G\u00d6LLER VE OLU\u015eUMLARI
\n1. Yerli Kaya G\u00f6lleri
\na. Yerli Kaya G\u00f6lleri: Yer kabu\u011funun \u00e7\u00f6kmesi veya k\u0131r\u0131lmas\u0131 neticesinde meydana gelen \u00e7ukurluklara sular\u0131n dolmas\u0131yla olu\u015furlar. D\u00fcnya\u2019n\u0131n en derin g\u00f6l\u00fc olan Baykal G\u00f6l\u00fc (1741 m), L\u00fbt G\u00f6l\u00fc, Hazar G\u00f6l\u00fc ve \u00c7ad G\u00f6l\u00fc yery\u00fcz\u00fcndeki ba\u015fl\u0131ca b\u00fcy\u00fck tektonik g\u00f6llerdir.
\n\u00dclkemizdeki ba\u015fl\u0131ca tektonik g\u00f6ller ise \u015funlard\u0131r:
\n\u2022 Marmara B\u00f6lgesi\u2019nde; Sapanca, \u0130znik, Ulubat ve Manyas g\u00f6lleri,
\n\u2022Ege B\u00f6lgesi\u2019nde; Simav G\u00f6l\u00fc,
\n\u2022G\u00f6ller Y\u00f6resi\u2019nde; Bey\u015fehir, E\u011firdir, Ac\u0131g\u00f6l, Burdur, Ilg\u0131n (\u00c7avu\u015f\u00e7u), Ak\u015fehir, Eber, Su\u011fla ve Kovada g\u00f6lleri,
\n\u2022\u0130\u00e7 Anadolu B\u00f6lgesi\u2019nde; Tuz, Seyfe ve Tuzla g\u00f6lleri,
\n\u2022Do\u011fu Anadolu B\u00f6lgesi\u2019nde Hazar, Hozapin ve Van g\u00f6lleri.
\nT\u00fcrkiye\u2019nin en b\u00fcy\u00fck tabii g\u00f6l\u00fc olan Van G\u00f6l\u00fc, tektonik bir \u00e7ukurlu\u011fun \u00f6n\u00fcn\u00fcn lavlarla kesilmesi sonucu olu\u015ftu\u011fundan volkanik set g\u00f6l\u00fc olarak da bilinir.
\nb. Karstik G\u00f6ller: Bu t\u00fcr g\u00f6ller, kayatuzu, jips, kalker gibi \u00e7\u00f6z\u00fcnebilen tabakalar\u0131n bulundu\u011fu sahalarda meydana gelir. Baz\u0131 karstik g\u00f6llerin olu\u015fumunda tektonik olaylar da etkili olmu\u015ftur.
\nKarstik g\u00f6ller, \u00fclkemizde en fazla Toros Da\u011flar\u0131\u2019n\u0131n bat\u0131 kesiminde bulunur. Buralarda yer alan K\u0131z\u0131l\u00f6ren obruk g\u00f6l\u00fc, Kestel, Avlan, Yar\u0131\u015fl\u0131 ve Salda g\u00f6lleri tipik birer karstik g\u00f6ld\u00fcr. Bu g\u00f6llerimiz sadece, kire\u00e7ta\u015flar\u0131n\u0131n \u00e7\u00f6z\u00fclmesiyle olu\u015fan \u00e7anaklar \u00fczerinde meydana gelmi\u015flerdir.
\nBununla birlikte, bu alandaki baz\u0131 g\u00f6llerimizin ise olu\u015fumu, tektonik \u00e7anaklarda ba\u015flam\u0131\u015f, karstik olaylarla devam etmi\u015ftir. Bu g\u00f6llerimizin ba\u015fl\u0131calar\u0131, Bey\u015fehir, E\u011firdir, Burdur, Ac\u0131g\u00f6l, Kovada ve Su\u011fla g\u00f6lleridir.
\nc. Volkanik G\u00f6ller: Volkanik faaliyetler esnas\u0131nda olu\u015fan patlama \u00e7ukurlar\u0131 i\u00e7erisinde meydana gelen g\u00f6llerdir. Ba\u015fl\u0131ca volkanik g\u00f6llerimiz, Meke G\u00f6l\u00fc, Ac\u0131g\u00f6l, Nemrut ve G\u00f6lc\u00fck g\u00f6lleri ile S\u00fcphan Da\u011f\u0131\u2019n\u0131n yan kraterlerinden birinde bulunan Ayg\u0131r G\u00f6l\u00fc\u2019d\u00fcr.
\nd. Buzul (Sirk) G\u00f6lleri: Da\u011f doruklar\u0131nda, buzullar\u0131n a\u015f\u0131nd\u0131rmas\u0131yla olu\u015fan ve sirk ad\u0131 verilen \u00e7ukurluklarda meydana gelirler. \u00dclkemizde Sat, A\u011fr\u0131, Erciyes, Ka\u00e7kar ve Bolkar da\u011flar\u0131 ile Alada\u011flar \u00fczerinde yer yer bu t\u00fcrden g\u00f6ller bulunmaktad\u0131r.
\n2. Set G\u00f6lleri
\na. Al\u00fcvyal Set G\u00f6lleri: Al\u00fcvyonlarla akarsuyun \u00f6n\u00fcn\u00fcn kapanmas\u0131 sonucu olu\u015fur. \u00dclkemizde, Marmara, \u00c7ami\u00e7i (Bafa), K\u00f6yce\u011fiz, Mogan ve Eymir G\u00f6lleri ile Uzung\u00f6l bu t\u00fcr g\u00f6llerdendir.
\nb. K\u0131y\u0131 Set G\u00f6lleri: Dalga ve ak\u0131nt\u0131lar\u0131n ta\u015f\u0131d\u0131\u011f\u0131 malzemeleri koy ve k\u00f6rfezlerin a\u011f\u0131z k\u0131sm\u0131nda biriktirmesiyle olu\u015fur. \u00dclkemizde, B\u00fcy\u00fck ve K\u00fc\u00e7\u00fck \u00c7ekmece g\u00f6lleri, Durusu (Terkos) g\u00f6l\u00fc, \u00c7ukurova deltas\u0131ndaki Akyatan g\u00f6l\u00fc k\u0131y\u0131 set g\u00f6lleridir.
\nc. Heyelan Set G\u00f6lleri: Heyelan sonucu bir akarsuyun \u00f6n\u00fcn\u00fcn kapanmas\u0131yla olu\u015fur. Tortum, Sera, Abant, Zinav ve S\u00fcl\u00fck g\u00f6lleri ile Yedig\u00f6ller bu t\u00fcr g\u00f6llerdendir.
\nAbant G\u00f6l\u00fc\u2019n\u00fcn olu\u015fumunda tektonik hareketler ile al\u00fcvyal birikimlerin de etkisi olu\u015fmu\u015ftur.
\nd. Volkanik Set G\u00f6lleri: Volkanizma sonucu vadi \u00f6nlerinin kapanmas\u0131yla meydana gelir. Van, Er\u00e7ek, Nazik, \u00c7\u0131ld\u0131r, Ha\u00e7l\u0131 ve Bal\u0131k g\u00f6lleri \u00fclkemizdeki volkanik set g\u00f6lleridir.
\ne. Baraj (Yapay) G\u00f6lleri: Yapay g\u00f6llerimizin en b\u00fcy\u00fckleri, Atat\u00fcrk, Keban, Karakaya ve Hirfanl\u0131 barajlar\u0131n\u0131n gerisinde kurulan g\u00f6llerdir.<\/p>\n","protected":false},"excerpt":{"rendered":"
G\u00d6LLER VE OLU\u015eUMLARI 1. Yerli Kaya G\u00f6lleri a. Yerli Kaya G\u00f6lleri: Yer kabu\u011funun \u00e7\u00f6kmesi veya k\u0131r\u0131lmas\u0131 neticesinde meydana gelen \u00e7ukurluklara sular\u0131n dolmas\u0131yla olu\u015furlar. D\u00fcnya\u2019n\u0131n en derin g\u00f6l\u00fc olan Baykal G\u00f6l\u00fc (1741 m), L\u00fbt G\u00f6l\u00fc, Hazar G\u00f6l\u00fc ve \u00c7ad G\u00f6l\u00fc yery\u00fcz\u00fcndeki ba\u015fl\u0131ca b\u00fcy\u00fck tektonik g\u00f6llerdir. \u00dclkemizdeki ba\u015fl\u0131ca tektonik g\u00f6ller ise \u015funlard\u0131r: \u2022 Marmara B\u00f6lgesi\u2019nde; Sapanca, \u0130znik, …<\/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":[3244,3248,3242,3246,3241,3243,3237,3240,3250,3249,3239,3247,3245,3251,3238],"class_list":["post-1099","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-acigol","tag-aluvyal-set-golleri","tag-beysehir","tag-buzul-sirk-golleri","tag-cad-golu","tag-egirdir","tag-goller-ve-olusumlari","tag-hazar-golu","tag-heyelan-set-golleri","tag-kiyi-set-golleri","tag-lut-golu","tag-set-golleri","tag-volkanik-goller","tag-volkanik-set-golleri","tag-yerli-kaya-golleri"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/1099","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=1099"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/1099\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=1099"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=1099"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=1099"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}