- Indawo: Hakone, Kanagawa, eJapan
I-archipelago apho iJapan ikhona khona kumxube weeplates ze-lithospheric. Yingakho ilizwe livame ukugungqiswa ngamazwe, kwaye izindlu zakhiwe ngamaphepha elayisi. Nangona kunjalo, kukho nakwintsikelelo yayo. Hayi, kungekhona kwiindyikima ezininzi, kodwa nakweminye imbonakalo yomsebenzi wesimo sezulu - malunga neNtlambo yamaGesi e-Ovakudani.
Yintoni le ndawo iya kubangela umdla kubakhenkethi?
Intlambo yamanzi i-Ovakudani yavuka emva kokuqhuma kwe- volcano i- Hakone, eyenzeka ngaphezu kweminyaka engama-3 eyadlulayo. Emva kwesi siganeko, intaba-mlilo emininzi yenziwe ngekrakra yayo, ebanzi ubude beekhilomitha ezili-13, kunye nemithombo yamasulfure yaqala ukuphuma.
Namhlanje, i-Ovakudani Valley of Geysers kufuneka ukuba iindwendwe ezininzi zezokhenketho. Into yokuqala apho umhambi evakalelwa ngayo xa efika kule ndawo yiphunga lesulfure. Nangona kunjalo, imbono ebonakalayo phambi khenketho ibonakala kakhulu - iindawo eziluhlaza zemithi, iintaba zeentaba kunye namanzi aseLake Asinoko.
Kukho kwiNtlambo yee-geysers iOvakudan kunye nesiko sayo. Ngokwembali, nabani na odla iqanda elimnyama elikhupha emithonjeni yamanzi , impilo yeminyaka eyi-10 iyongezwa. Ngenxa yokuba bayayipheka kuloo mijelo efanayo ye-sulfuric, kutheni igobolondo ithola umbala ongaqhelekanga. Ngaphandle koko, ungakhathazeki - iqanda njengeqanda, ukubunjwa kwalo emva kwendlela yokupheka ayitshintshi. Ngendlela, le "iipulo" zombala omnyama zithengiswa, kwinqanaba le-volcano - xa kungenakukwazi ukuphakama kwimithombo, kodwa ufuna ukuzinika ixesha elide. Iindleko ziyahluka phakathi kwe-$ 4.5.
Indlela yokufikelela kwiNtlambo yeGeys of Ovakudani?
Imoto yekhefu yeHakone Ropeway iholela eOvakudun. Ukuqala kwayo kukude kwe-1044 m ngaphezu kwelwandle. Ngemizuzu eyi-8 kuphela i-gondola izokuthatha emithonjeni yamatrha, ngexesha elinye livule ithuba elihle lokujonga malunga nommandla.
Ukuza apha eTokyo , uthathe isitimela ukuya kwisikhululo se-Odawara, uze utshintshe kumgca weHakone Tozan, oya kwisikhululo saseGora.