wabona kolunye lochungechunge lwama-animated lwaseJapan lwe INtaba iFuji. Iyintaba-mlilo edume kakhulu kulo lonke elaseJapan futhi itholakala esifundeni iShizuoka esiqhingini saseHonshu. Igama eligcwele laseJapan yiFuji-san yize libizwa ngamanye amagama afana neFujisan, Fuji-no-Yama, Fuji-no-Takane neHuzi, phakathi kwabanye. Kuwo wonke umlando ubusaziwa njengenye yezintaba-mlilo ezinhle kakhulu emhlabeni, lokhu kudale ukuthi kube wuphawu lweJapan.
Kulesi sihloko sizokutshela ngazo zonke izici, i-geology kanye nokufuna ukwazi kweNtaba iFuji.
Izici eziyinhloko
Ingenye yezintaba-mlilo ezidume kakhulu emhlabeni futhi bekuyisihloko esivela njalo sobuciko bendabuko baseJapan. Izwe lonke lasentshonalanga likhonjwe njengeNtaba iFuji. Inani eliphakeme kakhulu lifinyelela kumamitha we-3.375 futhi lifakwe ohlwini lwezazi zokwakheka komhlaba ezivamile ezisebenza ngentaba-mlilo. Lokhu kusho ukuthi iyaqhubeka nokukhombisa izimpawu zomsebenzi wentaba-mlilo ngokuqhubekayo futhi kusho ukuthi iqhume iminyaka eyizi-10.000 XNUMX edlule. Yize lokhu kubonakala kujwayelekile kwentaba-mlilo esebenzayo, uma sikhuluma ngokuma komhlaba.
Futhi ukuthi intaba-mlilo esebenzayo ihlaziywa kusukela esikhathini se- isikhathi sokuma komhlaba. Lokhu kusho ukuthi ukuqhuma kufanele kubekelwe isikhathi esikalini se-geological kanye non-human. Okwe-volcano, iminyaka eyi-100 ayisona isikhathi nhlobo. Eduze kwale ntaba kukhona amachibi aseKawaguchi, Yamanaka, Motosu, Shoji naseSai, futhi futhi iphakathi kweFuji-Hakone-Izu National Park, okuyindawo evakashelwa kakhulu ezweni.
I-morphology yale volcano ikhombisa ngendlela ecishe ifane. Okuphezulu esikubalulile ngenhla kunesimo sezulu sakhona. Lesi simo sezulu yi-tundra futhi siqopha amazinga okushisa asukela ku -38 degrees kuya ku-18 degrees. Kuwo wonke amakhoni ayingxenye yoshimula wentaba-mlilo indawo yokuhlala izinhlobo eziningi zezilwane nezitshalo. Inezinhlobo eziningi zezilwane ezincelisayo, ezifinyelela ezinhlotsheni ezingama-37.
Ukwakhiwa kweNtaba iFuji
Kuyi-stratovolcano noma i-volcano eyinhlanganisela eyakhiwa izingqimba eziningana zamatshe, umlotha, neLada eqinile. Yintaba-mlilo edinge izinkulungwane nezinkulungwane zeminyaka ukwakheka kwayo njengoba sazi namuhla. Itholakala phakathi kwamapuleti ama-tectonic ama-3 aziwa ngokuthi amapuleti aseNyakatho Melika, e-Euro-Asia nasePhilippines. Ngaphezu kwalokho, kubhekiswe ngqo kumapuleti amancane e-Okhotk nase-Amuria.
Le volcano kuthiwa yenziwa cishe iminyaka elinganiselwa eminyakeni engama-40.000. Siyabona ukuthi okwamanje iyingxenye yeqembu lezintaba-mlilo ezigqagqene. Ngaphambi kokuba kwakhiwe iMount Fuji, ezinye izintaba-mlilo zase zivele zisebenza, njenge-Ashitaka, Hakone neKomitake Ashitaka, Hakone neKomitake.
Ngemuva kokuqhuma okuhlukahlukene okwenzekile esikhathini esiyiminyaka engaba ngu-80.000 intaba-mlilo engamamitha ayi-3.000 XNUMX ukuphakama yadalwa eyaziwa ngokuthi iKo-Fuji. Kamuva, cishe eminyakeni eyi-17.000 eyedlule, ukugeleza okukhulu kwelava kwammboza ngokuphelele futhi kancane kancane kwaze kwaba kwakhiwa iShin-Fuji noma iNew Fuji. Zonke lezi yizigaba intaba edlule kuzo njengoba sazi namuhla.
Ngakho-ke, singabiza intaba-mlilo yamanje njengomkhiqizo womsebenzi wentaba-mlilo kusuka ekuceleni kwazo zonke izingqimba zezinto zokwakha ukuze zixoshe izintaba-mlilo ezedlule. Lokhu kusiholela ekutheni sithathe ngokuthi ngaphansi kwentaba-mlilo yamanje kunezintaba-mlilo zasendulo esizishilo.
Ukuqhuma kweMount Fuji
Ukuqhuma kokugcina kwale ntaba-mlilo kwaqoshwa ngo-1708. Kodwa-ke, lokhu kuyenza ihlukaniswe njenge-volcano esebenzayo ngoba inengozi enkulu lapho yethula i-fumaroles futhi ikhombisa izimpawu zomsebenzi wokuzamazama komhlaba. Ngokwe-Global Volcanism Programme yeSmithsonian Institution, Ukuqhuma okuqinisekisiwe okungama-58 sekurekhodwe kwathi i-9 ikhonjwe ngokuqiniseka okungaqinisekile. Lona yiwo wonke umsebenzi iNtaba iFuji eye yaba nawo ngesikhathi samarekhodi wabantu.
Ngesikhathi sokuvela kwayo kuleplanethi kwakuyintaba-mlilo esebenzayo kakhulu njengobuningi babo. Cishe zonke izintaba-mlilo ziyasebenza lapho zisencane futhi umsebenzi wazo uyaphela noma uncipha eminyakeni edlule. Ngemuva kokwakhiwa kweFuji entsha, bekukhona isikhathi sokungasebenzi kuze kube yiminyaka engaba ngu-5.000 XNUMX edlule. Yilapho ukuqhuma kuye kwagqama khona ngokuba namandla amakhulu noma inani elikhulu lodaka oluphonswe. Ngokwesibonelo, okunye kokuqhuma okurekhodiwe kwale volcano kwenzeka esikhathini sikaJogan ngo-864. Lokhu kuqhuma kudonse izinsuku eziyishumi lapho bekujikijelwa khona umlotha nezinye izinto ezifinyelela amabanga amade.
Uma ngaleso sikhathi abantu ababezungezile babencane kakhulu, ngokuhlaziya nje umonakalo ongaba khona namuhla, kuyenza ibe yintaba-mlilo enkulu. Ubungozi bentaba-mlilo noma ubungozi bayo abunqunywa kuphela yi izinhlobo zemihelo noma i-morphology yayo, kepha ngomonakalo ongaba khona kungadala. Okusho ukuthi, intaba-mlilo ingakhipha inani elikhulu lamatshe noma amagesi, kepha azikho izidalwa eziphilayo, abantu, ingqalasizinda, njll. ukuthi ingalimaza, ingozi yayo izoba ncane. Isibonelo, intaba-mlilo maphakathi nolwandle ayinabungozi kangako.
Ukuqhuma kokugcina kweNtaba iFuji kubuyela emuva ku-1708 futhi kwaziwa ngokuthi ukuqhuma kweNtaba iFuji esikhathini sanamuhla seHōei. Kulokhu kuqhuma akuzange kuveze ukugeleza kodaka oluya ngaphandle kodwa kwaxosha umlotha, amabhomu wentaba-mlilo nezinye izinto eziqinile ezafika eTokyo. Lo mcimbi ungamenyezelwa ngenxa yokuzamazama komhlaba okwandulele okwakungokukhulu kunakho konke emlandweni waseJapan, okwaba sesibili ngokuqina kokuzamazama komhlaba ngemuva kwalokhu okwenzeka ngo-0.8. Kusukela lapho, akukho ukuqhuma okuqinisekisiwe le ntabamlilo.
INtaba iFuji, yize ibhekwa njengentaba-mlilo eyingozi, iyindawo eheha izivakashi. Ngiyethemba ukuthi ngalolu lwazi ungafunda kabanzi ngeNtaba iFuji.