- Ikheli: Solheimajokull, Iceland;
- Iphuzu eliphakeme kakhulu: amamitha angu-1300 ngaphezulu kwezinga lolwandle;
- Usayizi: ubude - 8 km, ububanzi - 2 km.
I-Iceland idume ngokukhangayo kwayo yemvelo okungathandeka noma ubani. Phakathi kwazo yiSlaimaimajkutl ye-glacier, esemazweni aseningizimu asesiqhingini futhi yakha ogwini olungajwayelekile.
Indawo nobukhulu
Ungenye yezinto ezinjalo zemvelo, kodwa ubuhle obuhle kangaka. Itholakala eSowleymajkutlu esiseduze, kusukela esanda kuqhuma, i-Eyyafyadlyayukudl intaba-mlilo.
Ukuhamba kweqhwa kwehla cishe kusuka kwelinye i-glacier, ngaphansi kobunzima kakhulu kithi igama elithi - Myrdalsjökull. I-Soulheimajkutl idlulisela cishe ngqo ogwini lolwandle, ehlanganiswe ngezihlabathi.
I-glacier ihlanganisa ubude bamakhilomitha angu-11, ububanzi bayo buhluka ukusuka ku-1 kuya ku-2 amakhilomitha ezindaweni ezingefani.
I-glacier emnyama nemhlophe
Ngokuvamile bakholelwa ukuthi ama-glaciers ane-white hue, ene-blue eluhlaza, kodwa lokhu akusebenzi ku-Soulheimmaktüll. Ihlanganiswe ngengubo emnyama - ngumlotha oshayayo ovunguvungu ngemuva kokuqhuma.
Kuyaphawuleka ukuthi umlotha uthinta kabi hhayi ukubukeka kwe-glacier, kodwa nobukhulu bawo. Phela, umlotha omnyama ugcwele ukushisa, ngaphansi kokushisa kakhulu, imisebe yelanga, futhi lokhu kuholela ekuqhenqeni kweqhwa ngaphansi kwalo.
Kwezinye izindawo, uhlaka lomlotha lukhulu kangaka, lukhulu futhi lufanelwe ukuthi ngeke ucabange ngokushesha ngeqhwa. Nakuba kunjalo, imibala emhlophe nayo ikhona ngokwanele okwanele. Ikakhulukazi uma ubheka i-glacier kusukela phansi phezulu.
Ngendlela, indawo ephakeme kakhulu ye-glacier itholakala endaweni ephakeme ngamamitha angu-1300 ngaphezu kolwandle. Futhi ezansi kakhulu - kuphela ezingeni lamamitha angu-100 ngaphezu kwezinga lolwandle.
Ikusasa le-glacier
Ngesiza sama-glaciers, ososayensi bafunda izici zokuthuthukiswa kwesimo sezulu kanye nesimo semvelo esiqhingini, ngezikhathi ezahlukene zomlando. Ngokuyinhloko, ngaphezu kweminyaka yomsebenzi wayo, ochwepheshe kule ndaba baye bakwazi ukuthola ulwazi oluningi oluwusizo nolusithakazelisayo.
Ngakho-ke, yonke idatha etholakalayo eminyakeni yokulinganisa, ukuhlaziywa kweshintsho sezulu kwavumela ososayensi ukuba babikezele ukuthi kuzoba iminyaka engu-100 kuya kweyama-200, njengoba i-glacier iyancibilika ngokuphelele.
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Amanzi ngaphansi kwe-glacier
Ngaphansi kokuqina kweqhwa manje bese kudala umfula, okubangela ukumangala. Phela, iqhwa phezulu lihle kakhulu futhi limile ngempela. Kodwa-ke, ngenxa yobuningi obukhulu, i-glacier igxuma kancane kancane ngenxa yokungqubuzana okukhulu, izinga lokushisa kwezingxenye eziphansi ze-glacier liphuma futhi liqala ukucibilika. Lokho, kuholela ekutheni kube nokushisa okukhulu kwe-glacier, ukushayisana nokushisa okungaphezulu nakakhulu kwezigaba ezingezansi. Njengoba ubona, kuvela umbuthano ononya.
Nakuba, uma phezulu kwe-glacier ikhula, ukuqubuka kwengxenye engezansi ngeke kuthinte kabi usayizi we-Soulheimmaktylu, kodwa, njengoba kukhulunywe ngenhla, eminyakeni yamuva sekuye kwaba ncane kakhulu.
Ungafika kanjani?
I-Glacier yeSölheimajkütl itholakala ngamakhilomitha angu-160 ukusuka enhloko-dolobha yase-Iceland, eReykjavik . Kuvame ukuvakashelwa ukuvakasha okuhleliwe, ngokuqondiswa okuhlangenwe nakho neziqondiso.
Ungaya ku-glacier nawe ngokwakho ukuqasha imoto. Isikhathi sokuhamba cishe amahora angu-2.5. Kodwa, futhi, lokhu kunconywa kunconywa kuphela uma ungahambi nge-glacier, kodwa ufuna ukuyibuka ibanga. Ukuhamba ngaphandle komhlahlandlela kugcwele izingozi.
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