- Idilesi: Reykholt, Iceland;
- Umlambo: Kvitau;
- Ububanzi: 900 m.
I-Hrejnfossar ibinzana lesiganeko sommangaliso ongokwemvelo, ongummangaliso ngezinga kunye nobuhle bawo. Uninzi lweemilambo zenziwe zibe luhlu lweefomfolo, ubude obude obuba malunga neekhilomitha. Kwaye ukuqala kwesi senzo yimihlaba yelava eyenziwe emva kokuqhuma kwe-volcano. I-panorama yempompo ibonakala ikhulu.
Ivela phi imilambo?
Ekubonweni kokuqala, kunokuba kubonakale kumnandi ukuba imvula yamanzi ivela kwiintlambo ezibalekela kwi-volcano. Kodwa inkcazo yale ngxaki ilula kakhulu: Intaba-mlilo yaseLaungjökull iphantsi kweGlacier yaseLaungjökull, ngumzali we-Kwituau. Wayekwazi ukwenza umbhede wakhe, owawubeka umgca we-lava kwaye wadlula ngaphaya kwawo. Iliwa eliqhenqileyo le-lava, lavumela amanzi ukuba angene kuwo kwaye ayenze imilambo emininzi, emva koko aphuma emanzini. Ubume babo besaziwa ixesha elide, ngoko ke ukuqala kwegama lamanzi e-"hraun" liguqulelwe ngokuthi "lava". Ukongezelela, amehlo ngokwawo anokuthelekiswa namandla okulahla.
Hrejnfossar kunye neenxa zonke
Icandelo lamaconsi aphelela ngamatye abukhali, kwaye ngokufanayo kufana nehlathi eliqinileyo likhula. Ukunciphisa apha kuwela ngokukhawuleza, ngoko imibala yendawo yendawo iyancibilika kwaye iyintsha. Imvula ehlala rhoqo iqinisa ukuhamba, okwenza ibe namandla ngakumbi. Ngenxa yoko, impompo yehla i-5 m³ yamanzi emlambo isibini.
I-Hrejnfossar yiyona nto ibangelwa kulo mmandla, ngoko ukuthandwa kweendawo zendawo kukhulu kakhulu. Ekufuphi yidolophu yezokhenketho yaseGilsbakki. Kukho izinto ezithakazelisayo, kwaye ukuvakasha kwiindawo ezungezile kubandakanya ukutyelela eHrejnfossar.
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Ndingafika njani?
I-Hrejnfossar ifumaneka kwicala lasentshonalanga ye- Iceland , iikhilomitha eziyi-18 ukusuka kwiReykholt . Ephantse kwiimpawu eziphawulekayo kukho indlela ye-No.518, idibanisa iifomfolo kunye nesixeko, ukuze ufike eHrejnfossar kungcono ukuthatha inkambo yeRikhokho kuqala.