1. \u0130lk Zaman (Prekambrien)
\nEn eski k\u0131vr\u0131mlarla k\u0131talar\u0131n \u00e7ekirdek k\u0131s\u0131mlar\u0131 olu\u015fmu\u015ftur. Zaman\u0131n sonlar\u0131nda da bakteriler ve algler gibi tek h\u00fccreli canl\u0131lar ortaya \u00e7\u0131km\u0131\u015ft\u0131r.
\n2. Birinci Zaman (Paleozoik)
\nD\u00fcnya\u2019n\u0131n muhtelif b\u00f6lgelerinde \u015fiddetli k\u0131vr\u0131mlar olmu\u015f, k\u0131talar bu k\u0131vr\u0131mlar\u0131n eklenmesiyle b\u00fcy\u00fcm\u00fc\u015ft\u00fcr. T\u00fcrkiye\u2019de ve daha bir\u00e7ok \u00fclkede, ta\u015fk\u00f6m\u00fcr\u00fc yataklar\u0131 meydana gelmi\u015ftir.
\n3. \u0130kinci Zaman (Mezozoik)
\nJeosenklinallerde b\u00fcy\u00fck \u00f6l\u00e7\u00fcde tortula\u015fma ve birikmeler olu\u015fmu\u015ftur. Bu d\u00f6nem, Alp k\u0131vr\u0131mlar\u0131na haz\u0131rl\u0131k d\u00f6nemidir. Bu zamanda, yerkabu\u011fu k\u0131r\u0131klarla par\u00e7alanarak ayr\u0131 k\u0131talara b\u00f6l\u00fcnmeye ba\u015flam\u0131\u015f, deniz ilerlemesi sonucu karalar denizlerin alt\u0131nda kalm\u0131\u015ft\u0131r.
\n4. \u00dc\u00e7\u00fcnc\u00fc Zaman (Neozoik)
\nD\u00fcnya\u2019da ve T\u00fcrkiye\u2019de \u015fiddetli yerkabu\u011fu hareketleri olmu\u015ftur. Alp k\u0131vr\u0131mlar\u0131 olu\u015fmu\u015f ve eski k\u0131ta k\u00fctlelerine eklenmi\u015ftir. K\u0131talar g\u00fcn\u00fcm\u00fczdeki g\u00f6r\u00fcn\u00fcmlerini kazanm\u0131\u015flard\u0131r. \u015eiddetli volkanik olaylar ve depremler meydana gelmi\u015ftir.
\nAtlas ve Hint okyanuslar\u0131 ile T\u00fcrkiye\u2019nin ana yer\u015fekilleri olu\u015fmu\u015ftur. Linyit, petrol, tuz ve boraksit yataklar\u0131n\u0131n olu\u015fumu da bu d\u00f6nemlerdedir.
\n5. D\u00f6rd\u00fcnc\u00fc Zaman (Antropozoik)
\nBuzul\u00e7a\u011f\u0131 (Pleistosen): \u015eiddetli so\u011fuma olmu\u015ftur. Bu nedenle Kuzeybat\u0131 Avrupa, \u0130skandinavya, Kanada gibi karalar, buzullar alt\u0131nda kalm\u0131\u015ft\u0131r. Ege Denizi ile \u0130stanbul ve \u00c7anakkale bo\u011fazlar\u0131 bu d\u00f6nemde te\u015fekk\u00fcl etmi\u015ftir. \u0130nsan\u0131n varl\u0131\u011f\u0131 ve ilk prehistorik (tarih \u00f6ncesi) k\u00fclt\u00fcrler bu d\u00f6nemde g\u00f6r\u00fclm\u00fc\u015ft\u00fcr.
\nBuzul\u00e7a\u011f\u0131 sonras\u0131 (Postglasyal): \u0130klim gittik\u00e7e \u0131s\u0131narak bug\u00fcnk\u00fc \u015fartlara ge\u00e7mi\u015ftir. \u015eimdiki deniz seviyesine eri\u015filmi\u015f, \u0130ngiltere Avrupa\u2019dan koparak bir ada durumuna gelmi\u015ftir. Avrupa k\u0131tas\u0131 bug\u00fcnk\u00fc \u015feklini kazanm\u0131\u015ft\u0131r. Eski uygarl\u0131klar ortaya \u00e7\u0131karak geli\u015fmi\u015ftir.
\nBu d\u00f6nem ikiye ayr\u0131l\u0131r:
\nBUZUL \u00c7A\u011eI:
\n2.5 milyon y\u0131l s\u00fcrm\u00fc\u015ft\u00fcr.
\n\u0130nsanlar bu devirde yarat\u0131lm\u0131\u015flard\u0131r.
\n\u015eiddetli so\u011fumalarla birlikte , K,Y,K de buzulla\u015fma artm\u0131\u015ft\u0131r.
\nDeniz ve kara seviyesinde de\u011fi\u015fmeler g\u00f6r\u00fclm\u00fc\u015ft\u00fcr.
\n\u0130stanbul ve \u00c7anakkale bo\u011fazlar\u0131 olu\u015fmu\u015ftur.
\nBUZUL \u00c7A\u011eI SONRASI:
\n10 bin y\u0131l s\u00fcrm\u00fc\u015ft\u00fcr.
\nBug\u00fcnk\u00fc iklim ko\u015fullar\u0131 olu\u015fmu\u015ftur.
\nBuzullar\u0131n etki alanlar\u0131 daralm\u0131\u015ft\u0131r.
\nHayvanlar evcille\u015ftirilmi\u015f ve k\u00fclt\u00fcr bitkileri ortaya \u00e7\u0131km\u0131\u015ft\u0131r.<\/p>\n","protected":false},"excerpt":{"rendered":"
1. \u0130lk Zaman (Prekambrien) En eski k\u0131vr\u0131mlarla k\u0131talar\u0131n \u00e7ekirdek k\u0131s\u0131mlar\u0131 olu\u015fmu\u015ftur. Zaman\u0131n sonlar\u0131nda da bakteriler ve algler gibi tek h\u00fccreli canl\u0131lar ortaya \u00e7\u0131km\u0131\u015ft\u0131r. 2. Birinci Zaman (Paleozoik) D\u00fcnya\u2019n\u0131n muhtelif b\u00f6lgelerinde \u015fiddetli k\u0131vr\u0131mlar olmu\u015f, k\u0131talar bu k\u0131vr\u0131mlar\u0131n eklenmesiyle b\u00fcy\u00fcm\u00fc\u015ft\u00fcr. T\u00fcrkiye\u2019de ve daha bir\u00e7ok \u00fclkede, ta\u015fk\u00f6m\u00fcr\u00fc yataklar\u0131 meydana gelmi\u015ftir. 3. \u0130kinci Zaman (Mezozoik) Jeosenklinallerde b\u00fcy\u00fck \u00f6l\u00e7\u00fcde tortula\u015fma …<\/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":[11050,2862,4076,4077,4075,11049],"class_list":["post-5357","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-antropozoik","tag-jeolojik-zamanlar","tag-mezozoik","tag-neozoik","tag-paleozoik","tag-prekambrien"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/5357","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=5357"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/5357\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=5357"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=5357"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=5357"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}