Xa sibona ezinye zeentaba ezinkulu nezona ziphakamileyo kwiplanethi yethu, ezinje nge Iintaba zeAppalachian kunye Uluhlu lweentaba zehealayan, Sicinga ukuba akukho nto ingaphaya kwayo. Kwaye kukuba asinakuba siphosakele ngakumbi kuloo nto. Nangona uMhlaba kuphela komhlaba onokuhlala kuwo ISistema Solar, ayisiyiyo kuphela ene-morphologies enomdla kunye nolwakhiwo lwejoloji. Namhlanje sifudukela kwiplanethi Marte, apho sinentaba-mlilo enkulu kunazo zonke ezaziwayo kwiSolar System. Imalunga nayo INtaba iOlimpus.
Ungaphoswa zizo zonke iinkcukacha malunga nale volcano inkulu, imvelaphi yayo kunye nendlela eyafunyanwa ngayo.
Iimpawu eziphambili
Isijikelezi-langa uMars sinomdla omkhulu ebantwini okoko safunyanwa. Kukho izifundo kunye nohambo olunezinto ezininzi ezenziweyo olwenziwe ukuze kufunyanwe kungekuphela indawo kodwa ingaphakathi lomhlaba. Ngoku, I-InSight probe ize eMars ukuze ibone konke okungaphakathi kuyo. Imifanekiso engcono kunye nolwazi oluthe kratya lunokuqokelelwa ngalo lonke ixesha kunikwa inkqubela phambili yetekhnoloji esele siyifumene kumashumi eminyaka akutshanje.
INtaba iOlimpus yayisele isaziwa kukhenketho lwakudala, kuba isiphekepheke sasondela kwiplanethi kwaye inokubonwa. Nangona kunjalo, iinkcukacha zobu bungangamsha bezingaziwa kakuhle. Yeyona volcano incinci kwiplanethi ebomvu Kwaye yenziwe malunga ne-1.800 yezigidi zeminyaka eyadlulayo.
Ine-massif esembindini ukuphakama okuphakama ukuya phantse kwi-23 km ukuphakama. Siyakhumbula ukuba incopho enkulu eMhlabeni ayidluli kwi-9 km. Around it has a ithafa enkulu erhangqileyo. Kuqatshelwe ukuba ibekwe kuxinzelelo lobunzulu be-2 km kwaye zininzi kakhulu iingxondorha ezinkulu eziphantse zayi-6 km ukuphakama. Khawufane ucinge ubungakanani bale volcano, xa kuthelekiswa nale nto sinayo eMhlabeni. Iliwa elinye liphezulu kunayo nayiphi na incopho kuyo yonke iIberia.
Phakathi kweempawu zangaphakathi kwintaba-mlilo, sibona ukuba i-caldera yayo inayo Ubukhulu be-85 km ubude, i-60 km ububanzi kwaye phantse i-3 km ubunzulu. Ngokwenene lisilo lerhamncwa elifanele ukubonwa, nkqu nakwiifoto. Ineetshimini ezi-6 ezenziwe ngamaxesha ahlukeneyo onyaka. Isiseko sentaba-mlilo simalunga neekhilomitha ezingama-600 ubukhulu.
Ubukhulu kunye nokumila
INtaba iOlimpus ukuba yayiseSpain
Ukuba sibona isiseko esipheleleyo, siyayibona loo nto Inendawo engama-283.000 eekhilomitha eziqhelekileyo. Oku kuyafana nesiqingatha sesiqithi seIberia. Kunzima ukuba le milinganiselo inokuqikelelwa, kuba inkulu kakhulu. Intaba-mlilo ehlala isiqingatha seSpain ayisiyonto ilula ukuyicinga. Ngapha koko, ubukhulu bayo bunjalo kangangokuba ukuba besinokulandela umhlaba kaMars, besingayi kuyibona ngokupheleleyo imilo yale volcano. Nokuba besinokuhamba, besiya kubona udonga olukhangeleka ngathi liwa elikhulu.
Ingabonakala kuphela ngaphezulu ngaphezulu, kuba ukunqamka kweplanethi kuya kuthintela ukujonga kwethu phezulu. Njengo Ayinakubonwa ngokupheleleyo ukusuka emhlabeni, nokuba kungaphezulu. Ukuba besinokuhlala kwincopho yentaba-mlilo, besinokubona nje inxalenye yethambeka layo. Asizukubona isiphelo, kuba besiza kudibana. Ukuba sifuna ukubona iNtaba iOlimpus ngokupheleleyo, ekuphela kwendlela kukusuka emajukujukwini enqanaweni.
Ukuhlalutya uhlobo lwe-volcano eyiNtaba iOlimpus, sinokuthi luhlobo lwekhaka. Iintaba-mlilo ezikhuselekileyo zibonakaliswe ngokuba zibanzi kwaye zide kwaye zineemilo ezijikeleziweyo nezicaba Zifana neentaba-mlilo zaseHawaii.
Ubungakanani obukhulu obunje bunenkcazo kunye nemvelaphi. Kwaye ukuba amandla okusebenza kweplanethi awasebenzi ngendlela efanayo neyethu. Awunayo iiplate zeetectonic Ezishukumayo kwaye zihambisa isikwere selizwekazi. Ngesi sizathu, iNtaba iOlimpus ibisoloko ivelisa udaka lwendawo enye kwaye ibiqina, ifumana ubungakanani.
Imvelaphi yeNtaba iOlimpus
Njengoko sisazi, le volcano inkulu ibingumbandela wophando ukufumanisa imvelaphi yayo. Ukuqhuma kwe-volcano kucingelwa ukuba kwakha i-crater namhlanje. Kuba iMars ayinazo iipleyiti zetectonic, umphezulu uzinzile. Ngale ndlela, lava egxothiweyo yomelele ukwenza olu ncedo.
Le volcano iguqule ubuso bonke beMars. Inkunkuma evela kwintaba-mlilo yiyo eyenze ithafa elikhulu elilele emazantsi omqolo, obizwa ngokuba yithafa elikhulu laseTarsis. Yindawo eyi-5.000 isikwere seekhilomitha kunye ne-12 yeekhilomitha ubunzulu, sithathela ingqalelo ukuba iplanethi ebomvu inesiqingatha esikhulu njengale yethu. Olu tshintsho kwindlela uMars ajongeka ngayo ngokupheleleyo.
Uxinzelelo lwezinto ezenziwa leli qonga likhulu lisuse ubume beplanethi kwaye zihambisa zonke iindawo zoqweqwe lomntla. Izazinzulu zikholelwa ukuba ngenxa yokubonakala kwale volcano kunye nokuma kwayo okucothayo, iipali zeMars azisekho ezibondeni, kwaye zonke iindlela zemilambo zitshintshile kangangokuba ziye zafa.
Ukuba kwenzeka into enjalo kwiplanethi yethu, idolophu yaseParis ibiyinxalenye yesangqa sePolar, kuba iNtaba iOlimpus ibiya kuwususa wonke umhlaba.
Into ibonwa ngoososayensi kukuba le volcano inkulu, inokuphinda iqhume kwakhona njengoko uphando oluthile luphela. Kuyamangalisa ukuba kwezinye iiplanethi, ayikho enye into ngaphandle kokuba nolunye uhlobo lwe-dynamics kunokubangela ukuba olu hlobo luvele. Inyaniso yokuba uMars unezinye izinto eziguqukayo zangaphakathi kwaye ayinayo le mibhobho yokuhambisa izinto ihambisa iiplate ze-tectonic, into enye enjenge-volcano, inokubangela ukuba kubekho izakhiwo ezinkulu ezenza eyona ntaba inkulu kwiSolar System.