Ngokuqinisekileyo wakhe wambona kolunye uthotho lweopopayi baseJapan INtaba iFuji. Yeyona ntaba-mlilo idumileyo kuyo yonke iJapan kwaye ikwisithili saseShizuoka kwisiqithi saseHonshu. Igama elipheleleyo ngesiJapan yiFuji-san nangona ikwabizwa ngamanye amagama anje ngeFujisan, Fuji-no-Yama, Fuji-no-Takane kunye neHuzi, phakathi kwabanye. Ukutyhubela imbali ibisaziwa njengeyona ntaba-mlilo intle ehlabathini, oku kubangele ukuba ibe luphawu lweJapan.
Kweli nqaku siza kukuxelela ngazo zonke iimpawu, ijiology kunye nomdla weNtaba iFuji.
Iimpawu eziphambili
Yenye yeentaba-mlilo ezidumileyo ehlabathini kwaye ibingumxholo ophindaphindayo wobugcisa bemveli baseJapan. Ilizwe lonke lasentshona lichongiwe kwiNtaba iFuji. Incopho ephezulu ifikelela kwiimitha ezingama-3.375 kwaye idweliswe ziijoloji ezisebenzayo zentaba-mlilo. Oku kuthetha ukuba iyaqhubeka nokubonisa iimpawu zomsebenzi wentaba-mlilo ngokuqhubekekayo kwaye kuthetha ukuba iqhume kule minyaka ili-10.000 XNUMX idlulileyo. Nangona oku kubonakala kuyinto eqhelekileyo kwintaba-mlilo esebenzayo, ngokuthetha ngokwendawo yayo, kunjalo.
Kwaye kukuba intaba-mlilo esebenzayo ihlaziywa ukusuka kwixesha le Ixesha lejoloji. Oku kuthetha ukuba ugqabhuko-mlilo kufuneka lubekelwe ixesha kwisikali sejoloji kunye nesingeyoyabantu. Kwi-volcano, iminyaka eli-100 ayilixesha kwaphela. Kummandla wale ntaba kukho amachibi aseKawaguchi, Yamanaka, Motosu, eSaji naseSai, kwaye ikwindawo yePaki yeSizwe iFuji-Hakone-Izu, eyona ndawo ityelelweyo kweli lizwe.
I-morphology yale volcano ibonakalisa phantse ngokugqibeleleyo. Umphezulu esichazile ngasentla unemozulu yawo. Le mozulu yile tundra kwaye irejista amaqondo obushushu asusela kwi -38 degrees ukuya kwi-18 degrees. Kuyo yonke ikhowuni eyinxalenye yetshimini yentaba-mlilo yindawo yokuhlala yeentlobo ezininzi zezilwanyana nezityalo. Ineentlobo ezininzi zezilwanyana ezanyisayo, ezifikelela kuma-37 eentlobo.
Ukuyilwa kweNtaba iFuji
Yi stratovolcano edibeneyo okanye intaba-mlilo eyenziwe ngamatye aliqela, uthuthu kunye neLada eqinileyo. Yintaba-mlilo efune amawaka kunye namawaka eminyaka ukuyilwa kwayo njengoko sisazi namhlanje. Ime phakathi kwamacwecwe ama-3 eetectonic plates eyaziwa ngokuba yi North American, Euro-Asia kunye ne Philippines. Ukongeza, ikwa ngqo kwi-Okhotk kunye ne-Amuria iipleyiti ezincinci.
Le volcano ibangelwa ngaphezulu okanye ngaphantsi kweminyaka eqikelelweyo malunga neminyaka engama-40.000. Siyabona ukuba okwangoku yinxalenye yeqela leentaba-mlilo ezidlulayo. Ngaphambi kokuba i-Mount Fuji yenziwe, ezinye iintaba-mlilo zazisele zisebenza, njenge Ashitaka, Hakone kunye ne Komitake Ashitaka, Hakone kunye ne Komitake.
Emva kogqabhuko-dubulo olwahlukileyo olwenziweyo kwisithuba esimalunga neminyaka engama-80.000 intaba-mlilo emalunga neemitha ezingama-3.000 XNUMX ukuphakama yadalwa eyaziwa ngokuba yiKo-Fuji. Emva kwexesha, malunga neminyaka eli-17.000 eyadlulayo, ulophu olukhulu lwentaba-mlilo lwalugubungela ngokupheleleyo kwaye ngokuthe ngcembe de kwavela iShin-Fuji okanye iNew Fuji. Zonke ezi ngamanqanaba apho intaba idlule khona njengoko sisazi namhlanje.
Ngesi sizathu, singabiza i-volcano yangoku njengemveliso yomsebenzi wentaba-mlilo ukusuka ekuceleni kwazo zonke iileyili zezinto zokugxotha iintaba-mlilo zangaphambili. Oku kusikhokelela ekubeni sigqibe kwelokuba phantsi kwe-volcano yangoku kukho iintaba-mlilo zamandulo esele sizikhankanyile.
Ukuqhuma kweNtaba iFuji
Ukuqhuma kokugqibela kwale ntaba-mlilo kwarekhodwa ngo-1708. Nangona kunjalo, oku kuyenza ihlelwe njenge-volcano esebenzayo kuba inobungozi obukhulu xa kusungulwa i-fumaroles kwaye ibonisa iimpawu zenyikima. NgokweNkqubo ye-Global Volcanism yeZiko likaSmithsonian, Izidubulo ezingama-58 eziqinisekisiweyo zishicilelwe kwaza kwachongwa ezili-9 zokungaqiniseki ngokuqinisekileyo. Nguwo wonke umsebenzi owenziwe yiNtaba iFuji ngexesha leerekhodi zabantu.
Ngexesha lokuvela kwayo kule planethi yayiyintaba-mlilo esebenzayo njengona uninzi lwazo. Phantse zonke iintaba-mlilo ziyasebenza xa besebancinci kwaye umsebenzi wabo uyayeka okanye uncipha kule minyaka idlulileyo. Emva kokusekwa kweFuji entsha, bekukho ixesha lokungasebenzi kude kube malunga neminyaka engama-5.000 XNUMX eyadlulayo. Kulapho ugqabhuko-dubulo lubonakalise ukuba namandla amakhulu okanye isixa esikhulu selava esilahliweyo. Umzekelo, Olunye ugqabhuko-dubulo lwentaba-mlilo lwenzeka ngexesha likaJogan ngo-864. Olu dubulo luthathe iintsuku ezili-10 ngexesha apho laliphosa uthuthu nezinye izinto ezifikelela imigama emide.
Ukuba ngelo xesha abantu ababebangqongile babebancinci, behlalutya nje umonakalo onokubangelwa namhlanje, kuyenza ibe yintaba-mlilo ephezulu. Umngcipheko wentaba-mlilo okanye ubungozi bayo awugqitywanga kuphela iintlobo zemirhubhe okanye i-morphology yayo, kodwa ngomonakalo onokubangela. Oko kukuthi, intaba-mlilo inokukhupha isixa esikhulu segrabile okanye iigesi, kodwa akukho zinto ziphilayo, abantu, izakhiwo, njl. oko kunokonakalisa, ubungozi bayo buya kuncipha. Umzekelo, intaba-mlilo embindini wolwandle ayinabungozi kangako.
Ukuqhuma kokugqibela kweNtaba iFuji kubuyela kwi-1708 kwaye yaziwa ngokuba kukuqhuma kweNtaba iFuji kule mihla yeHōei. Kolu dubulo aluzange lwenze mlambo ukubaleka ukuya ngaphandle kodwa lukhuphe i-0.8 yeekhilomitha zothuthu, iibhombu zentaba-mlilo kunye nezinye izinto eziqinileyo ezafikelela eTokyo. Lo msitho ungabhengezwa ngenxa yenyikima eyandulelayo neyayiyeyona ibalulekileyo kwimbali yaseJapan, ikwindawo yesibini ngobunyikima emva kwesehlo sika-2011. Ukusukela ngoko, akukho qhushumbo luye lwaqinisekiswa le ntaba-mlilo.
INtaba iFuji, nangona ithathwa njengomngcipheko wentaba-mlilo, ngumtsalane kubakhenkethi. Ndiyathemba ukuba ngolu lwazi unokufunda ngakumbi ngeNtaba iFuji.