Intaba yaseFuji eJapan: imvelaphi, imbali kunye nobude beentaba. Ukubona kweNtaba yeFuji (isithunzi)

Ikhadi loshishino langempela laseJapan yiNtaba yeFiji. Iifoto zale ndlela yokulala i-stratovolcano igugu zonke iindlela zokutyelela ngeli lizwe. Intaba ihlanganiswe neengoma kunye neengcamango, ezihlabelelwa yizibongo, zenziwa kwimifanekiso yabaculi abadumileyo. Yintoni ezisa udumo olufanayo kuFujiyama? Mhlawumbi yiphondo ephezulu eYapan? Kunokwenzeka ukuba, kule meko, imbali yentaba idlala, kwaye ayikho imida yayo yeendawo. Ngombono wamaJapan, uFijiyama ude kakhulu nomfanekiso wakhe wangempela. Nangona umntu ofundisiweyo uqinisekile ukuba imiphefumlo yabakhanyiswayo ihlala emilonyeni yentshonalanga. Ngoko ke, amaJapan abiza ngenhlonipho - i-Fuji-san. Ukucaciswa kwayo kubumba iqela eligqibeleleyo. Eyona nto iphezulu ingcwele yeShinto. Kwaye kwisiseko, intsomi "Ihlathi lokuzibulala" likhula. Masizame ukwahlula inyaniso kwizinto eziyinyani kwaye sinqume ukuba yintoni na into - iNtaba iFuji.

Iinkcukacha zesayensi zesomileyo

Njengoko sele kukhankanywe, iPijiyama iyona ndawo ephakamileyo kuyo yonke indawo yaseJapan, kwaye ngelo xesha i-stratovolcano ekhona. Kukho inqabileyo kwisiqithi saseHonshu, engaphelelanga iikhilomitha ezilikhulu ukusuka eTokyo. Kwiintsuku ezicacileyo ukusuka kwipropati yaseJapan, unokubona nakwintshona-ntshona-ntshona i-mountain-shining mountain peak. Ubude beFiji bubungamamitha angama-3 776 ngaphezu kweli nqanaba lolwandle. Le ntaba iyimigaqo yeentaba zaseJapan. Ngako oko kuthiwa ngamatye amathathu kuMhlaba weNgqungquthela oyiNgqungquthela oyiNgisi uWilliam Gouland. Wakhupha incwadi ye-Yurophu ethi "Isikhokelo saseJapan", apho wafanisa khona iintaba zeentaba zendawo kunye neentaba. Nangona kunjalo, iNtaba yaseJapan yaseFanji ayiyi-volcano efile. Ixesha lokugqibela laqhuma ngo-1708, kwaye linamandla kakhulu. Emva koko izitrato zase-Edo (ngoku iTokyo) zifihlile umlotha we-volcanic ash ash 15 cm. Ngethuba le mpuphu, iCroat yaseHoi-zan yabonakala, iphikisa iindawo ezifanelekileyo zeFuji.

Imbali

Iingcali zenzululwazi zihlula i-volcano endala neyeNtshonalanga. Iyokuqala yenziwa iminyaka eyi-80 eyiminyaka edlulileyo. Wayekhuthele. Kwaye malunga neminyaka eyi-20 lamawaka edlulileyo kwakukho ukukhuphuka kwamandla amakhulu kwaye okude (iminyaka emininzi). Ngenxa yoko, i-lava ivimbile imilambo kwaye yakha i-"Five Five Fuji Lakes" enhle kakhulu, kwaye i-volcano endala yaphela ngokupheleleyo. Intsha yaqala ukukhula malunga ne-11 lamawaka eyadlulayo. Umsebenzi wakhe waqala ukunyulwa kwii-annals ukusuka kwi-781 ukuya phambili. Ukususela ngeli xesha, kubekho ukuqhuma kwe-12. Elona likhulu, ehamba kunye nokukhululwa kwe-basalt lava, yabonwa kwi-800th, 864 no-1708 iminyaka. INtaba iFuji eJapan kwaye ngoku ayizange ilahlekelwe umsebenzi, kodwa ilele nje. Inyaniso yokuba yi-volcano ibonakala ngamanzi amaninzi atshisayo. Kodwa i-crater (ngamamitha ama-500 ububanzi kunye no-200 m inzulu) ngoku iindawo ezikhuselekileyo.

UFijiyama kwisiko laseJapan

I-Stratovulkan kangangeminyaka eyi-500 iyinhloko eyaziwayo kwizobugcisa. Oku, ngaphezu kwakho konke, kwanegalelo kwiimbali zamandulo neembali. Kwakukholelwa ukuba phezulu kwentaba, emlonyeni, amadoda akhanyisiweyo aseTaoist ahlala. Umsi kwi-volcano yiselo lokungafi. Iingqungquthela kunye nabaculi bachaza uFuji-san njengentaba, ephezulu eboshwe yiqhwa elingunaphakade. Nangona kunjalo, ngokwenene ngoJulayi noAgasti, iqhwa liphela ngokupheleleyo. Kwizinkuni, intaba inqabileyo kwaye iphakamileyo, inemithamo engama-45 degrees. Kwakukholelwa ukuba kuphela i-elite eyayingakwazi ukufikelela kuloo ngqungquthela. Ngoko, ngokwembali, ukunyuka okunjalo kwenziwa nguPrince Shogoku. Nangona kunjalo, iimbono zeNtaba iFuji, ezifotwe kwii-angles ezahlukileyo, zibonisa ukuba zintlambo ezintle. Nangona i-volcano iqhubekile ngokuphindaphindiweyo, kwizinto zobubugcisa akukho mfanekiso omnye omele uFujiyama. Mhlawumbi, kuba eJapane, nokuba ne-volcano ayinakuvunyelwa ukubonisa iimvakalelo zabo.

Injongo yezokhenketho yehlabathi

INtaba yaseFuji eJapane yafumana udumo ngaphandle kwelizwe ngenxa yokuqoshwa kwexesha le-Edo. I-Woodcuts kaHokusai no-Hiroshige, ebonisa ukuphakama kwemilingo ephakamileyo ngaphezu kwamafu, yathintela ingcamango yabantu baseYurophu. Kunyaka ngamnye, malunga namawaka amabini amawaka abantu baya kufikelela kwiintlanganiso. Kwaye nangona kunjalo ukuba ukukhuphuka kuvunyelwe iinyanga ezimbini kuphela - ukususela ngoJulayi 1 ukuya ekupheleni kukaAgasti. Kodwa iindwendwe zokuvakatsha azinabo ababoneleli abaphambili beendwendwe kwi-crater ye-volcano. Isabelo sabasemzini phakathi kwabo abenyukela entabeni kuphela 30%. Injongo ephambili yokunyuka kwintlanganiso yindlela yokunyuka inkolo. Phezu kwe-Fuji, ekupheleni kwinqanaba le-crater, ithempile yeShinto itempileni ye-Sengen jinja. Iimonkampani zenkampani ziyi-meteorologists, isistim eso siseduze, kunye ... nabasebenzi beposi. Thumela ikhadi kumthonyama ngokuthe ngqo ukusuka kwintaba engcwele engcwele - oku kubonwa njengesigqibo esihle eJapan.

Uzuko lwehlabathi

NgoJuni 2013, iFujiyama yafakwa kwidilesi ye-UNESCO. Kuyaphawuleka ukuba wazifumanisa kule nhlu ehloniphekileyo kungekhona njengento enomdla, kodwa njengento yelifa lemveli. Le yintlawulo kwimiba emininzi kangangokuba i-volcano iphefumlele abaculi kunye neebongozi ekuveleni. Ngoko ke ngokusemthethweni kwisahlu ye-UNESCO: "INtaba iFuji. Umthombo ongapheliyo wokuphefumlelwa kunye nenkolo yonqulo. " Ukongezelela, i-volcano kunye neenxa zonke ziyingxenye yeFiji-Hakone-Izu - iNdawo yeNdalo yesiZwe. Kwaye amachibi amahlanu - iSi, i-Shodzin, i-Motosu, i-Yamanaka ne-Kawaguchi-yindawo yokuhlala apho abahlali baseTokyo bathanda ukuphumla.

I-Ascent ukuya kuFuji

Ngexesha elivulekele ukuvakhenketha kweentaba, kwiintlambo zeentaba kunamaziko amaninzi okuhlangula, iivenkile kunye ne-Yamagoya - indawo yokuhlala apho unokuchitha khona ubusuku. I-Fujiyama ihlukaniswe ngamanqanaba alishumi (ibarome). Ukufikelela kweyesihlanu kuya kufakwa ngebhasi, nangona kukho iindlela ezisemthethweni ezisuka kwinqanaba lomlilo. Inombolo enkulu yeYamagoy, iivenkile kunye nezinye izibonelelo zotyelelo zigcinwa kwintlambo esenyakatho. Endleleni, uya kufumana ama-biotoilets. Kuzo kwanebhodi yesitya yangasese (iJapan efanayo!) Ifudumala ukusuka kwiibhetri zelanga. UFuji udinga umgudu omkhulu kwiinquba. Iiyure ezisibhozo zokuphakamisa kunye neetlanu zokuzala, kwaye oku akubalanga ixesha lokumisa nokuchitha ubusuku. Yaye ukuba uthetha umgangatho ukusuka kwinqanaba lesihlanu, unako ukuhlala ngaphakathi kwimihla yokukhanya enye : iiyure ezintathu kunye neebini ezantsi.

Unonophelo oluyimfuneko

Ephantse phezulu ungabona i-glide ehambayo. Iindiza ezinjalo ziyakubungozi, kuba iNtaba iFiji idume ngokuba yimimoya yayo enamandla. Kwakhona, abanye abakhenkethi bathatha iindawo eziphakamileyo ezikhokelela umthambeka, malunga neendlela zokuhamba. Enyanisweni, le mizila eyingozi yenzelwe i-bulldozers, ehambisa amalungiselelo e-Yamagoya kwaye ihlise abavakhenkethi abachaphazelekayo. Hamba ngale ndlela, nangona kubonakala ngathi uchanekileyo kwendlela, kuyingozi. Akusiyo isidumbu, kwaye amatye angakulimaza wena kuphela, kodwa nabahamba ngeendlela zokuhamba. Ukulahla udoti kuwo wonke umzila onqatshelwe. Kwiintengiso kwiindawo ezithambileyo uza kuthengiswa ngamanzi kuphela ngokutshintshela ibhotile engenanto.

Kutheni ukhuphukela phezulu kwintaba

Nangona unokwenyuka uye wehla ukusuka phezulu kweFuji ngelinye ilanga lokukhanya, abatyeleli abaninzi banqwenela ukuchitha ubusuku kwishumi, esona sikhulu, kwisikhululo esincane. Yintoni eyenza ukuba banyamezele kubanda kwaye badle kunye nama-curry noodle kufuphi nesitofu samafutha (kathathu ngaphezu kwexabiso lokudlela kunezakhiwo zokudlela)? Inyaniso kukuba iNtaba iFuji idume ngokusa kwayo. Kwaye kuba bonke abavakhenkethi ngehora lesine ekuseni baya kushiya izikhwama zokulala baze bajonge ngeengqungquthela kummandla we-volcano ukuhlangabezana nelanga. Kodwa nangona ufika phezulu kwimini emva kwenjongo yokubuyela ekhaya ebumnyameni, uya kuba namava angalibalekiyo. Ingqungquthela yentaba ifana ne-Martian landscape. Ummandla wonke we-summit uhlanganiswe ngamatye emnyama. Isikhululo sezulu kunye nezibingelelo ezingcwele zizalisa umfanekiso ongaqhelekanga.

Intaba yaseFuji eJapan: ihlathi lokuzibulala

Akuthandi kakhulu kunye ne-Dziukai. Ukuguqulelwa kwiJapan kuthetha "uLwandle lwemithi". Ngexesha lokugqitywa kokugqibela, i-lava ayizange ifuthe iincinci, malunga neekhilomitha ezili-35 zecrafti, iqela lehlathi phantsi kwentaba. Ukususela ngoko, imithi ikhulile kakhulu kangangokuthi yakha intente encinci yesithsaba kunye ne-boxwood. Kuthiwa ukuba iintsapho ezihluphekileyo zangaphambili zazisa abantu abadala kunye nabantwana abangenakuzondla ngokwabo kulehlathi. Yaye ngokutsho kweenkolelo zaseJapan, imiphefumlo yalabo bafa ngokufa okubuhlungu kuhleli kweli hlabathi ukuze babuyisele kwizinto eziphilayo. Kwaye ihlathi eNtabeni iFiji yaba yinto yohambo lokuzibulala. Abathandwayo abathandwayo, abantu abalahlekelwa ingqiqo ebomini, batshiswe emsebenzini ngaphandle kwanoma yiziphi iintlobo zokuphakamisa i-plankton ye-ofisi-konke ukukhawuleza kwi-Dziukai. Inani lamalungu atholakala kuphela lihluka ukusuka kwi-70 ukuya kwi-100 ngonyaka. Ukuxhaswa nguZukai kwinani lokuzibulala, kuphela i-Golden Gate Bridge (iSan Francisco).