Yerkabu\u011funu olu\u015fturan 3 temel kaya\u00e7 t\u00fcr\u00fc vard\u0131r.Bunlar;magmatik kaya\u00e7lar,tortul kaya\u00e7lar ve ba\u015fkala\u015f\u0131m kaya\u00e7lar\u0131d\u0131r.Ancak bunlar,olu\u015ftuklar\u0131 g\u00fcnden bug\u00fcne kadar ge\u00e7en zamanda bir\u00e7ok de\u011fi\u015fikli\u011fe u\u011fram\u0131\u015flard\u0131r. Yani her ne kadar bulunduklar\u0131 yerde hi\u00e7 hareket etmeden dursalar da, her biri \u00e7ok uzun y\u0131llard\u0131r s\u00fcren bir de\u011fi\u015fikli\u011fin par\u00e7as\u0131d\u0131rlar. Kya\u00e7lar\u0131n olu\u015ftuklar\u0131 g\u00fcnden bu yana devam eden ve farkl\u0131 t\u00fcr kaya\u00e7lar\u0131n do\u011fal yollarla birbirine d\u00f6n\u00fc\u015fmesini a\u00e7\u0131klayan bu s\u00fcrece “kaya d\u00f6ng\u00fcs\u00fc” denir. Kaya d\u00f6ng\u00fcs\u00fcn\u00fc devam ettiren \u015fey ise do\u011fal olaylard\u0131r.\u015eimdi gelelim bu ser\u00fcvenin nas\u0131l ba\u015flay\u0131p ne \u015fekilde devam etti\u011fine:
\n Yeralt\u0131ndaki magman\u0131n so\u011fumas\u0131yla olu\u015fan magmatik bir kaya\u00e7tan ba\u015flayal\u0131m. Bu kayac\u0131n yerkabu\u011fundaki tektonik hareketler sonucu yery\u00fcz\u00fcne \u00e7\u0131kt\u0131\u011f\u0131n\u0131 d\u00fc\u015f\u00fcnelim. Y\u00fczeye \u00e7\u0131kan bu kaya\u00e7 art\u0131k burada olu\u015fan t\u00fcm ko\u015fullardan etkilenebilecek durumdad\u0131r. Bu etkile\u015fim olduk\u00e7a de\u011fi\u015fik yollarla olu\u015fabilir. Erozyon, ya\u011fmur suyu ve r\u00fczgar bunlardan birka\u00e7\u0131d\u0131r. Bu olaylar\u0131n sonucunda kaya\u00e7, fiziksel ve kimyasal olarak de\u011fi\u015fime u\u011frar ve ta\u015f\u0131nma sonucu bir yerde \u00e7\u00f6kelir. Farkl\u0131 yerlerden gelen t\u00fcm \u00e7\u00f6keller, yeni gelen \u00e7\u00f6kellerin de etkisiyle s\u0131k\u0131\u015farak zamanla kendi i\u00e7inde kayna\u015farak ta\u015fla\u015f\u0131r. Ve b\u00f6ylelikle tortul kayac\u0131m\u0131z olu\u015fur.Olu\u015fan bu yeni kayac\u0131m\u0131z\u0131n \u00fczerine uzun bir s\u00fcre daha yeni \u00e7\u00f6kelimlerin devam edece\u011fini d\u00fc\u015f\u00fcnelim. Zamanla \u00fcst\u00fcndeki malzeme birikece\u011fi i\u00e7in kayac\u0131m\u0131z bas\u0131nca ve s\u0131cakl\u0131\u011fa daha fazla maruz kalacak demektir. Bu da tortul kayac\u0131m\u0131z\u0131n yap\u0131s\u0131nda \u00e7ok daha farkl\u0131 de\u011fi\u015fimlere yol a\u00e7acakt\u0131r. Bas\u0131nc\u0131n ve s\u0131cakl\u0131\u011f\u0131n belli bir d\u00fczeye gelmesi sonucu olu\u015fan yeni kayac\u0131m\u0131z art\u0131k bir ba\u015fkala\u015f\u0131m kayac\u0131d\u0131r. Olduk\u00e7a y\u00fcksek bir s\u0131cakl\u0131\u011fa maruz kal\u0131rsa ba\u015fkala\u015f\u0131m kayac\u0131m\u0131z\u0131n da de\u011fi\u015fimi ka\u00e7\u0131n\u0131lmazd\u0131r. Ve bu s\u0131cakl\u0131\u011fa dayanamayan kayac\u0131m\u0131z sonunda eriyerek magmatik kayaca d\u00f6n\u00fc\u015f\u00fcr. B\u00f6ylece d\u00f6ng\u00fcm\u00fcz\u00fcn ba\u015flad\u0131\u011f\u0131 yere yani tekrar magmatik kaya\u00e7lara gelmi\u015f oluyoruz. Her ne kadar burada magmatik kaya\u00e7tan ba\u015flad\u0131ysak da ayn\u0131 \u015fekilde tortul vaya ba\u015fkala\u015f\u0131m kaya\u00e7tan da ba\u015flayabiliriz bu d\u00f6ng\u00fcye.<\/p>\n","protected":false},"excerpt":{"rendered":"
Yerkabu\u011funu olu\u015fturan 3 temel kaya\u00e7 t\u00fcr\u00fc vard\u0131r.Bunlar;magmatik kaya\u00e7lar,tortul kaya\u00e7lar ve ba\u015fkala\u015f\u0131m kaya\u00e7lar\u0131d\u0131r.Ancak bunlar,olu\u015ftuklar\u0131 g\u00fcnden bug\u00fcne kadar ge\u00e7en zamanda bir\u00e7ok de\u011fi\u015fikli\u011fe u\u011fram\u0131\u015flard\u0131r. Yani her ne kadar bulunduklar\u0131 yerde hi\u00e7 hareket etmeden dursalar da, her biri \u00e7ok uzun y\u0131llard\u0131r s\u00fcren bir de\u011fi\u015fikli\u011fin par\u00e7as\u0131d\u0131rlar. Kya\u00e7lar\u0131n olu\u015ftuklar\u0131 g\u00fcnden bu yana devam eden ve farkl\u0131 t\u00fcr kaya\u00e7lar\u0131n do\u011fal yollarla birbirine …<\/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":[3847,4179,2963],"class_list":["post-1474","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-erozyon","tag-kayac-dongusu","tag-yerkabugu"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/1474","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=1474"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/1474\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=1474"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=1474"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=1474"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}