{"id":1101,"date":"2011-06-09T09:53:46","date_gmt":"2011-06-09T06:53:46","guid":{"rendered":"http:\/\/www.islamidavet.com\/kutuphane\/\/?p=1101"},"modified":"2011-06-09T09:53:46","modified_gmt":"2011-06-09T06:53:46","slug":"buzullar-ve-olusturdugu-sekiller","status":"publish","type":"post","link":"https:\/\/www.islamidavet.com\/kutuphane\/buzullar-ve-olusturdugu-sekiller\/","title":{"rendered":"Buzullar ve olu\u015fturdu\u011fu \u015fekiller"},"content":{"rendered":"<p>BUZULLAR VE BUZULLARIN OLU\u015eTURDU\u011eU \u015eEK\u0130LLER<br \/>\nKutuplarda ve y\u00fcksek da\u011flar \u00fczerinde ya\u011f\u0131\u015flar genellikle kar halinde olur. S\u0131cakl\u0131k \u00e7ok d\u00fc\u015f\u00fck oldu\u011fu i\u00e7in ya\u011fan karlar erimeden \u00fcst \u00fcste birikir. Biriken bu karlara tokta\u011fan (kal\u0131c\u0131) kar denir. Yaz ve k\u0131\u015f karla \u00f6rt\u00fcl\u00fc olan b\u00f6yle yerlerin alt k\u0131s\u0131mlar\u0131na ise, tokta\u011fan (kal\u0131c\u0131) kar s\u0131n\u0131r\u0131 ad\u0131 verilir.<\/p>\n<p>T\u00fcrkiye\u2019de IV. Jeolojik zamanda buzulla\u015fmaya u\u011frayan sahalar<br \/>\nKar \u00f6rt\u00fcs\u00fc ba\u015flang\u0131\u00e7ta yumu\u015fak ve gev\u015fektir. Ancak, daha sonra so\u011fu\u011fun etkisi ve ya\u011fan karlar\u0131n s\u0131k\u0131\u015ft\u0131rmas\u0131 ile sertle\u015fir. Buna buzkar denir. Buzkarlar, daha sonra \u00fcst\u00fcste ya\u011fan karlar\u0131n bas\u0131nc\u0131 ile iyice kat\u0131la\u015f\u0131r ve buzul haline gelir.<br \/>\nBinlerce km2 lik sahalar\u0131 geni\u015f ve kal\u0131n bir \u00f6rt\u00fc gibi kaplayan buzullara \u00f6rt\u00fc buzulu, da\u011flar\u0131n zirvelerinde olu\u015fan buzullara da da\u011f buzulu denilmektedir. \u00dclkemizdeki buzullar da\u011f buzulu \u015feklinde olu\u015fmu\u015flard\u0131r.<br \/>\nT\u00fcrkiye\u2019deki buzul d\u00f6nemi, d\u00f6rd\u00fcnc\u00fc jeolojik zamanda, D\u00fcnya\u2019daki iklim de\u011fi\u015fmelerine ba\u011fl\u0131 olarak ba\u015flam\u0131\u015ft\u0131r. Bu devirde \u00f6zellikle \u00fclkemizin y\u00fcksek yerleri buzulla\u015fma olaylar\u0131ndan etkilenmi\u015ftir. Bundan dolay\u0131, 2200 m. den daha y\u00fcksek olan da\u011flar\u0131m\u0131z buzullarla kaplanm\u0131\u015ft\u0131r.<br \/>\nBuzullar\u0131n A\u015f\u0131nd\u0131rma \u015eekilleri<br \/>\nBuzul Vadisi: Buz \u00f6rt\u00fcleri alt\u0131nda kalm\u0131\u015f olan b\u00f6lgelerde, buzun yata\u011f\u0131n\u0131 a\u015f\u0131nd\u0131r\u0131p derinle\u015ftirmesi sonucunda olu\u015fan \u201cU\u201d \u015feklindeki vadilerdir.<br \/>\nH\u00f6rg\u00fc\u00e7 kaya: Anakayan\u0131n buzullar taraf\u0131ndan i\u015flenmesi sonucunda olu\u015fan kaya tepeleridir.<br \/>\nSirk \u00c7ana\u011f\u0131 (Buz Yala\u011f\u0131): Da\u011f yama\u00e7lar\u0131ndaki baz\u0131 buzullar\u0131n, bulunduklar\u0131 alan\u0131 a\u015f\u0131nd\u0131rmas\u0131yla olu\u015fan \u00e7anaklard\u0131r. Buzullar bazen eriyince bu \u00e7anaklar sularla dolarak sirk g\u00f6llerini meydana getirirler.<br \/>\nT\u00fcrkiye\u2019de, buzullar\u0131n a\u015f\u0131nd\u0131rma \u015fekilleri, en \u00e7ok a\u015fa\u011f\u0131daki da\u011flar\u0131m\u0131zda g\u00f6r\u00fcl\u00fcr:<br \/>\n\u2022 Toroslar\u2019da, Bey Da\u011flar\u0131, Sultan Da\u011flar\u0131, Bolkar Da\u011flar\u0131 ve Alada\u011flar<br \/>\n\u2022 G\u00f6ller Y\u00f6resi\u2019nde, Davras ve Dedeg\u00f6l Da\u011flar\u0131<br \/>\n\u2022 Do\u011fu Anadolu B\u00f6lgesi\u2019nde, Mescit, Yaln\u0131z\u00e7am, Bing\u00f6l, Buzul, S\u00fcphan, Sat ve A\u011fr\u0131 Da\u011flar\u0131<br \/>\n\u2022 \u0130\u00e7 Anadolu B\u00f6lgesi\u2019nde, Erciyes Da\u011f\u0131<br \/>\n\u2022 Marmara B\u00f6lgesi\u2019nde, Uluda\u011f<br \/>\n\u2022 Karadeniz B\u00f6lgesi\u2019nde, Ka\u00e7kar ve Giresun Da\u011flar\u0131<br \/>\nBuzullar\u0131n Biriktirme \u015eekilleri<br \/>\nMoren (Buzulta\u015f): Buzullar\u0131n a\u015f\u0131nd\u0131rd\u0131klar\u0131 malzemeleri biriktirmesiyle olu\u015furlar. Ortalama kal\u0131nl\u0131klar\u0131 50 &#8211; 60 m kadard\u0131r.<br \/>\nDrumlin: Buzullar\u0131n ta\u015f\u0131y\u0131p biriktirdi\u011fi materyallerin, buzulun alt k\u0131sm\u0131ndaki erimeler sonucu meydana gelen dereler taraf\u0131ndan i\u015flenmesiyle olu\u015fan birikintilerdir.<br \/>\nSander Ovas\u0131: Eriyerek \u00e7ekilen buzul sular\u0131n\u0131n olu\u015fturdu\u011fu d\u00fczl\u00fcklerdir.<br \/>\n\u00dclkemizde, buzul birikim \u015fekillerinden sadece morenler bulunur. Ancak, bunlar da pek yayg\u0131n de\u011fildir. \u00c7\u00fcnk\u00fc, morenlerin b\u00fcy\u00fck bir k\u0131sm\u0131 akarsular taraf\u0131ndan ta\u015f\u0131nm\u0131\u015ft\u0131r.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>BUZULLAR VE BUZULLARIN OLU\u015eTURDU\u011eU \u015eEK\u0130LLER Kutuplarda ve y\u00fcksek da\u011flar \u00fczerinde ya\u011f\u0131\u015flar genellikle kar halinde olur. S\u0131cakl\u0131k \u00e7ok d\u00fc\u015f\u00fck oldu\u011fu i\u00e7in ya\u011fan karlar erimeden \u00fcst \u00fcste birikir. Biriken bu karlara tokta\u011fan (kal\u0131c\u0131) kar denir. Yaz ve k\u0131\u015f karla \u00f6rt\u00fcl\u00fc olan b\u00f6yle yerlerin alt k\u0131s\u0131mlar\u0131na ise, tokta\u011fan (kal\u0131c\u0131) kar s\u0131n\u0131r\u0131 ad\u0131 verilir. T\u00fcrkiye\u2019de IV. Jeolojik zamanda buzulla\u015fmaya &hellip;<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1403,1406],"tags":[3254,3252,3257,3255,3253,3256],"class_list":["post-1101","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-buzul-vadisi","tag-buzullar-ve-olusturdugu-sekiller","tag-buzultas","tag-horguc-kaya","tag-jeolojik-zaman","tag-sirk-canagi"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/1101","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/comments?post=1101"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/1101\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=1101"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=1101"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=1101"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}