{"id":1285,"date":"2024-08-07T20:19:36","date_gmt":"2024-08-07T20:19:36","guid":{"rendered":"https:\/\/travelshelper.com\/staging\/?p=1285"},"modified":"2026-02-27T01:01:24","modified_gmt":"2026-02-27T01:01:24","slug":"vatnajokull-avrupanin-en-buyuk-buzulu","status":"publish","type":"post","link":"https:\/\/travelshelper.com\/tr\/magazine\/unusual-places\/vatnajokull-the-largest-glacier-in-europe\/","title":{"rendered":"VATNAJOKULL \u2013 Avrupa&#039;n\u0131n En B\u00fcy\u00fck Buzulu"},"content":{"rendered":"<p class=\"translation-block\">Vatnaj\u00f6kull, \u0130zlanda'n\u0131n (ve bir\u00e7ok say\u0131mla Avrupa'n\u0131n) en b\u00fcy\u00fck buzuludur. Bu geni\u015f buz \u00f6rt\u00fcs\u00fc yakla\u015f\u0131k 8.100 km\u00b2 \u2014 \u00fclkenin yakla\u015f\u0131k %8'i \u2014 alan\u0131 kaplar ve yakla\u015f\u0131k 3.000 km\u00b3 buz i\u00e7erir. Ortalama kal\u0131nl\u0131\u011f\u0131 400\u2013500 m olup baz\u0131 yerlerde ~1.000 m'ye ula\u015f\u0131r. Erimi\u015f suyu depolamas\u0131 nedeniyle yerel olarak <em>Vatna Glacier<\/em> (\u0130zlandaca <em>vatn<\/em> \u201csu\u201d) olarak adland\u0131r\u0131l\u0131r; Vatnaj\u00f6kull ad\u0131 kelimenin tam anlam\u0131yla \u201csular\u0131n buzu\u201d demektir. \u00d6l\u00e7e\u011fi \u015fa\u015f\u0131rt\u0131c\u0131d\u0131r: ony\u0131llar boyunca pek \u00e7ok da\u011f zirvesi ve sekiz subglasyal volkan buzun alt\u0131nda gizlidir. 2008'den beri bu buzul (ve \u00e7evresindeki peyzaj) Vatnaj\u00f6kull Milli Park\u0131'n\u0131 olu\u015fturmakta, ve 2019'da UNESCO onu \u201cVatnaj\u00f6kull \u2013 Dynamic Nature of Fire and Ice\u201d D\u00fcnya Miras\u0131 Listesi'ne kaydetti.<\/p>\n\n\n\n<p><strong>K\u0131sa Bilgiler:<\/strong><\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><em>Alan:<\/em> ~8.100 km\u00b2 (\u0130zlanda'n\u0131n yakla\u015f\u0131k %8'i)<\/li>\n\n\n\n<li><em>Hacim:<\/em> \u22483.000 km\u00b3 (Danimarka'n\u0131nkinin d\u00f6rt kat\u0131)<\/li>\n\n\n\n<li><em>Kal\u0131nl\u0131k:<\/em> Ortalama ~450 m (maksimum ~1.000 m)<\/li>\n\n\n\n<li><em>En y\u00fcksek rak\u0131m:<\/em> 2.110 m (Hvannadalshnj\u00fakur zirvesi)<\/li>\n\n\n\n<li><em>Volkanlar:<\/em> 8 b\u00fcy\u00fck buzul alt\u0131 sistemi (Gr\u00edmsv\u00f6tn, B\u00e1r\u00f0arbunga, \u00d6r\u00e6faj\u00f6kull, vb.)<\/li>\n\n\n\n<li><em>Milli Park:<\/em> 2008 y\u0131l\u0131nda kurulmu\u015ftur (yakla\u015f\u0131k 14.967 km\u00b2'lik bir alan\u0131 kapsar)<\/li>\n\n\n\n<li><em>UNESCO:<\/em> D\u00fcnya Miras\u0131 Alan\u0131 (Temmuz 2019'da tescil edildi)<\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Vatnaj\u00f6kull Nedir? Temel Bilgiler ve Rakamlar<\/h2>\n\n\n\n<p>Vatnaj\u00f6kull (telaffuzu \u201cVAT-nah-YEUH-kootl\u201d), \u0130zlanda'n\u0131n g\u00fcneydo\u011fusundaki devasa buz \u00f6rt\u00fcs\u00fcd\u00fcr. Yakla\u015f\u0131k 8.000\u20138.300 km\u00b2'lik bir alan\u0131 kaplayarak \u0130zlanda'n\u0131n en b\u00fcy\u00fck buzulu ve genellikle kutup Arktik b\u00f6lgesi d\u0131\u015f\u0131nda Avrupa'n\u0131n en b\u00fcy\u00fck buzulu olarak an\u0131l\u0131r. Buz, jeolojik a\u00e7\u0131dan nispeten \u201cgen\u00e7tir\u201d (birka\u00e7 bin ya\u015f\u0131nda). Buzulun b\u00fcy\u00fck bir k\u0131sm\u0131 yaz aylar\u0131nda da varl\u0131\u011f\u0131n\u0131 s\u00fcrd\u00fcr\u00fcr: y\u00fczeyinin yakla\u015f\u0131k '\u0131 denge \u00e7izgisinin (yaz kar \u00e7izgisi) \u00fczerinde bulunur, bu nedenle her yaz sadece en y\u00fcksek kenarlar\u0131 tamamen erir. Vatnaj\u00f6kull'\u00fcn alt\u0131nda y\u00fczlerce nunatak (a\u00e7\u0131kta kalan zirveler) ve sekiz merkezi volkan y\u00fckselir. Buz \u00f6rt\u00fcs\u00fc, bir platodan (600\u2013800 m y\u00fckseklik) her y\u00f6ne do\u011fru akarak d\u00fczinelerce \u00e7\u0131k\u0131\u015f buzulunu ve buzul nehrini besler.<\/p>\n\n\n\n<p>Kafa kar\u0131\u015f\u0131kl\u0131\u011f\u0131na yol a\u00e7an \u00f6nemli bir nokta: Vatnaj\u00f6kull <em>Bazen<\/em> \"Avrupa'n\u0131n en b\u00fcy\u00fck buzulu\" olarak adland\u0131r\u0131l\u0131r, ancak bu genellikle Arktik Rusya'y\u0131 d\u0131\u015far\u0131da b\u0131rak\u0131r. (Rusya'n\u0131n Novaya Zemlya buzulu, teknik olarak daha b\u00fcy\u00fck olan ancak y\u00fcksek Arktik'te bulunan 20.500 km\u00b2'lik Severny Adas\u0131 buz \u00f6rt\u00fcs\u00fcne sahiptir.) Vatnaj\u00f6kull, Avrupa anakaras\u0131ndaki en b\u00fcy\u00fck buzul olmaya devam etmektedir.<\/p>\n\n\n\n<figure class=\"wp-block-pullquote\"><blockquote><p>Vatnaj\u00f6kull ad\u0131 Eski \u0130skandinav dilinden gelir: vatna-, vatn (su veya g\u00f6l) kelimesinin genitif \u00e7o\u011fuludur ve j\u00f6kull buzul anlam\u0131na gelir. Buzul, say\u0131s\u0131z buzul alt\u0131 g\u00f6l\u00fc ve erime suyu kanal\u0131 i\u00e7erir; bu nedenle \"sular\u0131n buzulu\" lakab\u0131 olduk\u00e7a yerindedir.<\/p><cite>Tarihsel Not<\/cite><\/blockquote><\/figure>\n\n\n\n<h3 class=\"wp-block-heading\">Boyut ve \u00d6l\u00e7\u00fcler<\/h3>\n\n\n\n<figure class=\"wp-block-table\"><table class=\"has-fixed-layout\"><thead><tr><th>\u0130statistik<\/th><th>De\u011fer<\/th><\/tr><\/thead><tbody><tr><td><strong>Alan<\/strong><\/td><td>~8.100 km\u00b2 (\u0130zlanda'n\u0131n yakla\u015f\u0131k %8'i)<\/td><\/tr><tr><td><strong>Hacim<\/strong><\/td><td>~3.000 km\u00b3<\/td><\/tr><tr><td><strong>Ortalama Kal\u0131nl\u0131k<\/strong><\/td><td>~450 m<\/td><\/tr><tr><td><strong>Maksimum Kal\u0131nl\u0131k<\/strong><\/td><td>~950\u20131.000 m<\/td><\/tr><tr><td><strong>Kapsam<\/strong><\/td><td>~100 km (D-B) \u00d7 100 km (K-G)<\/td><\/tr><tr><td><strong>Zirve Rak\u0131m\u0131<\/strong><\/td><td>2.110 m (Hvannadalshnjukur)<\/td><\/tr><tr><td><strong>\u0130zlanda'n\u0131n alan\u0131n\u0131n %'si<\/strong><\/td><td>~8%<\/td><\/tr><tr><td><strong>\u00c7\u0131k\u0131\u015f Buzullar\u0131<\/strong><\/td><td>~30 b\u00fcy\u00fck buzul dili<\/td><\/tr><tr><td><strong>Ulusal Park<\/strong><\/td><td>Vatnaj\u00f6kull Milli Park\u0131 (tahmini 2008)<\/td><\/tr><tr><td><strong>UNESCO Stat\u00fcs\u00fc<\/strong><\/td><td>D\u00fcnya Miras\u0131 Alan\u0131 \u2014 <em>Ate\u015f ve Buz<\/em> (Temmuz 2019)<\/td><\/tr><\/tbody><\/table><\/figure>\n\n\n\n<h3 class=\"wp-block-heading\">\u201cAvrupa'n\u0131n En B\u00fcy\u00fck Buzulu\u201d<\/h3>\n\n\n\n<p>Vatnaj\u00f6kull, alan ve hacim bak\u0131m\u0131ndan \u0130zlanda'n\u0131n en b\u00fcy\u00fck buzuludur. Bir\u00e7ok tan\u0131ma g\u00f6re de Avrupa'n\u0131n en b\u00fcy\u00fck buzuludur. UNESCO, Vatnaj\u00f6kull'\u00fcn \"Avrupa'n\u0131n en b\u00fcy\u00fck buzulu\" oldu\u011funu belirtmektedir. Alan olarak (8.000+ km\u00b2) Avrupa anakaras\u0131ndaki herhangi bir buzuldan \u00e7ok daha b\u00fcy\u00fckt\u00fcr \u2013 kar\u015f\u0131la\u015ft\u0131rma i\u00e7in, \u0130svi\u00e7re'nin Aletsch Buzulu sadece ~79 km\u00b2'lik bir alan\u0131 kaplar. Sadece Arktik Rus buzullar\u0131 dahil edilirse baz\u0131 tart\u0131\u015fmalar ortaya \u00e7\u0131kar: Novaya Zemlya'n\u0131n Severny Adas\u0131 buzul \u00f6rt\u00fcs\u00fc (~20.500 km\u00b2) teknik olarak daha b\u00fcy\u00fckt\u00fcr, ancak \u0130zlanda'n\u0131n olduk\u00e7a kuzeyinde yer al\u0131r. Arktik hari\u00e7 tutuldu\u011funda, Vatnaj\u00f6kull Avrupa'n\u0131n en b\u00fcy\u00fck buzul \u00f6rt\u00fcs\u00fc unvan\u0131n\u0131 elinde tutmaktad\u0131r.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Vatnaj\u00f6kull Nerede?<\/h2>\n\n\n\n<p>Vatnaj\u00f6kull, \u0130zlanda'n\u0131n g\u00fcneydo\u011fusuna hakimdir. Yakla\u015f\u0131k 64.0\u201365.5\u00b0 Kuzey enlemi ve 16.0\u201318.5\u00b0 Bat\u0131 boylam\u0131n\u0131 kapsayan bu b\u00f6lge, orta yaylalardan k\u0131y\u0131ya yak\u0131n b\u00f6lgelere kadar uzan\u0131r. G\u00fcneyde k\u0131y\u0131 ovalar\u0131na ve \u00c7evre Yolu'na (1. G\u00fczergah) biti\u015fiktir; do\u011fuda H\u00f6fn kasabas\u0131na ve Okyanus'a do\u011fru uzan\u0131r; bat\u0131da Skaftafell'e yakla\u015f\u0131r; ve kuzeyde \u0131ss\u0131z yayla platosuna (Sprengizandur) do\u011fru incelir. Buzulun eriyen sular\u0131, birka\u00e7 b\u00fcy\u00fck nehri (\u00f6rne\u011fin Skei\u00f0ar\u00e1, J\u00f6kuls\u00e1) besleyerek geni\u015f siyah kumlu ovalar ve lag\u00fcnler olu\u015fturur (a\u015fa\u011f\u0131ya bak\u0131n\u0131z). Ziyaret\u00e7iler genellikle Vatnaj\u00f6kull'a \u00c7evre Yolu \u00fczerinden ula\u015f\u0131rlar: Reykjav\u00edk'ten Skaftafell\/Vatnaj\u00f6kull b\u00f6lgesine yakla\u015f\u0131k 320 km (~4-5 saat) s\u00fcren yolculuk, g\u00fcney k\u0131y\u0131s\u0131ndaki manzaral\u0131 kasabalar ve \u015felalelerden ge\u00e7er. Milli park, t\u00fcm buz \u00f6rt\u00fcs\u00fcn\u00fc ve \u00e7evresindeki b\u00f6lgeleri kaps\u0131yor; haritada \u0130zlanda'n\u0131n g\u00fcney-orta kesimini kapsayan devasa beyaz\/ye\u015fil bir alan olarak g\u00f6r\u00fcn\u00fcyor.<\/p>\n\n\n\n<p><strong>Harita ve Eri\u015fim:<\/strong> Vatnaj\u00f6kull, g\u00fcney ucunda \u00c7evre Yolu taraf\u0131ndan fiilen ikiye b\u00f6l\u00fcnm\u00fc\u015ft\u00fcr. Ba\u015fl\u0131ca eri\u015fim noktalar\u0131 Skaftafell ziyaret\u00e7i merkezi (bat\u0131 taraf\u0131), J\u00f6kuls\u00e1rl\u00f3n lag\u00fcn\u00fc \/ Brei\u00f0amerkurj\u00f6kull (do\u011fu taraf\u0131) ve 4x4 ara\u00e7lar i\u00e7in merkezi platoya giden F yollar\u0131d\u0131r (kuzey taraf\u0131). Asfalt yollar\u0131n \u00e7o\u011fu buz kenar\u0131nda sona erer; i\u00e7 kesimlere seyahat \u00f6zel turlar gerektirir. Buzulun kendisinde kasaba yoktur \u2013 en yak\u0131n k\u00f6yler H\u00f6fn (do\u011fu) ve Kirkjub\u00e6jarklaustur'dur (bat\u0131).<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Vatnaj\u00f6kull'\u00fcn Jeolojisi ve Olu\u015fumu<\/h2>\n\n\n\n<p>Vatnaj\u00f6kull, Holosen d\u00f6nemindeki aktif buzulla\u015fma sonucu olu\u015fmu\u015ftur. Bir\u00e7ok Alp buzulunun aksine, <strong>Olumsuz<\/strong> Son Buz \u00c7a\u011f\u0131'n\u0131n bir kal\u0131nt\u0131s\u0131: Son ara\u015ft\u0131rmalar, kal\u0131n buz tabakas\u0131n\u0131n sadece yakla\u015f\u0131k 2500 y\u0131l \u00f6nce olu\u015ftu\u011funu g\u00f6steriyor. Buz, k\u0131y\u0131ya do\u011fru hafif\u00e7e e\u011fimli bir y\u00fcksek platoda (ortalama 600-800 m y\u00fckseklik) yer al\u0131yor. Buz \u00f6rt\u00fcs\u00fcn\u00fcn kenarlar\u0131nda arazi deniz seviyesine yak\u0131n bir seviyeye inerken, merkezde buzul alt\u0131 ana kaya \u00fczerinde buz alanlar\u0131 bulunuyor. \u0130zlanda, y\u00fcksek ya\u011f\u0131\u015f ve jeotermal \u0131s\u0131ya sahip Orta Atlantik S\u0131rt\u0131 \u00fczerinde yer ald\u0131\u011f\u0131ndan, Vatnaj\u00f6kull \u00e7ok dinamik bir yap\u0131ya sahip.<\/p>\n\n\n\n<p>Buzulun i\u00e7 yap\u0131s\u0131, s\u0131k\u0131\u015fm\u0131\u015f kar (firn) katmanlar\u0131n\u0131n buza d\u00f6n\u00fc\u015fmesi ve baz\u0131 kabarc\u0131kl\u0131 buzul buzlar\u0131n\u0131n olu\u015fmas\u0131yla karakterize edilir. Y\u00fczeyin yakla\u015f\u0131k '\u0131 y\u0131l boyunca karla kapl\u0131 kal\u0131r (yaz kar \u00e7izgisi veya denge \u00e7izgisi, yakla\u015f\u0131k 1100-1300 m'nin \u00fczerinde). Buzun muazzam a\u011f\u0131rl\u0131\u011f\u0131 ayn\u0131 zamanda kabu\u011fu da a\u015fa\u011f\u0131 do\u011fru bast\u0131r\u0131r: jeodezik \u00e7al\u0131\u015fmalar, Vatnaj\u00f6kull eriyerek inceldik\u00e7e \u0130zlanda y\u00fczeyinin kademeli olarak eski haline d\u00f6nd\u00fc\u011f\u00fcn\u00fc g\u00f6stermektedir. Buzun alt\u0131nda, ge\u00e7mi\u015fteki j\u00f6kulhlauplarda (sellerde) oyulmu\u015f derin vadiler ve buzul alt\u0131 kanyonlar bulunur. \u00d6zetle, Vatnaj\u00f6kull, yo\u011fun kar ya\u011f\u0131\u015f\u0131ndan (g\u00fcney \u0130zlanda y\u00fcksek rak\u0131mlarda 5-10 m'ye kadar ya\u011f\u0131\u015f al\u0131r) ve yaz erimesi yoluyla kenarlarda a\u015f\u0131nmadan kaynaklanan birikimle karakterize edilen \"so\u011fuk\" bir buz \u00f6rt\u00fcs\u00fcd\u00fcr.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Buzun Alt\u0131ndaki Volkanlar: Vatnaj\u00f6kull'un Ate\u015fli Kalbi<\/h2>\n\n\n\n<p>Vatnaj\u00f6kull, b\u00fct\u00fcn bir volkanik tak\u0131maday\u0131 gizliyor. \u0130zlandal\u0131 volkanologlar bunu tespit ediyor. <strong>yedi b\u00fcy\u00fck volkanik sistem<\/strong> Buzun alt\u0131nda. \u0130ki \u00f6ne \u00e7\u0131kan merkez oyuncusu \u015funlard\u0131r: <strong>Grimsvotn<\/strong> Ve <strong>B\u00e1r\u00f0arbunga<\/strong>\u0130zlanda'n\u0131n en aktif yanarda\u011f\u0131 olan Gr\u00edmsv\u00f6tn (1.764 m, buz \u00f6rt\u00fcs\u00fcn\u00fcn merkezinde), yakla\u015f\u0131k her 5-10 y\u0131lda bir patlar. 2011'deki patlamas\u0131 yakla\u015f\u0131k 20 km y\u00fcksekli\u011fe k\u00fcl bulutlar\u0131 g\u00f6ndermi\u015ftir. B\u00e1r\u00f0arbunga (2.010 m), 70\u00d710 km'lik kalderas\u0131yla buz \u00f6rt\u00fcs\u00fcn\u00fcn en b\u00fcy\u00fck yanarda\u011f\u0131d\u0131r. 2014-2015 y\u0131llar\u0131nda devasa Holuhraun yar\u0131k patlamas\u0131n\u0131 beslemi\u015ftir: yakla\u015f\u0131k 0,85 km\u00b3 bazalt lav\u0131 d\u0131\u015far\u0131 akarak yakla\u015f\u0131k 85 km\u00b2'lik bir lav alan\u0131 olu\u015fturmu\u015ftur (\u0130zlanda'n\u0131n son d\u00f6nemdeki en b\u00fcy\u00fck patlamalar\u0131ndan biri).<\/p>\n\n\n\n<p><strong>Gr\u00edmsv\u00f6tn (\u0130zlanda'n\u0131n En Aktifi):<\/strong> Vatnaj\u00f6kull yanarda\u011f\u0131n\u0131n merkezinin alt\u0131nda Gr\u00edmsv\u00f6tn adl\u0131 buzul alt\u0131 g\u00f6l\u00fc yer almaktad\u0131r. 2011'deki patlamas\u0131 k\u0131sa ama \u015fiddetliydi ve s\u0131k s\u0131k su bask\u0131nlar\u0131na neden olur: her patlama genellikle b\u00fcy\u00fck buz k\u00fctlelerini eritir. Gr\u00edmsv\u00f6tn'\u00fcn \u00fczerindeki buzul, patlamalardan \u00f6nce \u015fi\u015fmi\u015fti ve alttan gelen buzul ta\u015fk\u0131nlar\u0131 (j\u00f6kulhlaup) tekrar tekrar meydana gelmi\u015ftir. \u00d6rne\u011fin, 2004'teki bir patlama (Gr\u00edmsv\u00f6tn), kaydedilen en b\u00fcy\u00fck buzul ta\u015fk\u0131nlar\u0131ndan birine yol a\u00e7m\u0131\u015ft\u0131r.<\/p>\n\n\n\n<p><strong>B\u00e1r\u00f0arbunga:<\/strong> Karma\u015f\u0131k bir kaldera ile \u00f6rt\u00fcl\u00fc bu devasa volkan, en son 2014-2015 \u00e7atlak olay\u0131nda tepesini patlatt\u0131. Patlama A\u011fustos 2014'te ba\u015flad\u0131 ve yakla\u015f\u0131k 6 ay s\u00fcrd\u00fc. Bu s\u00fcre zarf\u0131nda, yakla\u015f\u0131k 1,6 km\u00b3 lav p\u00fcsk\u00fcrd\u00fc (\u224884 km\u00b2 alan) \u2013 bu, Vatnaj\u00f6kull'\u00fcn d\u00fczinelerce \u00e7\u0131k\u0131\u015f buzulunun toplam hacmine e\u015fde\u011ferdir. Yukar\u0131daki buzul yava\u015f\u00e7a geri \u00e7ekildi (baz\u0131 k\u0131s\u0131mlarda ~65 m). B\u00e1r\u00f0arbunga'da huzursuzluk (deprem k\u00fcmeleri, deformasyon) g\u00f6r\u00fcld\u00fc\u011f\u00fcnden, jeologlar onu yak\u0131ndan izliyor.<\/p>\n\n\n\n<p><strong>\u00d6r\u00e6faj\u00f6kull (En Y\u00fcksek Volkan):<\/strong> Buzulun g\u00fcneydo\u011fusunda, \u00d6r\u00e6faj\u00f6kull, buzla kapl\u0131 iki zirvesi olan bir stratovolkanik da\u011fd\u0131r. \u0130zlanda'n\u0131n en y\u00fcksek zirvesi olan Hvannadalshnj\u00fakur'a (2.110 m) ev sahipli\u011fi yapmaktad\u0131r. \u00d6r\u00e6faj\u00f6kull'\u00fcn tarihsel patlamalar\u0131 y\u0131k\u0131c\u0131 olmu\u015ftur: 1362'de yakla\u015f\u0131k 10 km\u00b3 riyolit tefra (VEI ~6) \u00fcretmi\u015ftir; bu, \u0130zlanda'n\u0131n bilinen en b\u00fcy\u00fck patlamas\u0131d\u0131r. 1727-28'deki bir di\u011fer b\u00fcy\u00fck patlama da, manzaray\u0131 \u00f6nemli \u00f6l\u00e7\u00fcde de\u011fi\u015ftiren buzul sel bask\u0131nlar\u0131na neden olmu\u015ftur. Bug\u00fcn \u00d6r\u00e6faj\u00f6kull b\u00fcy\u00fck \u00f6l\u00e7\u00fcde sakindir, ancak buzun alt\u0131nda geni\u015f erime suyu g\u00f6lleri i\u00e7ermektedir.<\/p>\n\n\n\n<p>Di\u011fer buzul alt\u0131 volkanlar\u0131 \u015funlard\u0131r: <strong>Kverkfj\u00f6ll<\/strong> (B\u00e1r\u00f0arbunga'n\u0131n kuzeydo\u011fusunda), <strong>\u00c7eki\u00e7<\/strong> (eskiden B\u00e1r\u00f0arbunga sisteminin bir par\u00e7as\u0131yd\u0131) ve <strong>Torfaj\u00f6kull<\/strong> (Vatnaj\u00f6kull'\u00fcn g\u00fcneybat\u0131s\u0131ndaki b\u00fcy\u00fck bir kaldera) sistemi. Buz \u00f6rt\u00fcs\u00fcn\u00fcn i\u00e7 k\u0131sm\u0131nda bir\u00e7ok k\u00fc\u00e7\u00fck \u00e7atlak ve s\u0131cak su kayna\u011f\u0131 (\u00f6rne\u011fin Kverkfj\u00f6ll'de) bulunmaktad\u0131r.<\/p>\n\n\n\n<figure class=\"wp-block-pullquote\"><blockquote><p>Burada buzul alt\u0131 patlamalar\u0131 ve buzul ta\u015fk\u0131nlar\u0131 (j\u00f6kulhlaup) karakteristik \u00f6zelliklerdir. 1996 Kas\u0131m ay\u0131ndaki me\u015fhur olayda, Gr\u00edmsv\u00f6tn'\u00fcn patlamas\u0131 Vatnaj\u00f6kull'\u00fcn alt\u0131ndaki yakla\u015f\u0131k 3 km\u00b3 buzu eritti. 5-6 Kas\u0131m 1996'da buz baraj\u0131 y\u0131k\u0131ld\u0131: yakla\u015f\u0131k 50.000 m\u00b3\/s'lik bir su selinin Skei\u00f0ar\u00e1rsandur buzul ovas\u0131n\u0131 h\u0131zla ge\u00e7erek buray\u0131 k\u0131sa s\u00fcreli\u011fine d\u00fcnyan\u0131n ikinci b\u00fcy\u00fck nehri haline getirdi. Sel, k\u00f6pr\u00fcleri, yollar\u0131 ve kuleleri (tahmini 14 milyon dolarl\u0131k hasar) s\u00fcr\u00fckledi ve hatta ovay\u0131 yeni topraklarla geni\u015fletti. Bu olay, buzul patlamas\u0131 selinin ders kitaplar\u0131nda yer alan bir \u00f6rne\u011fi olarak kalm\u0131\u015ft\u0131r.<\/p><cite>Tarihsel Not<\/cite><\/blockquote><\/figure>\n\n\n\n<p><strong>Buzullar\u0131 Anlamak:<\/strong> A <em>buzul erimesi<\/em> Buzullar\u0131n erimesi, bir volkanik patlama s\u0131ras\u0131nda\/sonras\u0131nda buzul alt\u0131 sular\u0131n\u0131n aniden serbest kalmas\u0131d\u0131r. Bu seller, b\u00fcy\u00fck miktarda tortu ta\u015f\u0131yarak, buzullar\u0131n erimesiyle olu\u015fan d\u00fczl\u00fcklerde \u00f6rg\u00fcl\u00fc kanallar olu\u015fturabilir. Vatnaj\u00f6kull'\u00fcn volkanik dinamikleri, bir patlama buz \u00f6rt\u00fcs\u00fcn\u00fcn taban\u0131n\u0131 eritti\u011finde bu t\u00fcr olaylara yatk\u0131n hale getirir.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Vatnaj\u00f6kull'un Outlet Buzullar\u0131<\/h2>\n\n\n\n<p>Tek sayfadan farkl\u0131 olarak Vatnaj\u00f6kull, <strong>~30 b\u00fcy\u00fck \u00e7\u0131k\u0131\u015f buzulunun<\/strong>Bunlar, ana buz \u00f6rt\u00fcs\u00fcnden d\u0131\u015far\u0131 do\u011fru, genellikle vadilere veya ovalara do\u011fru akan buz nehirleridir. Ba\u015fl\u0131ca \u00e7\u0131k\u0131\u015f noktalar\u0131 \u015funlard\u0131r:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Dyangjuj\u00f6kull<\/strong> (kuzey) - J\u00f6kuls\u00e1 \u00e1 Fj\u00f6llum nehir sistemine akar.<\/li>\n\n\n\n<li><strong>Tungna\u00e1rj\u00f6kull<\/strong> (kuzeybat\u0131) \u2013 Tungna\u00e1 nehrini (Rio Thjorsa) besler.<\/li>\n\n\n\n<li><strong>Skaft\u00e1rj\u00f6kull<\/strong> (bat\u0131-orta) - Skaft\u00e1 nehrini besler.<\/li>\n\n\n\n<li><strong>S\u00ed\u00f0uj\u00f6kull<\/strong> (bat\u0131) \u2013 Skaftafell yak\u0131nlar\u0131nda daha k\u00fc\u00e7\u00fck bir dil.<\/li>\n\n\n\n<li><strong>Skei\u00f0ar\u00e1rj\u00f6kull<\/strong> (g\u00fcney) \u2013 Skei\u00f0ar\u00e1'y\u0131 (Skaft\u00e1) bo\u015falt\u0131r ve geni\u015ftir (~15 km geni\u015fli\u011finde).<\/li>\n\n\n\n<li><strong>S\u00ed\u00f0uj\u00f6kull<\/strong> (g\u00fcneybat\u0131) - Hvannadalshnj\u00fakur'dan Skaftafell b\u00f6lgesine akar.<\/li>\n\n\n\n<li><strong>Skaftafellsj\u00f6kull<\/strong> Ve <strong>Sv\u00ednafellsj\u00f6kull<\/strong> (G\u00fcneybat\u0131) \u2013 Skaftafell'deki turist dostu diller.<\/li>\n\n\n\n<li><strong>Brei\u00f0amerkurj\u00f6kull<\/strong> (g\u00fcneydo\u011fu) \u2013 \u00fcnl\u00fc J\u00f6kuls\u00e1rl\u00f3n lag\u00fcn\u00fcn\u00fcn ve Diamond Plaj\u0131'n\u0131n kayna\u011f\u0131.<\/li>\n\n\n\n<li><strong>Da\u011f buzulu<\/strong> (g\u00fcneydo\u011fu) - Brei\u00f0amerkur'un kom\u015fusu.<\/li>\n\n\n\n<li><strong>Hoffellsj\u00f6kull<\/strong> (do\u011fu) \u2013 H\u00f6fn yak\u0131n\u0131nda daha k\u00fc\u00e7\u00fck ayak parma\u011f\u0131.<\/li>\n<\/ul>\n\n\n\n<p>Her \u00e7\u0131k\u0131\u015f\u0131n kendine \u00f6zg\u00fc ak\u0131\u015f h\u0131z\u0131 ve dinamikleri vard\u0131r. \u00d6rne\u011fin, <strong>Brei\u00f0amerkurj\u00f6kull<\/strong> J\u00f6kuls\u00e1rl\u00f3n'a buzda\u011flar\u0131 buza\u011f\u0131l\u0131yor, bu arada <strong>Skei\u00f0ar\u00e1rj\u00f6kull<\/strong> Tarihsel olarak, buzul \u00f6rt\u00fcs\u00fcn\u00fcn en h\u0131zl\u0131 hareket eden kollar\u0131ndan biri olmu\u015ftur (son on y\u0131llarda incelmesine kadar). 1900'lerin ba\u015f\u0131ndan beri bir\u00e7ok \u00e7\u0131k\u0131\u015f noktas\u0131 \u00f6nemli \u00f6l\u00e7\u00fcde geri \u00e7ekilerek, u\u00e7 buzul birikintileri ve buzul g\u00f6lleri b\u0131rakm\u0131\u015ft\u0131r.<\/p>\n\n\n\n<figure class=\"wp-block-pullquote\"><blockquote><p>Vatnaj\u00f6kull'\u00fcn bir\u00e7ok \u00e7\u0131k\u0131\u015f\u0131 otoparklardan veya k\u0131sa y\u00fcr\u00fcy\u00fc\u015flerle g\u00f6r\u00fclebilir. Skaftafellsj\u00f6kull ve Sv\u00ednafellsj\u00f6kull'e i\u015faretli patikalarla ula\u015f\u0131labilir. En b\u00fcy\u00fckleri (Skei\u00f0ar\u00e1rj\u00f6kull, Tungna\u00e1rj\u00f6kull) \u00e7o\u011funlukla sadece havadan veya \u00e7ok uzun y\u00fcr\u00fcy\u00fc\u015flerle g\u00f6r\u00fclebilir. Brei\u00f0amerkurj\u00f6kull'e ise sadece J\u00f6kuls\u00e1rl\u00f3n'daki tekne turlar\u0131yla ula\u015f\u0131labilir (a\u015fa\u011f\u0131ya bak\u0131n\u0131z).<\/p><cite>Pratik Bilgiler<\/cite><\/blockquote><\/figure>\n\n\n\n<h2 class=\"wp-block-heading\">Vatnaj\u00f6kull Milli Park\u0131: Avrupa'n\u0131n En B\u00fcy\u00fck Park\u0131<\/h2>\n\n\n\n<p>Neredeyse <em>b\u00fct\u00fcn<\/em> Buzul ve \u00e7evresi, Vatnaj\u00f6kull Milli Park\u0131 (2008'de kuruldu) olarak korunmaktad\u0131r. Park, yakla\u015f\u0131k 14.967 km\u00b2'lik bir alan\u0131 kapsamakta olup, \u0130zlanda'n\u0131n yakla\u015f\u0131k '\u00fcn\u00fc olu\u015fturarak Avrupa'n\u0131n en b\u00fcy\u00fck milli parklar\u0131ndan biridir. Eski Skaftafell ve J\u00f6kuls\u00e1rglj\u00fafur parklar\u0131n\u0131n birle\u015ftirilmesi ve geni\u015f koruma alanlar\u0131n\u0131n eklenmesiyle olu\u015fturulmu\u015ftur. Temmuz 2019'da UNESCO, park\u0131 ola\u011fan\u00fcst\u00fc jeolojik yap\u0131s\u0131 (volkanlar, buzullar, nehirler, kanyonlar) nedeniyle D\u00fcnya Miras\u0131 Listesi'ne (\"Ate\u015f ve Buz\") dahil etmi\u015ftir.<\/p>\n\n\n\n<p>Park, buzullar, devasa volkanlar ve lav alanlar\u0131, buzul nehirleri ve al\u00fcvyon ovalar\u0131, y\u00fcksek \u015felaleler ve derin kanyonlar (\u00f6rne\u011fin Fjalls\u00e1rglj\u00fafur, J\u00f6kuls\u00e1rglj\u00fafur'un baz\u0131 b\u00f6l\u00fcmleri) ve dinamik k\u0131y\u0131 lag\u00fcnleri (J\u00f6kuls\u00e1rl\u00f3n, Fjalls\u00e1rl\u00f3n) gibi \u00e7arp\u0131c\u0131 bir dizi \u00f6zelli\u011fi korumaktad\u0131r. Koruma hedefleri aras\u0131nda el de\u011fmemi\u015f vah\u015fi do\u011fan\u0131n ve dinamik s\u00fcre\u00e7lerin korunmas\u0131 yer almaktad\u0131r. Her y\u0131l park g\u00f6revlileri ve bilim insanlar\u0131 buzul de\u011fi\u015fimini, volkanik aktiviteyi ve nadir Arktik flora ve faunas\u0131n\u0131 izlemektedir.<\/p>\n\n\n\n<p><strong>Tarihsel Not:<\/strong> 7 Haziran 2008'de Vatnaj\u00f6kull Milli Park\u0131 resmen kuruldu. O d\u00f6nemde iki k\u00fc\u00e7\u00fck park\u0131 (Skaftafell ve J\u00f6kuls\u00e1rglj\u00fafur) b\u00fcnyesine katt\u0131. Bu birle\u015fmi\u015f park, hemen \u0130zlanda'n\u0131n (ve daha sonra Avrupa'n\u0131n) en b\u00fcy\u00fck milli park\u0131 oldu. Ama\u00e7, \"ate\u015f ve buz\" ekosistemini bir b\u00fct\u00fcn olarak korumakt\u0131; bu yakla\u015f\u0131m UNESCO taraf\u0131ndan 2019'da \u00f6vg\u00fcyle kar\u015f\u0131land\u0131.<\/p>\n\n\n\n<p><strong>Ziyaret\u00e7i Merkezleri:<\/strong> Park, Skaftafell (bat\u0131) ve J\u00f6kuls\u00e1rl\u00f3n'da (do\u011fu) haritalar, sergiler ve rehberlik hizmeti sunan bilgi merkezleri i\u015fletmektedir. Skaftafell merkezi (k\u0131\u015f\u0131n kapal\u0131d\u0131r) hava durumu g\u00fcncellemeleri, y\u00fcr\u00fcy\u00fc\u015f parkurlar\u0131 hakk\u0131nda bilgi ve buzul turlar\u0131 hakk\u0131nda tavsiyeler sunmaktad\u0131r. J\u00f6kuls\u00e1rl\u00f3n\/Ziyaret\u00e7i Merkezi'nde tekne turlar\u0131 rezervasyonu yapabilir ve lag\u00fcndeki vah\u015fi ya\u015fam hakk\u0131nda bilgi edinebilirsiniz. Her iki merkezde de temel yiyecek ve i\u00e7ecekler ile hediyelik e\u015fyalar mevcuttur. (Not: Giri\u015f \u00fccreti yoktur, ancak baz\u0131 otoparklar ve k\u0131\u015f turlar\u0131 i\u00e7in bilet gerekebilir.)<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">\u0130zlanda'n\u0131n En Y\u00fcksek Zirvesi: Hvannadalshnjukur<\/h2>\n\n\n\n<p>Vatnaj\u00f6kull'\u00fcn g\u00fcney yamac\u0131nda \u0130zlanda'n\u0131n zirvesi yer almaktad\u0131r: <strong>Hvannadalshnjukur<\/strong> (2.110 m). Bu zirve, \u00d6r\u00e6faj\u00f6kull volkan\u0131n\u0131n \u00fczerinde yer almaktad\u0131r. Deneyimli da\u011fc\u0131lar aras\u0131nda pop\u00fcler bir hedeftir. Skaftafell'den t\u0131rman\u0131\u015f, yakla\u015f\u0131k 1.600 m y\u00fckseklik art\u0131\u015f\u0131yla uzun bir buzul y\u00fcr\u00fcy\u00fc\u015f\u00fcd\u00fcr (gidi\u015f-d\u00f6n\u00fc\u015f 12-15+ saat). Ba\u015far\u0131l\u0131 bir t\u0131rman\u0131\u015f i\u00e7in krampon, buz baltas\u0131, ip ve bir buzul rehberi gereklidir. Yaz aylar\u0131nda bile \u00fcst yama\u00e7larda derin kar ve yar\u0131klar bulunur. Rehberler genellikle gruplar\u0131 iple ba\u011flar ve karda yol a\u00e7arlar.<\/p>\n\n\n\n<p>The <em>en iyi t\u0131rmanma sezonu<\/em> Bu d\u00f6nemde t\u0131rman\u0131\u015flar genellikle Nisan ortas\u0131ndan Haziran ay\u0131na kadar s\u00fcrer (kar daha sert ve g\u00fcn \u0131\u015f\u0131\u011f\u0131 daha uzun oldu\u011funda). Bu aylar\u0131n d\u0131\u015f\u0131nda hava daha tehlikelidir ve g\u00fcn \u0131\u015f\u0131\u011f\u0131n\u0131n k\u0131salmas\u0131 zirveye t\u0131rmanmay\u0131 daha riskli hale getirir. Buzul ge\u00e7i\u015fleri ve \u0131ss\u0131zl\u0131k g\u00f6z \u00f6n\u00fcne al\u0131nd\u0131\u011f\u0131nda, da\u011fc\u0131lar\u0131n m\u00fckemmel bir fiziksel durumda olmalar\u0131 ve tam k\u0131\u015fl\u0131k ekipman ta\u015f\u0131malar\u0131 gerekir. Zorlu\u011fa ra\u011fmen, \u00f6d\u00fcl, a\u00e7\u0131k bir g\u00fcnde Vatnaj\u00f6kull'\u00fcn t\u00fcm zirvelerinin ve Kuzey Atlantik'in panoramik manzaras\u0131d\u0131r.<\/p>\n\n\n\n<figure class=\"wp-block-pullquote\"><blockquote><p>Hvannadalshnj\u00fakur'a t\u0131rmanmay\u0131 d\u00fc\u015f\u00fcn\u00fcyorsan\u0131z, deneyimli bir rehberle gidin. Kar\/buz ko\u015fullar\u0131 her y\u0131l de\u011fi\u015fir; profesyonel rehberler \u00e7\u0131\u011f vericileri, sondalar ve telsizler ta\u015f\u0131r. Gitmeden \u00f6nce bilmeniz gerekenler: yaz aylar\u0131nda bile zirvedeki s\u0131cakl\u0131klar s\u0131f\u0131r\u0131n alt\u0131nda olabilir ve f\u0131rt\u0131nalar aniden \u00e7\u0131kabilir. Yan\u0131n\u0131zda her zaman s\u0131cak tutacak k\u0131yafetler, yiyecek ve kafa lambas\u0131 bulundurun.<\/p><cite>Pratik Bilgiler<\/cite><\/blockquote><\/figure>\n\n\n\n<h2 class=\"wp-block-heading\">J\u00f6kuls\u00e1rl\u00f3n Buzulu Lag\u00fcn\u00fc ve Diamond Plaj\u0131<\/h2>\n\n\n\n<p>J\u00f6kuls\u00e1rl\u00f3n, Vatnaj\u00f6kull'\u00fcn g\u00fcneydo\u011fu ucunda yer alan muhte\u015fem bir buzda\u011f\u0131 lag\u00fcn\u00fcd\u00fcr. Olu\u015fumu \u015fu \u015fekildedir: <strong>Brei\u00f0amerkurj\u00f6kull<\/strong> \u00c7\u0131k\u0131\u015f buzulunun 20. y\u00fczy\u0131lda geri \u00e7ekilmesiyle olu\u015fan lag\u00fcn, bug\u00fcn yakla\u015f\u0131k 18 km\u00b2'lik bir alan\u0131 kaplamakta ve \u00e7ok derin (yakla\u015f\u0131k 250 m'ye kadar) olup \u0130zlanda'n\u0131n en derin g\u00f6l\u00fcd\u00fcr. Brei\u00f0amerkurj\u00f6kull'dan s\u00fcrekli olarak buzda\u011flar\u0131 kopmakta ve turkuaz renkli suda y\u00fczmektedir. Atlantik Okyanusu'na do\u011fru s\u00fcr\u00fcklenirken, baz\u0131lar\u0131 biti\u015fik k\u0131y\u0131lara vurmaktad\u0131r. <em>Elmas Plaj\u0131<\/em> (Yukar\u0131da), buz par\u00e7alar\u0131n\u0131n m\u00fccevher gibi par\u0131ldad\u0131\u011f\u0131 siyah kumlu bir plaj. Bu foto\u011fraf \u00e7ekmeye de\u011fer manzaralar, Vatnaj\u00f6kull ziyaretinin en \u00f6nemli noktalar\u0131ndand\u0131r.<\/p>\n\n\n\n<p>K\u0131y\u0131dan kalkan tekne turlar\u0131, turistlerin buz da\u011flar\u0131 aras\u0131nda s\u00fcz\u00fclmelerine olanak tan\u0131r. Yar\u0131 amfibik tekneler ve daha k\u00fc\u00e7\u00fck zodyak turlar\u0131 yaz aylar\u0131nda (\u00e7o\u011funlukla J\u00f6kuls\u00e1rl\u00f3n ve yak\u0131n\u0131ndaki Fjalls\u00e1rl\u00f3n \u00e7evresinde) d\u00fczenlenmektedir. Bu turlar y\u0131l boyunca (hava ko\u015fullar\u0131 elveri\u015fli oldu\u011fu s\u00fcrece) d\u00fczenlenmekte ve lag\u00fcn\u00fcn buzlar\u0131 ile burada ya\u015fayan foklar\u0131n e\u015fsiz manzaralar\u0131n\u0131 sunmaktad\u0131r. Liman foklar\u0131 burada s\u0131k s\u0131k buz da\u011flar\u0131n\u0131n \u00fczerinde uzan\u0131r veya teknelerin yan\u0131nda y\u00fczerler. (K\u0131\u015f\u0131n, lag\u00fcn\u00fcn baz\u0131 k\u0131s\u0131mlar\u0131 donabilir, ancak baz\u0131 turlar a\u00e7\u0131k kanallar\u0131 kullanarak yine de d\u00fczenlenmektedir.) Deniz ya\u015fam\u0131 da g\u00f6r\u00fclmektedir: eider \u00f6rdekleri ve sumrular g\u00f6r\u00fclebilir ve zaman zaman balinalar veya yunuslar buzlu ak\u0131nt\u0131dan ge\u00e7ebilir.<\/p>\n\n\n\n<figure class=\"wp-block-pullquote\"><blockquote><p>Elmas Plaj\u0131'n\u0131 g\u00fcn do\u011fumu veya g\u00fcn bat\u0131m\u0131nda ziyaret edin; al\u00e7aktan gelen g\u00fcne\u015f, siyah kum \u00fczerindeki buzu arkadan ayd\u0131nlatarak \u00e7arp\u0131c\u0131 foto\u011fraflar \u00e7ekmenizi sa\u011flar. Ge\u00e7 ilkbahar ve erken sonbahar genellikle ideal \u0131\u015f\u0131k ko\u015fullar\u0131na sahiptir. Ayr\u0131ca J\u00f6kuls\u00e1rl\u00f3n'daki otopark\u0131n yo\u011fun olabilece\u011fini unutmay\u0131n; kalabal\u0131\u011f\u0131 \u00f6nlemek i\u00e7in sabah erken veya ak\u015fam ge\u00e7 saatlerde ziyaret edin.<\/p><cite>\u0130\u00e7eriden bir ipucu<\/cite><\/blockquote><\/figure>\n\n\n\n<p>J\u00f6kuls\u00e1rl\u00f3n'un hemen bat\u0131s\u0131nda yer alan daha k\u00fc\u00e7\u00fck bir buzda\u011f\u0131 g\u00f6l\u00fc olan Fjalls\u00e1rl\u00f3n, daha sakin ama benzer bir deneyim sunuyor (Fjallsj\u00f6kull nehrinin ak\u0131nt\u0131s\u0131yla besleniyor). Her iki lag\u00fcn de filmlerde yer ald\u0131 (\u00f6rne\u011fin, <em>James Bond<\/em>, <em>Batman Ba\u015fl\u0131yor<\/em>) ola\u011fan\u00fcst\u00fc g\u00fczellikleri nedeniyle.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Vatnaj\u00f6kull Buz Ma\u011faralar\u0131<\/h2>\n\n\n\n<p>Vatnaj\u00f6kull'un buzullar\u0131 pek \u00e7ok buzulu bar\u0131nd\u0131r\u0131yor <strong>buz ma\u011faralar\u0131<\/strong> \u2013 Eriyen buz sular\u0131n\u0131n oydu\u011fu mevsimsel t\u00fcneller. Bu ma\u011faralar her k\u0131\u015f (genellikle Ekim-Mart aylar\u0131 aras\u0131nda) y\u00fczeydeki eriyen buz sular\u0131n\u0131n buzun i\u00e7inden akmas\u0131yla yeniden olu\u015fur. Ma\u011faralar genellikle yaz sonuna do\u011fru \u00e7\u00f6ker, bu nedenle her k\u0131\u015f yeni bir a\u011f olu\u015fur. Buz duvarlar\u0131 canl\u0131 mavi bir renkte parlayarak ger\u00e7ek\u00fcst\u00fc odalar yarat\u0131r. \u00d6nemli ma\u011fara alanlar\u0131ndan baz\u0131lar\u0131 kuzeyde Kverkfj\u00f6ll'\u00fcn alt\u0131nda ve g\u00fcneyde Svinafellsj\u00f6kull\/Skaftafell \u00e7evresindedir. (Bir\u00e7ok tur ayr\u0131ca buzul kenarlar\u0131ndaki yaz \"buz t\u00fcnellerini\" de ziyaret eder.)<\/p>\n\n\n\n<p>Buz ma\u011faralar\u0131 son derece k\u0131r\u0131lgand\u0131r ve tek ba\u015f\u0131na girilmesi \u00f6l\u00fcmc\u00fcl olabilir. <strong>Her zaman bir rehber kullan\u0131n.<\/strong> H\u00f6fn ve Skaftafell'deki tur operat\u00f6rleri, baret ve \u0131\u015f\u0131klarla donat\u0131lm\u0131\u015f rehberli buz ma\u011faras\u0131 turlar\u0131 d\u00fczenliyor. Yo\u011fun sezonda (Kas\u0131m-Mart), buzul buzunda yakla\u015f\u0131k 2-4 km y\u00fcr\u00fcy\u00fc\u015f yapabilir, ard\u0131ndan 50-200 metre kadar ma\u011faraya s\u00fcr\u00fcnerek girebilirsiniz. \u0130\u00e7eride, yo\u011fun buz nedeniyle \u00e7ok parlak mavi duvarlar ve donmu\u015f erime suyundan olu\u015fan sark\u0131tlar g\u00f6receksiniz. Ortam s\u0131cakl\u0131\u011f\u0131 0\u00b0C'nin hemen alt\u0131nda. Sa\u011flam botlar, kramponlar ve katmanl\u0131 giysiler \u015fart. Bir\u00e7ok rehber g\u00fcvenlik nedeniyle ma\u011faraya giri\u015f s\u00fcrelerini s\u0131n\u0131rl\u0131yor. Ma\u011faralar\u0131n akusti\u011fi de olduk\u00e7a belirgin: uzaktan gelen bir damlama veya \u00e7atlama sesi \u00fcrk\u00fct\u00fcc\u00fc derecede y\u00fcksek, bu nedenle dinlemek de\u011fi\u015fiklikleri \u00f6nceden tahmin etmenize yard\u0131mc\u0131 olur.<\/p>\n\n\n\n<figure class=\"wp-block-pullquote\"><blockquote><p>Buz ma\u011faras\u0131 turlar\u0131 son derece pop\u00fclerdir. K\u0131\u015f aylar\u0131nda ziyaret edecekseniz aylar \u00f6ncesinden rezervasyon yapt\u0131r\u0131n. Tur fiyatlar\u0131 de\u011fi\u015fmektedir (k\u00fc\u00e7\u00fck grup y\u00fcr\u00fcy\u00fc\u015f\u00fc + buz ma\u011faras\u0131 i\u00e7in ki\u015fi ba\u015f\u0131 yakla\u015f\u0131k 100-200 dolar) ve genellikle gerekli t\u00fcm ekipmanlar\u0131 i\u00e7ermektedir. Tur sa\u011flay\u0131c\u0131lar\u0131 genellikle g\u00fcvenlik bilgilendirmeleri ve yak\u0131ndaki kasabalardan servis hizmeti sunmaktad\u0131r. Unutmay\u0131n: i\u015faretlenmemi\u015f yollardan ke\u015fif yapmak yasakt\u0131r. Taze karda derin ayak izleri bile gizli bir ma\u011faray\u0131 i\u015faret eder \u2013 i\u015faretlenmi\u015f yollardan ayr\u0131lmak yasakt\u0131r.<\/p><cite>Pratik Bilgiler<\/cite><\/blockquote><\/figure>\n\n\n\n<h2 class=\"wp-block-heading\">Vatnaj\u00f6kull'de Yap\u0131lacak Aktiviteler ve Maceralar<\/h2>\n\n\n\n<p>Vatnaj\u00f6kull, deneyimli gezginler i\u00e7in bir macera cennetidir. Ba\u015fl\u0131ca aktiviteler \u015funlard\u0131r:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Buzul Y\u00fcr\u00fcy\u00fc\u015f\u00fc:<\/strong> Buz \u00fczerinde rehberli y\u00fcr\u00fcy\u00fc\u015fler (genellikle 2-6 saat). Krampon ve ip gereklidir. Geziler, kolay d\u00fcz y\u00fcr\u00fcy\u00fc\u015flerden (\u00f6rne\u011fin Sv\u00ednafellsj\u00f6kull'da) zorlu t\u0131rman\u0131\u015flara kadar de\u011fi\u015fmektedir. Basit y\u00fcr\u00fcy\u00fc\u015fler i\u00e7in uygun, formda yeni ba\u015flayanlar i\u00e7in uygundur.<\/li>\n\n\n\n<li><strong>Buz T\u0131rman\u0131\u015f\u0131:<\/strong> Buzul dillerindeki dikey buz duvarlar\u0131 (Skaftafell'de yayg\u0131n). T\u0131rman\u0131c\u0131lar buz baltas\u0131 ve emniyet kemeri kullan\u0131rlar. Bu yar\u0131m g\u00fcnl\u00fck veya tam g\u00fcnl\u00fck turlar daha y\u00fcksek kondisyon ve g\u00fc\u00e7 gerektirir.<\/li>\n\n\n\n<li><strong>Kar motoruyla gezinti:<\/strong> Yaz aylar\u0131nda buz \u00f6rt\u00fcs\u00fcnde kar motoruyla gezinti (Stafafell \u00fcss\u00fcnden). S\u00fcr\u00fcc\u00fcler, buz \u00fczerindeki izlerde karl\u0131 platolar ve s\u0131rtlar boyunca h\u0131zla ilerliyorlar \u2013 geni\u015f buz alan\u0131n\u0131 deneyimlemenin heyecan verici bir yolu.<\/li>\n\n\n\n<li><strong>Foto\u011fraf Turlar\u0131:<\/strong> \u00d6zel turlar g\u00fcn do\u011fumu\/g\u00fcn bat\u0131m\u0131 foto\u011fraf\u00e7\u0131l\u0131\u011f\u0131na (buz ma\u011faralar\u0131, lag\u00fcnler, buzul zirvesi panoramalar\u0131) odaklanmaktad\u0131r. Rehberler en iyi \u0131\u015f\u0131\u011f\u0131 ve g\u00fcvenli g\u00f6r\u00fc\u015f noktalar\u0131n\u0131 bilirler.<\/li>\n\n\n\n<li><strong>\u00c7ok G\u00fcnl\u00fck Geziler:<\/strong> Uzman ekipler taraf\u0131ndan d\u00fczenlenen, da\u011f kul\u00fcbelerinde konaklayarak buz \u00f6rt\u00fcs\u00fcn\u00fc a\u015fan (7-14 g\u00fcn s\u00fcren) ke\u015fif gezileri. Bu geziler ke\u015fif becerileri gerektirir ve genellikle buzulun merkezine ula\u015fmay\u0131 i\u00e7erir.<\/li>\n<\/ul>\n\n\n\n<p>T\u00fcm buzul aktiviteleri <em>mutlak<\/em> Rehber e\u015fli\u011finde y\u00fcr\u00fcy\u00fc\u015f yap\u0131n. Basit y\u00fcr\u00fcy\u00fc\u015flerde bile g\u00fcvenlik halatlar\u0131 ve ekipmanlar\u0131 kullan\u0131l\u0131r. Yerel i\u015fletmeciler (\u00f6rne\u011fin Glacier Guides, Arctic Adventures) buz \u00fczerindeki havan\u0131n h\u0131zla de\u011fi\u015fti\u011fini vurguluyor. Rehberler acil durumlar i\u00e7in uydu telefonlar\u0131 ta\u015f\u0131yor. Vatnaj\u00f6kull i\u00e7in (baz\u0131 bat\u0131 buzullar\u0131n\u0131n aksine) izin gerekmiyor, ancak resmi tavsiye her zaman akredite bir rehber tutmak ve park g\u00f6revlilerini plan\u0131n\u0131z hakk\u0131nda bilgilendirmektir.<\/p>\n\n\n\n<figure class=\"wp-block-pullquote\"><blockquote><p>Buz botlar\u0131, kramponlar, emniyet kemerleri gibi ekipman kiralama hizmetleri \u00e7o\u011fu rehberlik \u015firketinde mevcuttur. S\u0131cak i\u00e7 katmanlar ve r\u00fczgar ge\u00e7irmez d\u0131\u015f giysiler \u015fiddetle tavsiye edilir; yaz aylar\u0131nda bile Vatnaj\u00f6kull'den gelen r\u00fczgar s\u0131cakl\u0131\u011f\u0131 \u00f6nemli \u00f6l\u00e7\u00fcde d\u00fc\u015f\u00fcrebilir. Rak\u0131mlar\u0131n d\u00fc\u015f\u00fck (\u22642.110 m) oldu\u011funu, bu nedenle y\u00fckseklik hastal\u0131\u011f\u0131n\u0131n nadir oldu\u011funu, ancak so\u011fuk ve a\u00e7\u0131kta kalman\u0131n ger\u00e7ek tehlikeler oldu\u011funu unutmay\u0131n.<\/p><cite>Pratik Bilgiler<\/cite><\/blockquote><\/figure>\n\n\n\n<h2 class=\"wp-block-heading\">Vatnaj\u00f6kull'\u00fc Nas\u0131l Ziyaret Edebilirsiniz: Kapsaml\u0131 Planlama Rehberi<\/h2>\n\n\n\n<p><strong>Ula\u015f\u0131m:<\/strong> \u0130zlanda'y\u0131 \u00e7evreleyen \u00c7evre Yolu (1 Numaral\u0131 G\u00fczergah), Vatnaj\u00f6kull'\u00fcn g\u00fcney kenar\u0131 boyunca uzan\u0131r. Reykjav\u00edk'ten 1 Numaral\u0131 G\u00fczergah \u00fczerinden do\u011fuya do\u011fru ilerleyin: Skaftafell\/Skaft\u00e1rdalur (bat\u0131 buzul giri\u015fi) V\u00edk \u00fczerinden yakla\u015f\u0131k 330 km (5-6 saat) uzakl\u0131ktad\u0131r. J\u00f6kuls\u00e1rl\u00f3n (do\u011fu lag\u00fcn\u00fc) H\u00f6fn \u00fczerinden yakla\u015f\u0131k 380 km (5,5-6,5 saat) uzakl\u0131ktad\u0131r. (Buzulun kuzeyinden ge\u00e7en) yollar yaz aylar\u0131nda iyi bak\u0131ml\u0131d\u0131r. K\u0131\u015f\u0131n, yo\u011fun kar ya\u011f\u0131\u015f\u0131 1 Numaral\u0131 G\u00fczergah\u0131n baz\u0131 b\u00f6l\u00fcmlerini kapatabilir (seyahatten \u00f6nce \u0130zlanda Karayollar\u0131 \u0130daresi sitesini kontrol edin). Buzulun i\u00e7ine hi\u00e7bir yol girmez; t\u00fcm turlar ana merkezlerden (Skaftafell, H\u00f6fn, vb.) hareket eder.<\/p>\n\n\n\n<p><strong>Giri\u015f Noktalar\u0131 ve Tesisler:<\/strong><br>\u2013 <em>Skaftafell (Bat\u0131 Yakas\u0131):<\/em> Burada bir ziyaret\u00e7i merkezi, kamp alan\u0131 ve buzullara giden patikalar\u0131n ba\u015flang\u0131\u00e7 \u200b\u200bnoktalar\u0131 (\u00f6rne\u011fin Sv\u00ednafellsj\u00f6kull) bulunmaktad\u0131r. Buras\u0131 y\u00fcr\u00fcy\u00fc\u015fler ve buz ma\u011faralar\u0131 i\u00e7in \u00f6nemli bir merkezdir. Konaklama yerleri, hosteller ve bir kamp alan\u0131 mevcuttur.<br>\u2013 <em>J\u00f6kuls\u00e1rl\u00f3n (Do\u011fu Yakas\u0131):<\/em> Lag\u00fcn kenar\u0131ndaki k\u00fc\u00e7\u00fck ziyaret\u00e7i merkezinde otopark, tuvalet ve tekne turlar\u0131 mevcuttur. Konaklama (oteller\/pansiyonlar) ise yak\u0131ndaki H\u00f6fn'de (~80 km do\u011fuda) bulunmaktad\u0131r.<br>\u2013 <em>Liman:<\/em> Vatnaj\u00f6kull'\u00fcn do\u011fusunda yer alan ve \"\u0131stakoz ba\u015fkenti\" olarak adland\u0131r\u0131lan kasaba, do\u011fu buzullar\u0131na yap\u0131lan turlar i\u00e7in bir \u00fcs g\u00f6revi g\u00f6r\u00fcyor (Brei\u00f0amerkurj\u00f6kull yak\u0131nlar\u0131nda). Kasabada \u00e7e\u015fitli otel ve restoranlar bulunmaktad\u0131r.<br>\u2013 <em>Eri\u015fim Yollar\u0131:<\/em> Vatnaj\u00f6kull'\u00fcn kuzeyinde (\u00f6rne\u011fin F88, F905) i\u00e7 kesimlerdeki yaylalara ba\u011flanan F yollar\u0131 (engebeli \u00e7ak\u0131ll\u0131 yollar) bulunmaktad\u0131r (sadece 4x4 ara\u00e7lar i\u00e7in uygundur). Bu yollar nehir ge\u00e7i\u015flerini gerektirir ve sadece yaz aylar\u0131nda Super Jeep'lerle ge\u00e7ilebilir.<\/p>\n\n\n\n<p><strong>Ziyaret i\u00e7in en uygun zaman (ay baz\u0131nda):<\/strong><\/p>\n\n\n\n<figure class=\"wp-block-table\"><table class=\"has-fixed-layout\"><thead><tr><td>Ay<\/td><td>Ko\u015fullar ve \u00d6ne \u00c7\u0131kanlar<\/td><\/tr><\/thead><tbody><tr><td><strong>Ocak-\u015eubat<\/strong><\/td><td>Derin k\u0131\u015f: bol kar, k\u0131sa g\u00fcnler (4-6 saat ayd\u0131nl\u0131k). Buz ma\u011faralar\u0131 mevcut; bir\u00e7ok patika karla kapl\u0131. Tekne turlar\u0131 mevsimlik (donmu\u015f lag\u00fcn). Karl\u0131 manzaralar e\u015fli\u011finde Kuzey I\u015f\u0131klar\u0131n\u0131 izlemek i\u00e7in ideal.<\/td><\/tr><tr><td><strong>Mart-Nisan<\/strong><\/td><td>Bahara ge\u00e7i\u015f. Buz ma\u011faralar\u0131 hala a\u00e7\u0131k; uzun g\u00fcn \u0131\u015f\u0131\u011f\u0131 ba\u015fl\u0131yor. Kar motoru sezonu aktif. Yollar Nisan sonuna kadar buzlu kal\u0131yor. Erken y\u00fcr\u00fcy\u00fc\u015f (kramponlarla) m\u00fcmk\u00fcn.<\/td><\/tr><tr><td><strong>May\u0131s<\/strong><\/td><td>Ge\u00e7 bahar: G\u00fcn \u0131\u015f\u0131\u011f\u0131nda h\u0131zl\u0131 art\u0131\u015f, kar s\u0131n\u0131r\u0131n\u0131n geri \u00e7ekilmesi. Buzulda baz\u0131 turlar ba\u015fl\u0131yor. Yollar temizleniyor. Skaftafell'de bir\u00e7ok k\u0131r \u00e7i\u00e7e\u011fi var. Kalabal\u0131k hala orta seviyede.<\/td><\/tr><tr><td><strong>Haziran\u2013A\u011fustos<\/strong><\/td><td>En yo\u011fun sezon. Yaz boyunca: uzun (Haziran'da 24 saat) g\u00fcn \u0131\u015f\u0131\u011f\u0131, al\u00e7ak patikalarda minimum kar. T\u00fcm turlar d\u00fczenleniyor (y\u00fcr\u00fcy\u00fc\u015f, buz t\u0131rman\u0131\u015f\u0131, tekne gezisi). J\u00f6kuls\u00e1rl\u00f3n'da gemiyle ula\u015f\u0131m m\u00fcmk\u00fcn. Karayolu eri\u015fimi g\u00fcvenilir. En fazla turisti ve daha y\u00fcksek fiyatlar\u0131 bekleyin.<\/td><\/tr><tr><td><strong>Eyl\u00fcl<\/strong><\/td><td>Sonbahar\u0131n ba\u015f\u0131: daha serin, daha az kalabal\u0131k. Baz\u0131 buz ma\u011faralar\u0131 olu\u015fmaya ba\u015flar (\u00f6zellikle Ekim ay\u0131nda). Geceler geri d\u00f6nerken Kuzey I\u015f\u0131klar\u0131 g\u00f6r\u00fclebilir. Fiyort bal\u0131k\u00e7\u0131l\u0131\u011f\u0131 sezonu (H\u00f6fn).<\/td><\/tr><tr><td><strong>Ekim-Kas\u0131m<\/strong><\/td><td>\u0130lk kar ya\u011f\u0131\u015flar\u0131. Buz ma\u011faralar\u0131 Kas\u0131m ay\u0131nda (hava \u015fartlar\u0131 elveri\u015fliyse) a\u00e7\u0131l\u0131yor. Bir\u00e7ok tur operat\u00f6r\u00fc Kas\u0131m ortas\u0131na kadar turlar\u0131n\u0131 sonland\u0131r\u0131yor. F\u0131rt\u0131nalardan sonra yollar kapanmaya ba\u015flayabilir. Buzullar\u0131n kenarlar\u0131nda muhte\u015fem sonbahar renkleri.<\/td><\/tr><tr><td><strong>Aral\u0131k<\/strong><\/td><td>Karanl\u0131k k\u0131\u015f geri d\u00f6n\u00fcyor. Buz ma\u011faralar\u0131 kesinlikle a\u00e7\u0131k; g\u00fcnler \u00e7ok k\u0131sa (Aral\u0131k ay\u0131nda 4-5 saat). Buzulda kayak turu m\u00fcmk\u00fcn. Buzulda kar motoru kullan\u0131m\u0131 m\u00fcmk\u00fcn. Yollar genellikle f\u0131rt\u0131nalardan etkilenir \u2013 g\u00fcncellemeleri kontrol edin.<\/td><\/tr><\/tbody><\/table><\/figure>\n\n\n\n<p><strong>Planlama Notu:<\/strong> Yaz aylar\u0131 (Haziran-A\u011fustos) ula\u015f\u0131m a\u00e7\u0131s\u0131ndan en uygun d\u00f6nemdir, ancak ayn\u0131 zamanda en yo\u011fun ve en pahal\u0131 d\u00f6nemdir. K\u0131\u015f aylar\u0131nda ziyaret ediyorsan\u0131z, bir\u00e7ok hizmetin ask\u0131ya al\u0131nd\u0131\u011f\u0131n\u0131 veya faaliyetlerini azaltt\u0131\u011f\u0131n\u0131 unutmay\u0131n. Her zaman kontrol edin. <strong>yol.d\u0131r<\/strong> Karayolu ve hava ko\u015fullar\u0131 i\u00e7in (\u00f6zellikle Kas\u0131m-Mart aylar\u0131 aras\u0131nda).<\/p>\n\n\n\n<p><strong>Neleri Yan\u0131n\u0131za Almal\u0131s\u0131n\u0131z:<\/strong> Y\u00fcn\/i\u00e7 katmanlar, yal\u0131t\u0131ml\u0131 ceket, su ge\u00e7irmez d\u0131\u015f katman. Sa\u011flam y\u00fcr\u00fcy\u00fc\u015f botlar\u0131 (su ge\u00e7irmez, bilek deste\u011fi). S\u0131cak \u015fapka, eldiven ve g\u00fcne\u015f g\u00f6zl\u00fc\u011f\u00fc (kardan yans\u0131yan parlamay\u0131 \u00f6nler). Buzul turlar\u0131 i\u00e7in k\u00fc\u00e7\u00fck bir s\u0131rt \u00e7antas\u0131, yedek pilleri olan bir kamera (so\u011fuk pilin \u00f6mr\u00fcn\u00fc k\u0131salt\u0131r) getirin. Tur \u015firketleri genellikle emniyet kemeri, krampon ve kask sa\u011flar; i\u00e7 katmanlar\u0131n\u0131z s\u0131cak olmal\u0131d\u0131r. Kendi arac\u0131n\u0131zla gidiyorsan\u0131z, acil durum battaniyesi ve yedeklerini yan\u0131n\u0131zda bulundurun (yollar \u0131ss\u0131z olabilir).<\/p>\n\n\n\n<p><strong>K\u0131lavuzlar ve G\u00fcvenlik:<\/strong> Buzullara seyahat veya buz aktiviteleri i\u00e7in sertifikal\u0131 bir rehber tutun. Lisansl\u0131 \u015firketler g\u00fcvenli rotalar\u0131 bilir ve acil durum ekipmanlar\u0131 ta\u015f\u0131r. Vatnaj\u00f6kull'e tek ba\u015f\u0131na gitmek kesinlikle \u00f6nerilmez. Planlar\u0131n\u0131z\u0131 ve tahmini d\u00f6n\u00fc\u015f saatinizi her zaman birine bildirin. Hava durumu h\u0131zla de\u011fi\u015febilir; a\u00e7\u0131k g\u00f6ky\u00fcz\u00fc alt\u0131nda yola \u00e7\u0131k\u0131p saatler i\u00e7inde tipi benzeri bir sisle kar\u015f\u0131la\u015fmak yayg\u0131nd\u0131r.<\/p>\n\n\n\n<p><strong>Maliyetler ve B\u00fct\u00e7e:<\/strong> Tur fiyatlar\u0131 de\u011fi\u015fkenlik g\u00f6sterir: 1-2 saatlik basit buzul y\u00fcr\u00fcy\u00fc\u015fleri genellikle ki\u015fi ba\u015f\u0131 100-200 \u20ac; tam g\u00fcnl\u00fck y\u00fcr\u00fcy\u00fc\u015fler 200-300 \u20ac civar\u0131ndad\u0131r. Buz ma\u011faras\u0131 turlar\u0131 (ekipman dahil) benzer fiyatlardad\u0131r. J\u00f6kuls\u00e1rl\u00f3n'da tekne turlar\u0131 30-50 \u20ac civar\u0131ndad\u0131r. Vatnaj\u00f6kull yak\u0131nlar\u0131ndaki konaklama se\u00e7enekleri, uygun fiyatl\u0131 pansiyonlardan (~100 \u20ac\/gece) l\u00fcks otellere (200 \u20ac ve \u00fczeri) kadar de\u011fi\u015fmektedir. Ara\u00e7 kiralama (k\u0131\u015f\u0131n 4x4 \u00f6nerilir), yak\u0131t, yemek (H\u00f6fn'deki restoranlar daha pahal\u0131d\u0131r) ve de\u011fi\u015fen ko\u015fullar i\u00e7in sigorta masraflar\u0131n\u0131 da hesaba kat\u0131n.<\/p>\n\n\n\n<p><strong>Eri\u015filebilirlik:<\/strong> Turistik altyap\u0131n\u0131n \u00e7o\u011fu (merkezler, k\u0131sa y\u00fcr\u00fcy\u00fc\u015f parkurlar\u0131) otopark alanlar\u0131nda veya yak\u0131n\u0131ndad\u0131r. Ancak, buzul arazisine tekerlekli ara\u00e7larla eri\u015fim m\u00fcmk\u00fcn de\u011fildir. Baz\u0131 tur \u015firketleri, minimum y\u00fcr\u00fcy\u00fc\u015f gerektiren kar motoru deneyimleri sunmaktad\u0131r. Tekerlekli sandalye eri\u015fimi: S\u0131n\u0131rl\u0131 \u2013 arazi engebeli. Ziyaret\u00e7i merkezleri \u00e7o\u011funlukla tekerlekli sandalye dostudur, ancak do\u011fal alanlarda (\u00f6rne\u011fin J\u00f6kuls\u00e1rl\u00f3n) zemin engebeli olabilir.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">\u0130klim De\u011fi\u015fikli\u011fi ve Vatnaj\u00f6kull'\u00fcn Gelece\u011fi<\/h2>\n\n\n\n<p>Vatnaj\u00f6kull buzulu \u00f6l\u00e7\u00fclebilir bir \u015fekilde k\u00fc\u00e7\u00fcl\u00fcyor. T\u00fcm \u0130zlanda buzullar\u0131 gibi, K\u00fc\u00e7\u00fck Buz \u00c7a\u011f\u0131'nda (yakla\u015f\u0131k 1600'ler) zirveye ula\u015fm\u0131\u015f ve o zamandan beri gerilemi\u015ftir. Tahminler, \u0130zlanda buzullar\u0131n\u0131n 1890'dan beri alanlar\u0131n\u0131n yakla\u015f\u0131k 'sini kaybetti\u011fini g\u00f6steriyor; bu kayb\u0131n b\u00fcy\u00fck bir k\u0131sm\u0131 Vatnaj\u00f6kull ve Langj\u00f6kull'dan kaynaklan\u0131yor. 2000'li ve 2010'lu y\u0131llarda buzul erimesi h\u0131zland\u0131: 2000-2017 y\u0131llar\u0131 aras\u0131nda \u0130zlanda buzulu y\u0131lda ortalama ~43 km\u00b2 kaybetti. Vatnaj\u00f6kull buz \u00f6rt\u00fcs\u00fc \u015fu anda y\u0131lda ortalama 1 m inceliyor (kenarlarda daha fazla incelme oluyor). Ba\u011flam a\u00e7\u0131s\u0131ndan, Vatnaj\u00f6kull ~3.000 km\u00b3 buz i\u00e7eriyor (\u0130zlanda'n\u0131n toplam buzunun '\u0131ndan fazlas\u0131); tamamen erirse k\u00fcresel deniz seviyesini ~1 cm y\u00fckseltecektir.<\/p>\n\n\n\n<p>Bilim insanlar\u0131, k\u00fcresel \u0131s\u0131nma alt\u0131nda buzullar\u0131n geri \u00e7ekilmesinin devam edece\u011fini \u00f6ng\u00f6r\u00fcyor. Modeller, iklim birka\u00e7 derece \u0131s\u0131n\u0131rsa buzulun \u00f6n\u00fcm\u00fczdeki y\u00fczy\u0131lda hacminin yar\u0131s\u0131n\u0131 kaybedebilece\u011fini g\u00f6steriyor. Zaten, birka\u00e7 \u00e7\u0131k\u0131\u015f buzulunun \u00f6nemli \u00f6l\u00e7\u00fcde geri \u00e7ekilmesiyle ana kaya ortaya \u00e7\u0131kt\u0131 ve yeni g\u00f6ller olu\u015ftu. Buz kayb\u0131 yerel hidrolojiyi de etkiliyor: Son on y\u0131llarda yaz aylar\u0131ndaki erime suyu ak\u0131\u015f\u0131 artt\u0131 ve bu da nehirlerdeki tortu y\u00fck\u00fcn\u00fc ve hidroelektrik kaynaklar\u0131n\u0131 etkiledi.<\/p>\n\n\n\n<p><strong>\u0130klim Ba\u011flam\u0131:<\/strong> G\u00f6zlemevleri, \u0130zlanda'n\u0131n y\u00fcksek ya\u011f\u0131\u015f miktar\u0131 ve denizden gelen s\u0131cak hava nedeniyle Vatnaj\u00f6kull'\u00fcn geri \u00e7ekilmesinin bir\u00e7ok k\u00fc\u00e7\u00fck buzuldan daha h\u0131zl\u0131 oldu\u011funu belirtiyor. Buzul, hassas bir iklim g\u00f6stergesidir: kar ya\u011f\u0131\u015f\u0131ndaki azalma veya erimedeki art\u0131\u015f, hacim kayb\u0131na h\u0131zla yol a\u00e7ar (daha k\u00fc\u00e7\u00fck \u00f6l\u00e7ekte Gr\u00f6nland'\u0131n \u00e7\u0131k\u0131\u015f buzullar\u0131na \u00e7ok benzer). Bu durum, k\u00fcresel iklim endi\u015felerini g\u00fc\u00e7lendiriyor.<\/p>\n\n\n\n<p>Ancak Vatnaj\u00f6kull'\u00fcn muazzam boyutu, bir gecede yok olmayaca\u011f\u0131 anlam\u0131na geliyor. Baz\u0131 bilim insanlar\u0131, \u015fiddetli \u0131s\u0131nma alt\u0131nda bile, 21. y\u00fczy\u0131l\u0131n sonlar\u0131na kadar \u00f6nemli bir buz k\u00fctlesi olarak (her ne kadar olduk\u00e7a azalm\u0131\u015f olsa da) kalabilece\u011fini tahmin ediyor. \u0130zlanda Meteoroloji Ofisi ve buzul bilimciler taraf\u0131ndan yap\u0131lan s\u00fcrekli izleme, her y\u0131l kal\u0131nl\u0131k de\u011fi\u015fimine (k\u00fctle dengesi) ili\u015fkin g\u00fcncel verilerin elde edilmesini sa\u011fl\u0131yor.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Vatnaj\u00f6kull ve Di\u011fer B\u00fcy\u00fck Buzullar<\/h2>\n\n\n\n<p>\u0130\u015fte Vatnaj\u00f6kull'\u00fcn di\u011fer \u00fcnl\u00fc buz k\u00fctleleriyle kar\u015f\u0131la\u015ft\u0131rmas\u0131:<\/p>\n\n\n\n<figure class=\"wp-block-table\"><table class=\"has-fixed-layout\"><thead><tr><td>Buzul \/ Buz \u00d6rt\u00fcs\u00fc<\/td><td>Konum<\/td><td>Alan (km\u00b2)<\/td><td>Notlar<\/td><\/tr><\/thead><tbody><tr><td><strong>Vatnaj\u00f6kull<\/strong><\/td><td>\u0130zlanda<\/td><td>~8,100<\/td><td>\u0130zlanda'n\u0131n en b\u00fcy\u00fc\u011f\u00fc; <em>genellikle Avrupa'n\u0131n en b\u00fcy\u00fc\u011f\u00fc olarak an\u0131l\u0131r<\/em> Kuzey Kutbu'nun d\u0131\u015f\u0131nda. Hacim ~3.000 km\u00b3.<\/td><\/tr><tr><td><strong>Severny Adas\u0131 Buz \u00d6rt\u00fcs\u00fc<\/strong><\/td><td>Novaya Zemlya, Rusya<\/td><td>~20,500<\/td><td>Alan bak\u0131m\u0131ndan en b\u00fcy\u00fc\u011f\u00fc (Avrupa) Rusya'da bulunur \u2013 Kuzey Kutbu'nun en kuzeyinde yer al\u0131r, bu nedenle genellikle \"Avrupa\" say\u0131m\u0131na dahil edilmez.<\/td><\/tr><tr><td><strong>Austfonna (Kuzeydo\u011fu)<\/strong><\/td><td>Svalbard, Norve\u00e7<\/td><td>~8,100<\/td><td>Alan bak\u0131m\u0131ndan yakla\u015f\u0131k olarak Vatnaj\u00f6kull'a (Svalbard'\u0131n en b\u00fcy\u00fck buz \u00f6rt\u00fcs\u00fc) e\u015fittir. Norve\u00e7'te alan bak\u0131m\u0131ndan en b\u00fcy\u00fck buz \u00f6rt\u00fcs\u00fcd\u00fcr.<\/td><\/tr><tr><td><strong>Langj\u00f6kull<\/strong><\/td><td>\u0130zlanda<\/td><td>~950<\/td><td>\u0130zlanda'n\u0131n ikinci en b\u00fcy\u00fck buz \u00f6rt\u00fcs\u00fc (Bat\u0131 Yaylalar\u0131).<\/td><\/tr><tr><td><strong>Hofsj\u00f6kull<\/strong><\/td><td>\u0130zlanda<\/td><td>~925<\/td><td>\u0130zlanda'n\u0131n 3. en b\u00fcy\u00fck buz \u00f6rt\u00fcs\u00fc (Orta Yaylalar).<\/td><\/tr><tr><td><strong>Jostedalsbreen<\/strong><\/td><td>Norve\u00e7 (Anakara)<\/td><td>~487<\/td><td>Norve\u00e7'in (Avrupa anakaras\u0131ndaki) en b\u00fcy\u00fck buzulu.<\/td><\/tr><tr><td><strong>Aletsch<\/strong><\/td><td>\u0130svi\u00e7re (Alpler)<\/td><td>~79<\/td><td>Uzunluk\/alan bak\u0131m\u0131ndan Avrupa'n\u0131n en b\u00fcy\u00fck (Arktik olmayan) da\u011f buzulu.<\/td><\/tr><\/tbody><\/table><\/figure>\n\n\n\n<p>Vatnaj\u00f6kull, ana karadaki Avrupa'daki herhangi bir da\u011f buzulundan \u00e7ok daha b\u00fcy\u00fckt\u00fcr. Langj\u00f6kull ve Hofsj\u00f6kull birlikte bile (&lt;2.000 km\u00b2) Vatnaj\u00f6kull&#039;un b\u00fcy\u00fckl\u00fc\u011f\u00fcn\u00fcn yaln\u0131zca yakla\u015f\u0131k &#039;idir. (Hacim a\u00e7\u0131s\u0131ndan fark daha da b\u00fcy\u00fckt\u00fcr.) K\u00fcresel \u00f6l\u00e7ekte Vatnaj\u00f6kull, Gr\u00f6nland (1,7 milyon km\u00b2) veya Antarktika buz tabakalar\u0131yla kar\u015f\u0131la\u015ft\u0131r\u0131ld\u0131\u011f\u0131nda k\u00fc\u00e7\u00fck say\u0131l\u0131r, ancak \u0130zlanda ve Avrupa&#039;n\u0131n devleri aras\u0131nda \u00e7o\u011funun \u00fczerinde y\u00fckselir \u2014 Rusya&#039;daki o istisnai \u00f6rnek hari\u00e7.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Vatnaj\u00f6kull hakk\u0131nda S\u0131k\u00e7a Sorulan Sorular<\/h2>\n\n\n\n<p><strong>S: Vatnaj\u00f6kull nedir?<\/strong><br>A: Vatnaj\u00f6kull, \u0130zlanda'n\u0131n g\u00fcneydo\u011fusundaki devasa buz \u00f6rt\u00fcs\u00fcd\u00fcr. Yakla\u015f\u0131k 8.100 km\u00b2'lik bir alan\u0131 kaplayan buzul, \u0130zlanda'n\u0131n en b\u00fcy\u00fck buzuludur ve (Arktik b\u00f6lgesi d\u0131\u015f\u0131nda) genellikle Avrupa'n\u0131n en b\u00fcy\u00fck buzulu olarak adland\u0131r\u0131l\u0131r. Bir\u00e7ok da\u011f ve volkan\u0131n tepesinde yer al\u0131r ve d\u00fczinelerce \u00e7\u0131k\u0131\u015f buzulunu besler. Ad\u0131 \u0130zlandaca'da \"sular\u0131n buzulu\" anlam\u0131na gelir.<\/p>\n\n\n\n<p><strong>S: Vatnaj\u00f6kull ger\u00e7ekten Avrupa'n\u0131n en b\u00fcy\u00fck buzulu mu?<\/strong><br>A: Genel kullan\u0131mda evet: Vatnaj\u00f6kull, Kuzey Kutbu d\u0131\u015f\u0131nda Avrupa'n\u0131n en b\u00fcy\u00fck buzuludur. Novaya Zemlya'n\u0131n Severny Adas\u0131 (Rusya) daha b\u00fcy\u00fck bir buz \u00f6rt\u00fcs\u00fcne (~20.500 km\u00b2) sahip ancak uzak Kuzey Kutbu'nda yer al\u0131yor. Bunu d\u0131\u015far\u0131da b\u0131rak\u0131rsak, Vatnaj\u00f6kull'\u00fcn ~8.100 km\u00b2'lik alan\u0131 onu k\u0131ta Avrupas\u0131'n\u0131n en b\u00fcy\u00fck buzulu yap\u0131yor.<\/p>\n\n\n\n<p><strong>S: J\u00f6kuls\u00e1rl\u00f3n nedir ve Elmas Plaj\u0131 nerede bulunur?<\/strong><br>A: J\u00f6kuls\u00e1rl\u00f3n, Vatnaj\u00f6kull'\u00fcn g\u00fcney kenar\u0131nda, Brei\u00f0amerkurj\u00f6kull \u00e7\u0131k\u0131\u015f\u0131n\u0131n geri \u00e7ekilmesiyle olu\u015fan b\u00fcy\u00fck bir buzul g\u00f6l\u00fcd\u00fcr. \u015eu anda yakla\u015f\u0131k 18 km\u00b2'lik bir alan\u0131 kaplamaktad\u0131r. Elmas Plaj\u0131, J\u00f6kuls\u00e1rl\u00f3n'un hemen yan\u0131nda bulunan siyah kumlu plajd\u0131r. Buzda\u011flar\u0131 g\u00f6lden denize do\u011fru s\u00fcr\u00fcklenir ve s\u0131kl\u0131kla Elmas Plaj\u0131'na vurarak koyu renkli kumda par\u0131ldar. Yaz aylar\u0131nda J\u00f6kuls\u00e1rl\u00f3n'da tekne turlar\u0131 d\u00fczenlenmekte ve buzda\u011flar\u0131n\u0131n yak\u0131ndan g\u00f6r\u00fclmesine olanak sa\u011flanmaktad\u0131r.<\/p>\n\n\n\n<p><strong>S: Turistler Vatnaj\u00f6kull'de y\u00fcr\u00fcyebilir mi?<\/strong><br>A: Sen <em>olabilmek<\/em> Buzulun \u00fczerinde y\u00fcr\u00fcy\u00fcn, ama <strong>sadece rehberli tur ve uygun ekipmanla<\/strong>Gizli yar\u0131klar ve ani hava de\u011fi\u015fiklikleri nedeniyle buz \u00fczerinde ba\u011f\u0131ms\u0131z seyahat yasakt\u0131r. Rehberli buzul y\u00fcr\u00fcy\u00fc\u015fleri (krampon ve iplerle) Skaftafell, J\u00f6kuls\u00e1rl\u00f3n veya H\u00f6fn'den ba\u015flar ve birka\u00e7 saatten tam g\u00fcnlere kadar s\u00fcrebilir. K\u0131sa buzul y\u00fcr\u00fcy\u00fc\u015fleri bile g\u00fcvenlik i\u00e7in sertifikal\u0131 bir rehber gerektirir.<\/p>\n\n\n\n<p><strong>S: Vatnaj\u00f6kull'deki buz ma\u011faralar\u0131 do\u011fal m\u0131 ve ne zaman ziyaret edebilirim?<\/strong><br>A: Muhte\u015fem mavi buz ma\u011faralar\u0131 her k\u0131\u015f eriyen buz sular\u0131 taraf\u0131ndan do\u011fal olarak olu\u015fturulur. So\u011fuk hava ve eriyen buz sular\u0131 buzulun alt\u0131nda t\u00fcneller a\u00e7t\u0131\u011f\u0131 i\u00e7in, bu ma\u011faralar yakla\u015f\u0131k olarak Kas\u0131m-Mart aylar\u0131 aras\u0131nda varl\u0131\u011f\u0131n\u0131 s\u00fcrd\u00fcr\u00fcr. \u0130lkbahar sonu\/yaz ba\u015f\u0131nda ise \u00e7\u00f6kerler. Bu nedenle, rehberli buz ma\u011faras\u0131 turlar\u0131 \u00e7o\u011funlukla k\u0131\u015f aylar\u0131nda d\u00fczenlenir. Ma\u011faralar\u0131n yerleri her y\u0131l de\u011fi\u015fir; her zaman kask ve kafa lambas\u0131 takan deneyimli bir rehberle gidin.<\/p>\n\n\n\n<p><strong>S: Vatnaj\u00f6kull'\u00fc ziyaret etmek i\u00e7in en uygun zaman ne zaman?<\/strong><br>A: \u0130lgi alanlar\u0131n\u0131za ba\u011fl\u0131. Y\u00fcr\u00fcy\u00fc\u015f ve \u0131l\u0131man hava i\u00e7in en uygun d\u00f6nem ge\u00e7 ilkbahardan erken sonbahara (May\u0131s-Eyl\u00fcl) kadard\u0131r: yollar a\u00e7\u0131kt\u0131r ve \u00e7o\u011fu aktivite devam eder. Buz ma\u011faralar\u0131 ve k\u0131\u015f manzaralar\u0131 i\u00e7in Aral\u0131k-\u015eubat aylar\u0131 karl\u0131 manzaralar ve Kuzey I\u015f\u0131klar\u0131 sunar (ancak g\u00fcn \u0131\u015f\u0131\u011f\u0131 k\u0131sad\u0131r). J\u00f6kuls\u00e1rl\u00f3n'da tekne turlar\u0131 yaz aylar\u0131nda d\u00fczenlenir. Ara mevsimler (Nisan veya Eyl\u00fcl) daha az kalabal\u0131k ve \u0131l\u0131man hava anlam\u0131na gelir.<\/p>\n\n\n\n<p><strong>S: Vatnaj\u00f6kull, Reykjav\u00edk'e ne kadar uzakl\u0131kta ve oraya arabayla gidilebilir mi?<\/strong><br>A: Vatnaj\u00f6kull'\u00fcn kenar\u0131, Reykjav\u00edk'ten \u00c7evre Yolu \u00fczerinden yakla\u015f\u0131k 330 km uzakl\u0131ktad\u0131r. Yolculuk (molalar dahil) yakla\u015f\u0131k 4-6 saat s\u00fcrer. \u00c7evre Yolu, g\u00fcney buzul kenar\u0131 boyunca tamamen asfaltlanm\u0131\u015ft\u0131r. Yaz aylar\u0131nda yollar iyi bak\u0131ml\u0131d\u0131r. K\u0131\u015f\u0131n, yo\u011fun kar ya\u011f\u0131\u015f\u0131 nedeniyle baz\u0131 b\u00f6l\u00fcmler k\u0131sa s\u00fcreli\u011fine kapanabilir, bu nedenle her zaman g\u00fcncel yol ko\u015fullar\u0131n\u0131 kontrol edin (bkz. <em>yol.d\u0131r<\/em>) seyahat etmeden \u00f6nce.<\/p>\n\n\n\n<p><strong>S: Vatnaj\u00f6kull'de veya yak\u0131nlar\u0131nda vah\u015fi ya\u015fam var m\u0131?<\/strong><br>A: Evet, \u00f6zellikle k\u0131y\u0131 ve al\u00e7ak rak\u0131ml\u0131 b\u00f6lgelerde. Kutup tilkileri y\u00fcksek b\u00f6lgelerde dola\u015f\u0131yor. J\u00f6kuls\u00e1rl\u00f3n ve Diamond Beach'te, liman foklar\u0131 s\u0131k s\u0131k buz k\u00fctlelerinin \u00fczerinde g\u00fcne\u015flenir ve eider \u00f6rdekleri, sumrular, kutup skualar\u0131 ve mart\u0131lar\u0131 g\u00f6rebilirsiniz. Akdo\u011fan veya alt\u0131n kartal gibi y\u0131rt\u0131c\u0131 ku\u015flar bazen yak\u0131ndaki vadilerde avlan\u0131r. K\u0131\u015f\u0131n park\u0131n eteklerinde ren geyikleri g\u00f6rebilirsiniz. Ancak, b\u00fcy\u00fck kara hayvanlar\u0131 ya\u015fam\u0131yor. <em>A\u00e7\u0131k<\/em> Buzun kendisi.<\/p>","protected":false},"excerpt":{"rendered":"<p>For millennia, adventurers, scientists, and environmentalists have been enthralled by Europe&#8217;s biggest glacier, Vatnajokull, a magnificent natural wonder. Covering 8,101 square kilometers, it is proof of the unvarnished force and beauty of earthly geological events. Large sheets of ice accumulating in the region marked the start of the story of the glacier 2.5 million years ago Its surface, covered in ice formations with sharp edges and seracs reaching heavens, is always changing masterpiece.<\/p>","protected":false},"author":1,"featured_media":2935,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_eb_attr":"","footnotes":""},"categories":[19,5],"tags":[],"class_list":{"0":"post-1285","1":"post","2":"type-post","3":"status-publish","4":"format-standard","5":"has-post-thumbnail","7":"category-unusual-places","8":"category-magazine"},"_links":{"self":[{"href":"https:\/\/travelshelper.com\/tr\/wp-json\/wp\/v2\/posts\/1285","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/travelshelper.com\/tr\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/travelshelper.com\/tr\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/travelshelper.com\/tr\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/travelshelper.com\/tr\/wp-json\/wp\/v2\/comments?post=1285"}],"version-history":[{"count":0,"href":"https:\/\/travelshelper.com\/tr\/wp-json\/wp\/v2\/posts\/1285\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/travelshelper.com\/tr\/wp-json\/wp\/v2\/media\/2935"}],"wp:attachment":[{"href":"https:\/\/travelshelper.com\/tr\/wp-json\/wp\/v2\/media?parent=1285"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/travelshelper.com\/tr\/wp-json\/wp\/v2\/categories?post=1285"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/travelshelper.com\/tr\/wp-json\/wp\/v2\/tags?post=1285"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}