- Idilesi: Solheimajokull, Iceland;
- Inqaku eliphakamileyo: 1300 iimitha ngaphezu kweli nqanaba lolwandle;
- Ubukhulu: ubude - 8 km, ububanzi - 2 km.
I-Iceland idume ngokukhenkceleka kwezinto eziqhelekileyo ezinokubethisa nabani na. Phakathi kwazo yi-glacier i-Soulheimajkutl, ehlala kumazantsi ase siqithi kwaye yakha unxweme olungapheliyo.
Indawo kunye nobukhulu
Ngomnye wezinto ezinjalo zendalo, kodwa enye yezobuhle obuhle kangaka. Itholakala kwiSowleymajkutlu kufuphi, ukusuka kutshanje, i-Eyyafyadlyayukudl.
Ukuqhwala kweqhwa kwehla kuvela kwelinye icebo, ngaphantsi kobunzima kakhulu kuthi igama elithi - Myrdalsjökull. I-Soulheimajkutl idlulisela phantse ngqo kunxweme lolwandle, ehlanganiswe ngeesanti.
I-glacier iya kufikelela ubude beekhilomitha ezili-11, kwaye ububanzi bayo buhluka ukusuka kwi-1 kuya kweekhilomitha ezimbini kwiindawo ezahlukeneyo.
Iqhwa elimnyama nelomhlophe
Ngokuqhelekileyo kukholelwa ukuba i-glaciers ine-white hue, ene-blue bluhlaza, kodwa oku akusebenzi ku-Soulheimmaktüll. Ihlanganiswe ngengubo emnyama - ngumlotha womlilo oqhumayo emva kokuqhuma.
Kuyaphawuleka ukuba umlotha uphatha kakubi nje ukubonakala kwendiza, kodwa ubukhulu bayo. Emva kwakho konke, umlotha omnyama uphephe ngamandla, ngaphantsi kokushisa kakhulu, ukukhanya kwelanga, kwaye oku kuholele ekuqhenqeni kweqhwa phantsi kwalo.
Kwezinye iindawo, ulawulo lomlotha lukhulu kakhulu, lukhulu kunye nomfaniswano ongeke ucinge ngokukhawuleza malunga neqhwa. Nangona, kunjalo, imibala emhlophe ikhona nakwaneleyo ngokwaneleyo. Ngokukodwa xa ukhangela i-glacier ukusuka phezulu.
Ngendlela, indawo ephezulu yeqonga le-glacier itholakala kwindawo ephakamileyo yee-1300 kumitha ngaphezulu kwezinga elwandle. Kwaye iphantsi kakhulu - kuphela kwizinga leemitha ezili-100 ngaphezulu kwezinga elwandle.
Ixesha elizayo leqhwa
Ngokuncedwa ngamaqhwala, izazinzulu zifunda iimpawu zokuphuhliswa kwemozulu kunye nesimo semvelo esiqithi, kwiimeko ezahlukeneyo zembali. Ngokukodwa, ngaphezu kweminyaka yomsebenzi wayo, iingcali kulo mbandela ziye zakwazi ukufumana ulwazi olunolwazi nolunomdla.
Ngoko ke, yonke idatha efunyenwe kwiminyaka yokulinganisa, ukuhlaziywa kweenguqu zemozulu kwavumela oososayensi ukuba baqikelele ukuba kuya kuba ngama-100 ukuya kuma-200 ubudala, njengoko i-glacier iyancibilika.
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Amanzi phantsi kweqhwa
Ngaphantsi kobunzima beqhankqalaza ngoku kwaye yakha umlambo, obangela ukumangalisa. Emva koko, iqhwa phezulu liqinileyo kwaye limile. Nangona kunjalo, ngaphandle kobunzima obukhulu, i-glacier igxuma ngokukhawuleza kwaye ngenxa yokuxubana okukhulu, ukushisa kweengqimba ezingaphantsi kweqhwala kuphakama kwaye baqala ukuyibilika. Oko ke, kukhokelela ekutheni i-glazing ephezulu kakhulu, ukuxubana kunye nokufudumala okukhulu kweendawo eziphantsi. Njengoko ubona, kuvela isangqa esichukumisayo.
Nangona, ukuba i-top gla glacier ikhula, ukuchithwa kwecandelo eliphantsi akuyi kubachaphazela kakubi ubukhulu be-Soulheimmaktylu, kodwa, njengoko kubhekiswe ngasentla, kwiminyaka yamuva iyancinci.
Ndingafika njani?
I-Glacier yeSölheimajkütl ifumaneka malunga neekhilomitha ezili-160 ukusuka kwisikhululo sase-Iceland, iReykjavik . Kukho rhoqo ukulungiswa kohambo lwezokhenketho, kunye nezikhokelo ezinamava kunye nezikhokelo.
Unako ukuya kwinqanaba le-glacier kunye nawe ngokuqasha imoto. Ixesha lokuhamba li malunga neeyure ezingama-2.5. Kodwa, kwakhona, olu khetho lunconywa kuphela ukuba awuyi kuhamba kwiqhwa, kodwa ufuna ukuwujonga kude. Ukuhamba ngaphandle kwesikhokelo kubangelwa izingozi.
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