Iintaba zaseScandinavia - intlanethi yeentaba zeentaba kunye nemilambo enzulu

Inkqubo yeentaba kwi- peninsula yaseScandinavia yaseMntla Yurophu, ephethe ububanzi bee-1,700 km kunye nobubanzi beekhilomitha ezili-1,300, ibizwa ngokuba yiiNtaba zeScandinavia. Inxalenye yasentshonalanga yeentaba zeentaba iya kuLwandle oluMntla, lenze iibhanki ezincinci kunye neziqithi, ii-peninsula, i-capes, iziqithi. Ubunzima nokungakwazi ukufikelela kwiintaba kuboniswa ngama-178 amathoni asekwe kwicandelo le-Oslo-Bergen (Norway). Icandelo lesempuma liyehliswa kancane kwaye lidlulele kwisiqithi saseNorland. Iintaba zaseScandinavia ziyintlambo, equlethwe ngamagqabi ahlukeneyo, amathafa kunye neentlambo zasemaphandleni. Kwiindawo ezininzi, iindawo ezihambelanayo zidibaniswe ziintlanzi kunye neendlambo ezinzulu. Ukhuselo lwangoku lwalwenziwa ngenxa yokukhukhula kwamanzi, iqhwa, umoya kunye nekhephu.

Intaba ye-mountain massif yee-fjords ezininzi, ezakhiwa phantsi kwezenzo ze-glaciers. Ezi ziindawo zokuloba zaselwandle ezinqumla kakhulu umhlaba, kunye namanxweme amakhulu. Njengomthetho, ubunzulu beScandinavian fjords bafikelela kwikhilomitha enye.

Kukholelwa ukuba iintaba zaseScandinavia ziphantsi. Intaba ephezulu yeGalakhepiggen enokuphakama kwe-2469 m - ifumaneka kwintlambo yezantsi yentaba, kwintsimi yaseNorway. Ingongoma ephezulu yeSweden - iNtaba iKebnekaise (2111 m) - isecaleni elisenyakatho ye-peninsula. Inkqubo yeStaba yaseScandinavia ihlanganiswe ngamaqhwa, okubhekwa njengowona mkhulu kunxalenye yeYurophu. Imozulu yila ma candelo iyingqinelana, kuphela kwindawo yecala elingasenyakatho.

Kwintsimi yaseSweden, kwiintaba zaseScandinavia (eLapland), kukho i-National Reserve "iSarek" enkulu. Yasekwa ngo-1909 kwaye ihlanganisa indawo yeehektha ezingama-194,000. Kule ndawo kunamapopu angaphezu kwe-90 ukuphakama ukusuka kwii-1800 zamitha. Phakathi kwabo imilambo yeentaba, imifudlana, iigorge kunye ne-glaciers eziyi-100.

Iintaba zaseScandinavia zigcwele inethiwekhi yomlambo onomdaka, owenziwe yi-predominance yemozulu yolwandle olumanzi kunye nokuqothulwa okukhulu kwe-mountain massif. Imifula, njengomthetho, imfutshane kwaye inzulu, igcwele imvula yamanzi kunye neempuphu ezininzi. Ukuzaliswa kwazo ngokubanzi kuqala entwasahlobo, ngokukodwa ngokusuka kweenkwenkwezi kunye neemvula ezinzima, kaninzi kunamaqabunga. Ngenxa yesantya esiphezulu samanje, icebo ayifaki kwimifula ebusika. Ezi ntaba eYurophu zinenani elikhulu lamachibi e-tectonic-glacial.

Lapho ukuphakama kweentaba kufinyelela kumitha engama-1000 kummandla wasezantsi kwaye kufike kumitha engama-500 kumntla, iintlambo zihlanganiswe namahlathi e-coniferous taiga. Ubunzima behlathi beentlambo ezisentshonalanga zihamba kunye nezihluma zasemahlathini kunye neebhogi. Kule ndawo, ipayini kunye ne-spruce ibaluleke kakhulu. Ngaphandle kwalezi ziphakamileyo, ibhanti leemithi ze-birch lifikelela kwindawo ephakamileyo yemitha engama-200, eyatshintshwa indawo yintaba. Abemi basekhaya basebenzisa le ndawo ehlotyeni ukuba badle imfuyo.

Engxenyeni esempuma yeentaba, i-widleaf kunye namahlathi axutywe kakhulu . Izilwanyana zeentaba zaseScandinavia zimelelwe iinqweba, izimpungushe, i-moose, i- reindeer, i- squirrels, i-roe deer, iimpawu. Phakathi kweentaka ezisemaphandleni kukho i-hazel grouse, i-black grouse, i-wood grouse, ngaselunxwemeni lolwandle kunye namachibi apho kukho iintaka zamanzi. Emanzini nasemanzini, kukho iintlanzi ezininzi zentengiso.

Iintaba zaseScandinavia zizityebi kwiipasiti zepirrites, ubhedu, isinyithi, i-lead kunye ne-titanium. KuLwandle oluMntla, kwi-shelf ingxenye, kukho iindawo zokugcina ioli.