Lava


I-Stratovulkan Lavu ifumaneka kwisiqithi saseJava e- Indonesia . I-volcano yindawo elambileyo, umsebenzi wokugqibela wabhalwa ngoNovemba 28, 1885. Namhlanje, iLava yenye yeyona ndawo inomdla kakhulu yokunyuka. Kwakhona, abahambahambayo bahlangana apha ngonyaka, okwenza le ntaba ibe yinto ephakathi kwendawo yonqulo kunye nesayithi elithandwayo.

Yintoni enomdla ngoLuthando?

I-volcano iyabonakala ngenxa yobuhle bayo. Ubunqabileyo balo bukho kwinto yokuba ifomu engavumelekanga ye-stratovolcano kwaye ibonisa intaba yonke intaba elineentaba eziliqela, ii-craters kunye nemigqomo. Ephantse neLava ibonakala ikhangayo, kunye nokude.

Umvuzo wabakhenkethi abaye banqoba indlela ende ukuya phezulu kwi-Khargo Dahlem abayi kuba yimbono emangalisayo yeentaba ezinqabileyo iMerbabu ne- Merapi, kodwa kunye nokutyelela kwitempile yobuBuddha. Kukho rhoqo iindawo zokuhamba. Ba thandaza kwizakhiwo ezithobekileyo ezifumaneka ecaleni kwetempile. Ngokwembali, indawo apho itempile ikhona khona indawo yokukhanyiswa komnye wabalawuli be-Majapahita. Ngoko ke, iziqwenga ze Kharg Dalem kunye neKharga Dumiling zibhekwa njengezingcwele. AmaSulumane akholelwa ukuba uDahlem unceda ukubonakalisa ubuchule bentliziyo yomntu.

Ukunyuka kweLava

Ukunyuka kwi-stratovolcano kwenzeka kwinani le-Khargo Demak, elingama-3170m ukuphakama. Kukho iindlela ezintathu:

  1. Ukusuka etempileni yaseCheto. Ekuqaleni komendo kukho impompo yamanzi. Ukunyuka kuya kuthatha iiyure eziyi-8.
  2. Cemaro Kandang. Abakhenkethi bafikelela kwiintlanganiso kuma-4.5-5.5 iiyure.
  3. Cemaro Sewu, apho kukho abantu abaninzi. Apha, amanyathelo aphakamileyo ngamatye ayafakwa, ngoko le ndlela ihamba kakuhle, kodwa kunzima ukunyuka. Ukunyuka kuya kuthatha malunga neeyure ezingama-5, ukuzala-3.5.

Ngokuqhelekileyo iindwendwe zidlula emigqeni emibini: enye inyukela phezulu, enye-yehla. Indlela ethandwa kakhulu yiCheto-Chemaro Kandang. Phakathi kwamacandelo alo amabini ayikho ngaphezu kweekhilomitha ezili-1.5, ngoko le ndlela ikhelele labo bafika eLava ngemoto. Yiya emotweni emiswe ngokukhawuleza ngokwaneleyo.

Ukunyuka kuyadlula kwiindawo ezixhotywe kakhulu, kwezinye iindawo nakwiziteyathelo zamatye zifumaneka. Abasomashishini basekhaya baye bavula i-varungi encinci, iikofu zendabuko zase-Indonesian, apho ungasiphuza itiye elitshisayo kwaye ube ne-snack. Kwezinye zazo zikhona amagumbi okuphumla apho kunokwenzeka khona ukuphumla nokulala. Inkqubo yokunyuka ngokuqinisekileyo iquka intlanganiso yesantya-yinto ebusayo. Ngeenyanga zasebusika, ukushisa okuphezulu kungaphantsi kwe-zero, nto leyo ingabonwa ngokukhawuleza kwi-crusts e-ice kwii-craters. Kuye kwalungiselelwa intlanganiso yokusa kwelanga: thabatha kunye neempahla ezifudumele kunye ne-thermos ngehayiti elishisayo.

Uhlala phi?

Ngasemva kweLava, kukho idolophana encinci yeTavangamangu apho ungahlawula khona indawo yokuhlala. Ukunyuka kwentaba kudla ngokuqala ekuseni, ngoko ke iindwendwe ziqeshisa indlu edolophini usuku, okanye ezimbini ngaphambi kokuya eLvava. Ukongeza, iThawangamang nayo inezinto ezithakazelisayo: iitempile, iimfesane kunye ne-bazaar yendabuko. Ukutyelela idolophu kuba ibhonasi ebumnandi ukuhamba.

Kwizixeko eziphambili, i- Surakarta ikufutshane ne-stratovolcano, i-23 km nje. Kuyo unokrazula igumbi kwihotele efanelekileyo okanye kwihostela elula kakhulu.

Indlela yokufikelela entabeni?

Unokufika kwiLava ukusuka kwicala lasentshonalanga ngomzila wesitimela, ngenxa yoko kufuneka uhambe kwisikhululo "Solo Jebres" okanye ngebhasi-terminal "Tirtonadi". Ukusuka kwisikhululo kunye nesiphelo kufuneka ufike eTawangmanga nge-shuttle ibhasi. Ukusuka edolophini ukuya kutsho kwe-volcano kungafihla ibhasi, intengo yetikiti ayidluli kwi-$ 1.3.