I-volbrano e-Elbrus iyasebenza okanye iphela? Makhe sifumane impendulo

U-Elbrus uthathwa njenge-volcano yobuncinane, kuba i-massifs entaba yale ndawo yenziwa malunga nezigidi ezimashumi amabini edlulileyo, kwaye ukuqhutyelwa kwangoko kwintaba enzima kwenzeka malunga nezigidi ezilishumi elinesihlanu kwiminyaka edlulileyo. Ngoku kuthethwa kwinqanaba lamaqhwaba asele, kodwa amaninzi amakhelwane kunye nokuqhekeka, apho iifom ze-sulfur zivela khona , zibonisa iinkqubo ezimbi ezenzeka ngaphakathi. Ngako-ke i-volcano ye-Elbrus isebenza njani okanye iphela?

Inkcazo ye-volcano

Umthala-mlilo wase-Elbrus ungenye yezinto ezidalwa yendalo - yintaba ephakamileyo. Ukuphakama kweentlanzi kuya kufana. Ukwahlula kwalo kumamitha angamashumi amabini kuphela: inqanaba elithile liphakama ukuya kuma-5621 amamitha ngaphezu kolwandle, okwesibini ukuya kuma-5642 amitha. Ukuxinezeleka okubahlula ngamakhilomitha amathathu kufinyelela kuma-5200 amitha.

Intaba-mlilo i-Elbrus kwimaphu ibonakala ihle kakhulu. Le ntaba inamagama amaninzi ahluka ngokuxhomekeke kulwimi lwesizwe ekuthethwa kuso. Ngokomzekelo, ngesiGeorgia, igama lakhe liya kuzwakala njengeYalbuz, naseArmenian - Alberis. Umthombo wegama lakwa-Elbrus lanamhlanje ligama elithi "antibares", eliyimvelaphi yase-Iranian.

Intaba yeHarsh

I-volbrano e-Elbrus iyasebenza okanye iphela? Ngokusemthethweni kuthathwa njengesiqhwaba esingapheliyo kunye neentaba zayo kunye nemithambeka ihlanganiswa ngamaqhwala, indawo epheleleyo yeekhilomitha ezili-134.5. Ngonyaka uninzi inani labantu lifa, abafuna ukunqoba iingqameko zalo. Iimbangela zokufa kwazo zivele ngokukhawuleza zivele iintambo, ama-avalanchi, ukungabi namava kunye nezimo zezulu eziguqukayo.

Iindawo zokunyuka kwi-slope efanayo zingaba nezinga elihlukeneyo lobunzima. Kwiintlambo ezisempumalanga, iindawo ezininzi zeqhwa ziqokelela, kuba zilula kunezona ntshona kunye nenyakatho, apho kukho iindawo ezininzi ezinqabileyo kunye namanzi omhlaba. Ngasempuma-mpuma yale ntaba ye-mountain massif ibeke , ikhuphukela kwindawo ephakamileyo malunga neekhilomitha ezingama-3750, kukho ihotele. Le ndawo yindawo ehlala kuyo - ilapha apho abakhwelayo nabathandi bemvelo yentaba bevela kwihlabathi lonke.

Izinto malunga nomsebenzi wentshonalanga

Kodwa akukho mntu uyayazi ngokwenene, i-Elbrus intaba-mlilo-iyasebenza okanye iphela. Njengomlilo omtsha-ukuphefumula kwentaba kunokuvela kwindawo entsha, i-giant long-fallen falls can rise with time. Kukho iinkcukacha ezibonisa ukuba uElbrus akayikuphela: kungekude kuyo imithombo yamanzi eshushu. Eyona edume kakhulu kubo nguGila-Su. Amanzi kuwo aya kufumana ukushisa kwama-degrees angamashumi amabini anesine ngaphezu kwe-Celsius. Ubukho bamanzi ashushu busoloko bubonisa ukuba iinkqubo zentaba-mlilo zenzeka ngaphantsi komhlaba. Kwakhona, ukulinganisa kobushushu bomhlaba wendawo ephakamileyo yee-5,621 amamitha kubonisa amadireyi angamashumi amabini anesibini ngaphezu kwe-zero, ngelixa ukushisa komoya kungaphantsi kwama-20 nangaphantsi. Kukho neendawo ezikhulayo ezikhulayo. Konke oku kubonisa ngokuthe ngqo ukuba umsebenzi we-volcano akayekanga. Ezinye izazinzulu zize ziqikelele ukuqhuma kwayo kwiminyaka embalwa eminyaka.

I-Volcano ebalazweni

I-volbrano Elbrus kwimaphu iboniswa njengendawo enkulu emhlophe. Iilwimi zeqhwa zihamba ngeendlela ezahlukeneyo ukuya kwiindawo eziphantsi.

Kufuneka kukhunjulwe ukuba i-Elbrus intaba-mlilo (esebenzayo okanye iphela, isaphinde ifunyaniswe lulwazi) isisigxina esingenza izinto ezinobungozi emhlabeni. Ukuba uyavuka, iziqhumane ezinkulu kunye neziqhwala zeqhwa ziyancibilika kwaye zihla ezantsi kwintlambo yesempuma njengendlela yomlambo, obulalayo. Umendo walo uya kuthunyelwa iikhilomitha ezingamashumi amahlanu, ukuba kungaphezulu, ukuya eTyrnyauz. Abemi balapha bahlala malunga namawaka angamawaka amabini.

Kuza kube namhlanje, u-Elbrus - umthala-mlilo ophelile, ngokuchanekileyo-ukulala. Kodwa kwakhona imikhosi ekhulile ebudeni bayo iyakhula.