Ovalar\u0131n tan\u0131m\u0131 ve yap\u0131sal \u00f6zellikleri<\/p>\n
Akarsularla fazla yar\u0131lmam\u0131\u015f,d\u00fcz ya da hafif egimli \u00e7ukur alan g\u00f6r\u00fcn\u00fcm\u00fcnde y\u00fczey \u015feklidir.B\u00fcy\u00fckl\u00fc\u011f\u00fc birka\u00e7 hektardan, y\u00fcz binlerce kilometrekareye kadar de\u011fi\u015febilen ovalar,\u00e7esitli y\u00fcksekliklerde yer alabilir.Y\u00fckseltisi 2000 metreye \u00e7ok yakla\u015fan ya da bu y\u00fckseltiyi de a\u015fan y\u00fcksek ovalar oldu\u011fu gibi, deniz seviyesinden y\u00fcksekligi \u00e7ok az olan ovalarda vard\u0131r.<\/p>\n
Y\u00fckseklik ne olursa olsun,ovalardan ge\u00e7en akarsular\u0131n derin yataklar\u0131 yoktur,yani ova y\u00fczeyi ile talveg \u00e7izgisi aras\u0131ndaki d\u00fczey fark\u0131 \u00e7ok azd\u0131r.Bu da ovay\u0131 platodan ay\u0131ran en belirgin \u00f6zelliktir.Ova t\u00fcm\u00fcyle d\u00fcz oldu\u011fu gibi,y\u00fczeyi engebeli de olabilir;hatta yer yer \u00fcst\u00fcnde tepeler bulunabilir.Ovalardaki akarsular genellikle a\u011f\u0131r ak\u0131\u015fl\u0131d\u0131r ve menderesler \u00e7izer ya da bir\u00e7ok kola ayr\u0131larak aralar\u0131nda adac\u0131klar olu\u015ftururlar.\u00d6nlem al\u0131nmazsa ta\u015fk\u0131n s\u0131ras\u0131nda yataklar\u0131ndan \u00e7\u0131k\u0131p ovaya veya \u00fcr\u00fcnlere zarar verebilirler. <\/p>\n
Yery\u00fcz\u00fcnde toplam kara alan\u0131n\u0131n \u00fc\u00e7te birinden biraz fazlas\u0131n\u0131 kaplayan ovalar,Antarktika d\u0131\u015f\u0131nda t\u00fcm k\u0131talarda g\u00f6r\u00fcl\u00fcr.Geni\u015f co\u011frafi da\u011f\u0131l\u0131mlar\u0131 nedeni ile ovalar\u0131n bitki \u00f6rt\u00fcs\u00fc de \u00e7e\u015fitlilik g\u00f6sterir.A\u011fa\u00e7,\u00e7al\u0131 ve ot kapl\u0131 ovalar oldu\u011fu gibi,neredeyse \u00e7\u00f6l g\u00f6r\u00fcn\u00fcm\u00fcnde olanlarda vard\u0131r.Kuru ve otsu bitkili ovalara bozk\u0131r denir.\u00c7ay\u0131rlarda bozk\u0131rlardakilerden daha k\u0131sa ama daha nitelikli ot yeti\u015fir.Savanlar ise uzun otsu bitkiler ve seyrek a\u011fa\u00e7lar\u0131n bulundugu ovalard\u0131r.Irmak havzalar\u0131ndaki ormanl\u0131k ovalara \u201cselva\u201d denir.Ovalar co\u011frafi konumlar\u0131na g\u00f6re k\u0131y\u0131 ovas\u0131 ve karasal ova ad\u0131 ile kabaca ikiye ayr\u0131l\u0131r.Karasal ovalardan biri da\u011f ete\u011fi ovas\u0131d\u0131r.Da\u011flar\u0131n ete\u011finde yer alan birikinti konilerinin kenarlardan birle\u015fmesiyle olusur.T\u00fcrkiye\u2019de Bursa ve \u0130neg\u00f6l ovalar\u0131n\u0131n g\u00fcney kenarlar\u0131nda tipik da\u011f ete\u011fi ovalar\u0131 vard\u0131r.Bu t\u00fcr ovalarda e\u011fim fazla,y\u00fczey profili hafif d\u0131\u015fb\u00fckeydir.D\u00fczg\u00fcn y\u00fczeyleri ve tar\u0131ma elveri\u015fli topraklar\u0131 nedeni ile ovalar y\u00fczy\u0131llardan beri ba\u015fl\u0131ca yerle\u015fim merkezleri olmu\u015ftur. <\/p>\n
OLU\u015eUMLARINA G\u00d6RE OVALAR VE T\u00dcRK\u0130YE’DE OVALARA \u00d6RNEKLER:<\/p>\n
A) B\u0130R\u0130K\u0130M (KIYI) OVALARI:<\/p>\n
Akarsular\u0131n ta\u015f\u0131d\u0131klar\u0131 al\u00fcvyonlar\u0131 deniz veya g\u00f6l k\u0131y\u0131s\u0131nda biriktirmesi ile olu\u015fan ovalard\u0131r.Kabaca bir \u00fc\u00e7gene benzediklerinden dolay\u0131 delta ovas\u0131 da denir.Delta ovalar\u0131n\u0131n olu\u015fabilmesi i\u00e7in akarsuyun yeterli miktarda materyal ta\u015f\u0131mas\u0131,k\u0131y\u0131n\u0131n s\u0131\u011f olmas\u0131,gelgit olaylar\u0131 ile k\u0131y\u0131 ak\u0131nt\u0131lar\u0131n\u0131n etkisiz olmas\u0131 gerekir. K\u0131y\u0131 ovalar\u0131n\u0131n olu\u015fumunda akarsular kadar,deniz ve g\u00f6llerdeki b\u00fcy\u00fck seviye de\u011fi\u015fiklikleri ve tektonik olaylar da etkilidir.<\/p>\n
\u00dclkemizde k\u0131y\u0131 ovalar\u0131,b\u00fcy\u00fck akarsular\u0131n denize d\u00f6k\u00fcld\u00fc\u011f\u00fc alanlarda meydana gelmi\u015ftir. Karadeniz k\u0131y\u0131lar\u0131m\u0131zdaki en \u00f6nemli k\u0131y\u0131 ovalari \u00c7arsamba, Bafra ve Sakarya deltalar\u0131d\u0131r. Bunlar,akarsular\u0131n ta\u015f\u0131d\u0131\u011f\u0131 al\u00fcvyonlar ve Karadeniz\u2019deki seviye degi\u015fiklikleri sonucunda olu\u015fmu\u015ftur. \u00c7arsamba Ovas\u0131;Ye\u015filirmak\u2019\u0131n ta\u015f\u0131d\u0131\u011f\u0131 al\u00fcvyonlar\u0131 denize biriktirmesiyle olu\u015fmu\u015ftur.\u00c7ok verimli topraklara sahip olan bu ova,b\u00f6lge tar\u0131m\u0131 i\u00e7in olduk\u00e7a \u00f6nemlidir. Bafra Ovas\u0131 da;K\u0131z\u0131l\u0131rmak\u2019\u0131n ta\u015f\u0131d\u0131\u011f\u0131 materyalleri k\u0131y\u0131ya biriktirmesi sonucunda olu\u015fan delta ovalar\u0131ndand\u0131r.Burada yer alan batakl\u0131klar kurutularak tar\u0131ma kazand\u0131r\u0131lm\u0131\u015ft\u0131r. Delta g\u00f6r\u00fcn\u00fcm\u00fcnden ziyade k\u0131y\u0131 d\u00fczl\u00fc\u011f\u00fc \u00f6zelli\u011fi g\u00f6steren Sakarya Deltas\u0131 ,Sakarya nehrinin ta\u015f\u0131d\u0131\u011f\u0131 al\u00fcvyonlarla meydana gelmi\u015ftir.\u00d6nceleri s\u0131k s\u0131k ta\u015fk\u0131na u\u011frayan ova,Hasan Polatkan Baraj\u0131\u2019n\u0131n yap\u0131m\u0131 ile ta\u015fk\u0131nlardan korunmu\u015f ve tar\u0131ma kazand\u0131r\u0131lm\u0131\u015ft\u0131r. <\/p>\n
Ege Denizi k\u0131y\u0131lar\u0131nda olu\u015fan ovalardan ba\u015fl\u0131calar\u0131; Meri\u00e7,Bak\u0131r\u00e7ay, Gediz ile K\u00fc\u00e7\u00fck ve B\u00fcy\u00fck Menderes deltalar\u0131d\u0131r.
\nMeri\u00e7 Deltas\u0131;h\u0131zl\u0131 ilerleyen ta\u015fk\u0131n alanlara sahip bir ovad\u0131r.Meri\u00e7 \u0131rma\u011f\u0131n\u0131n ta\u015f\u0131d\u0131\u011f\u0131 al\u00fcvyonlarla olu\u015fmu\u015ftur. Bak\u0131r\u00e7ay Deltas\u0131; ayn\u0131 ad\u0131 ta\u015f\u0131yan akarsuyun,\u00c7andarl\u0131 K\u00f6rfezi\u2019ni doldurmas\u0131 ile olu\u015fmu\u015ftur.Yer yer tuzlu batakl\u0131klar bulunan ovada, eski uygarl\u0131klar\u0131n kal\u0131nt\u0131lar\u0131 da yer al\u0131r. Ba\u015flang\u0131\u00e7ta \u0130zmir K\u00f6rfezi\u2019ne akan Gediz Irma\u011f\u0131,k\u00f6rfezi doldurmaya ba\u015flad\u0131\u011f\u0131 i\u00e7in 1886 y\u0131l\u0131nda a\u00e7\u0131lan kanallarla daha kuzeydeki bug\u00fcnk\u00fc yata\u011f\u0131na \u00e7ekilmi\u015ftir.Bu defa,k\u00f6rfezin kuzeybat\u0131s\u0131nda olduk\u00e7a geni\u015f bir delta olu\u015fmu\u015ftur.Geni\u015f bir \u00e7\u00f6k\u00fcnt\u00fc alan\u0131n\u0131n ucunda yer alan Gediz Deltas\u0131,Ege B\u00f6lgesi\u2019nin \u00f6nemli tar\u0131m alanlar\u0131ndand\u0131r. K\u00fc\u00e7\u00fck ve B\u00fcy\u00fck Menderes deltalar\u0131 da birer \u00e7\u00f6k\u00fcnt\u00fc alan\u0131n\u0131n ucunda olu\u015fan birikinti ovalar\u0131d\u0131r.B\u00fcy\u00fck ve K\u00fc\u00e7\u00fck Menderes Irmaklar\u0131,Ege Denizinin seviye de\u011fi\u015fikliklerine de ba\u011fl\u0131 olarak tarihi d\u00f6nemlerde h\u0131zla denizi doldurmu\u015ftur.\u00d6yle ki, \u0130lk \u00c7a\u011f\u2019da bir liman kenti olan Milet,B\u00fcy\u00fck Menderes\u2019in denizi doldurmas\u0131 ile bu g\u00fcn k\u0131y\u0131dan bir hayli i\u00e7eride kalm\u0131\u015ft\u0131r. <\/p>\n
Akdeniz k\u0131y\u0131lar\u0131nda yer alan en \u00f6nemli k\u0131y\u0131 ovalar\u0131 \u00c7ukurova,G\u00f6ksu ve Asi deltalar\u0131 ile Antalya Ovas\u0131dir. Bir \u00e7\u00f6k\u00fcnt\u00fc alan\u0131nda yer alan \u00c7ukurova,Seyhan ve Ceyhan Irmaklar\u0131n\u0131n biriktirdi\u011fi al\u00fcvyonlarla olu\u015fmu\u015ftur. \u00c7ukurova,Akdeniz\u2019in ve \u00fclkemizin en b\u00fcy\u00fck delta ovas\u0131d\u0131r.\u00dclkemizin en b\u00fcy\u00fck tar\u0131m alan\u0131 da olan \u00c7ukurova\u2019n\u0131n k\u0131y\u0131 kesiminde k\u0131y\u0131 set g\u00f6lleri ve kumullar olu\u015fmu\u015ftur. Ta\u015feli platosundan beslenen ve buray\u0131 derin vadilerle par\u00e7alam\u0131\u015f olan G\u00f6ksu, denize d\u00f6k\u00fcld\u00fc\u011f\u00fc yerde bir delta d\u00fczl\u00fc\u011f\u00fc olu\u015fturmu\u015ftur.Delta alan\u0131 i\u00e7inde yer yer g\u00f6ller ve batakl\u0131klar bulunmaktad\u0131r. Akdeniz k\u0131y\u0131lar\u0131nda ayr\u0131ca,Aksu \u00e7ay\u0131n\u0131n Antalya K\u00f6rfezi\u2019ni doldurarak olu\u015fturdu\u011fu Antalya Ovas\u0131 ile Asi nehrinin denize d\u00f6k\u00fcld\u00fc\u011f\u00fc yerde olu\u015fan deltalar di\u011fer k\u0131y\u0131 ovalar\u0131d\u0131r. <\/p>\n
Genellikle y\u00fcksek da\u011f s\u0131ralar\u0131n\u0131n bulundu\u011fu k\u0131y\u0131lar\u0131m\u0131zdaki delta ovalar\u0131,buralardaki en \u00f6nemli d\u00fczl\u00fcklerdir.Denizin iklim \u00fczerindeki olumlu etkileri bu ovalar\u0131n \u00f6nemini artt\u0131r\u0131r.Yine,\u00e7e\u015fitli bitkilerin yeti\u015fmesi i\u00e7in gerekli olan mineraller a\u00e7\u0131s\u0131ndan zengin olan bu ovalar,tar\u0131m i\u00e7in \u00e7ok elveri\u015flidir.Gerek iklim,gerekse su ve toprak \u015fartlar\u0131 a\u00e7\u0131s\u0131ndan uygun \u00f6zellikler ta\u015f\u0131yan k\u0131y\u0131 ovalar\u0131,n\u00fcfusun ve tar\u0131msal faaliyetlerin yo\u011funla\u015ft\u0131\u011f\u0131 alanlard\u0131r.<\/p>\n
\u0130\u00c7 B\u00d6LGELERDEK\u0130 OVALAR: <\/p>\n
Baz\u0131 k\u00fctleler,toptan y\u00fckselme ve \u00e7\u00f6kmeye u\u011fram\u0131\u015ft\u0131r.Bu olaylarla meydana gelen \u00e7\u00f6k\u00fcnt\u00fc alanlar\u0131nda,g\u00f6ller te\u015fekk\u00fcl etmi\u015ftir.Daha sonra g\u00f6llerin sular\u0131 \u00e7ekilmi\u015f ve akarsular\u0131n biriktirme faaliyetleri artm\u0131\u015ft\u0131r.Akarsular taraf\u0131ndan ta\u015f\u0131nan al\u00fcvyonlar,eski g\u00f6l tabanlar\u0131n\u0131 kaplam\u0131\u015f ve ovalar meydana gelmi\u015ftir. \u0130\u015fte i\u00e7 b\u00f6lgelerdeki ovalar\u0131n b\u00fcy\u00fck bir b\u00f6l\u00fcm\u00fc bu \u015fekilde olu\u015fmu\u015ftur.\u0130\u00e7 b\u00f6lgelerdeki ovalar,bazen fay hatlar\u0131 boyunca olu\u015fan \u00e7\u00f6k\u00fcnt\u00fc alanlarda dizi halinde yer al\u0131rken,bazen de tek tek serpilmi\u015f durumdad\u0131r. <\/p>\n
Do\u011fu Anadolu fay ku\u015fa\u011f\u0131 boyunca, Antakya-Kahramanmara\u015f-Karl\u0131ova olu\u011funda,birbirini takip eden bir\u00e7ok ova bulunmaktad\u0131r.Bunlar\u0131n ba\u015fl\u0131calar\u0131 Amik,Kahramanmara\u015f,Ad\u0131yaman,Malatya,Elaz\u0131\u011f ve Mu\u015f ovalar\u0131 ile Varto,H\u0131n\u0131s,Karl\u0131ova ve G\u00f6yn\u00fck ovalar\u0131d\u0131r.Bu \u00e7\u00f6k\u00fcnt\u00fc alanlar\u0131,engebeli bir yap\u0131ya sahip olan Do\u011fu Anadolu B\u00f6lgesi\u2019nin n\u00fcfus ve ekonomik faaliyetler bak\u0131m\u0131ndan en yo\u011fun alanlar\u0131d\u0131r.Ancak,fay ku\u015fa\u011f\u0131 \u00fczerinde yer almasi dolay\u0131s\u0131yla buralar s\u00fcrekli deprem tehdidi alt\u0131ndad\u0131r. Kuzey Anadolu fay ku\u015fa\u011f\u0131 ad\u0131 verilen ve Kuzey Anadolu da\u011flar\u0131n\u0131n g\u00fcney eteklerinden ge\u00e7en k\u0131r\u0131k hatt\u0131 boyunca,bir dizi \u00e7\u00f6k\u00fcnt\u00fc alan\u0131 bulunmaktad\u0131r.Bu ku\u015fakta yer alan ba\u015fl\u0131ca ovalar,bat\u0131da Ezine,Biga, G\u00f6nen,Manyas-Ulubat,Bursa,\u0130neg\u00f6l,Yeni\u015fehir,\u0130znik,Orhangazi ve Gemlik ovalar\u0131d\u0131r.\u0130zmit-Sapanca olu\u011fundan itibaren ise Adapazar\u0131,D\u00fczce,Bolu,Kayna\u015fl\u0131 ovalar\u0131 yer al\u0131r.Yine bu hat boyunca Ilgaz- Tosya, Karg\u0131, Vezirk\u00f6pr\u00fc, Suluova, Zile, Turhal, Erbaa, Niksar,Su\u015fehri,Erzincan,Erzurum ve Pasinler ovalar\u0131 ile A\u011fr\u0131-Ele\u015fkirt ovalar\u0131 yer almaktad\u0131r.Tar\u0131msal faaliyetlerin ve n\u00fcfusun yo\u011fun oldu\u011fu bu ovalar da fay hatt\u0131 \u00fczerinde yer ald\u0131\u011f\u0131 i\u00e7in deprem tehdidi alt\u0131ndad\u0131r. Bu hat \u00fczerinde zaman zaman meydana gelen depremler,can ve mal kayb\u0131na yol a\u00e7maktad\u0131r. <\/p>\n
Ergene Havzas\u0131,Ergene Irma\u011f\u0131 taraf\u0131ndan ta\u015f\u0131nan al\u00fcvyonlarla dolmustur.Olduk\u00e7a geni\u015f olan Ergene havzas\u0131 \u00fclkemizin en \u00f6nemli tarim alanlar\u0131ndan biridir. <\/p>\n
\u0130\u00e7 Anadolu B\u00f6lgesi\u2019nde yer alan ovalar da,\u00e7\u00f6k\u00fcnt\u00fc alanlar\u0131na al\u00fcvyonlar\u0131n birikmesiyle olu\u015fmu\u015ftur.Bunlar\u0131n ba\u015fl\u0131calar\u0131;Yukar\u0131 Sakarya,Eski\u015fehir ve Ak\u015fehir ovalar\u0131 ile Konya,Ere\u011fli,Ak\u0131nc\u0131 ve \u00c7ubuk ovalar\u0131d\u0131r. B\u00f6lgenin g\u00fcneydo\u011fusunda yer alan Kayseri ve Develi ovalar\u0131 ise,Erciyes Da\u011f\u0131\u2019ndan p\u00fcsk\u00fcren volkanik malzemelerden olu\u015fan ovalard\u0131r. <\/p>\n
Bat\u0131 Anadolu\u2019da yer alan ovalar orojenik ve epirojenik hareketlerle olu\u015fmu\u015ftur. Bu hareketler s\u0131ras\u0131nda baz\u0131 alanlar y\u00fckselmi\u015f ve bug\u00fcnk\u00fc da\u011fl\u0131k alanlar\u0131 meydana getirmi\u015f,baz\u0131 alanlar ise \u00e7\u00f6km\u00fc\u015f ve \u00e7\u00f6k\u00fcnt\u00fc alanlar\u0131 olu\u015fmu\u015ftur.Bu \u00e7\u00f6k\u00fcnt\u00fc alanlar\u0131n\u0131n akarsular taraf\u0131ndan al\u00fcvyonlarla doldurulmas\u0131 sonucunda g\u00fcn\u00fcm\u00fczdeki ovalar olu\u015fmu\u015ftur.Ege B\u00f6lgesi\u2019nin g\u00fcneydo\u011fusunda yer alan ovalar ise \u00e7\u00f6kme olaylar\u0131n\u0131n yan\u0131nda karstik olaylar\u0131n da etkisi ile olu\u015fmu\u015ftur.Denizli,Tavas,\u00c7ivril gibi ovalar\u0131n olu\u015fumunda karstik olaylar olduk\u00e7a etkilidir. <\/p>\n
Akdeniz B\u00f6lgesi\u2019nin bat\u0131s\u0131nda da karstik k\u00f6kenli ovalar yayg\u0131nd\u0131r.Bu alandaki \u00e7\u00f6k\u00fcnt\u00fc havzalar\u0131n\u0131n bir k\u0131sm\u0131 sular alt\u0131nda kalm\u0131\u015f ve bir\u00e7ok g\u00f6l olu\u015fmu\u015ftur.Baz\u0131 \u00e7\u00f6k\u00fcnt\u00fc havzalar\u0131 da karstik olaylar\u0131n etkisiyle geni\u015fleyerek ovalar\u0131 olu\u015fturmu\u015ftur.Bu \u015fekilde olusan ba\u015fl\u0131ca ovalar; Ac\u0131payam,Elmal\u0131,Korkuteli ve Kestel ovalar\u0131d\u0131r. <\/p>\n
G\u00fcneydo\u011fu Anadolu B\u00f6lgesi\u2019ndeki ovalar ise genellikle b\u00f6lgenin g\u00fcneyinde yer al\u0131r.Bu ovalar da \u00e7\u00f6kme,a\u015f\u0131nma ve biriktirme faaliyetleri ile olu\u015fmu\u015ftur.Nizip,Suru\u00e7,Alt\u0131nba\u015fak ve Ceylanp\u0131nar ovalar\u0131 bunlar\u0131n en \u00f6nemlileridir.<\/p>\n
Ba\u015fta Alt\u0131nba\u015fak ovas\u0131 olmak \u00fczere,b\u00f6lgenin b\u00fcy\u00fck bir b\u00f6l\u00fcm\u00fc GAP kapsam\u0131 i\u00e7indedir.Yap\u0131m\u0131 b\u00fcy\u00fck \u00f6l\u00e7\u00fcde tamamlanan \u015eanl\u0131urfa sulama t\u00fcnelleri ile sulanacak olan bu ovalar,\u00fclkemizin tar\u0131msal \u00fcretimini \u00f6nemli \u00f6l\u00e7\u00fcde artt\u0131racakt\u0131r. \u00dclkemiz,d\u00fcnyada kendine yetecek miktarda tar\u0131msal \u00fcretime sahip az say\u0131daki \u00fclkelerden biridir.Ayr\u0131ca,ihtiya\u00e7 fazlas\u0131 tar\u0131m \u00fcr\u00fcnlerini de ihra\u00e7 etmektedir.T\u00fcrkiye,\u015f\u00fcphesiz bu \u00f6zelli\u011fini b\u00fcy\u00fck oranda,sahip oldugu verimli ovalara bor\u00e7ludur.<\/p>\n
\u0130hra\u00e7 edilebilen tar\u0131m \u00fcr\u00fcnlerinin b\u00fcy\u00fck bir k\u0131sm\u0131 k\u0131y\u0131 ovalar\u0131nda yeti\u015ftirilmektedir.\u0130\u00e7 b\u00f6lgelerdeki ovalar ise,yeterince sulanamad\u0131\u011f\u0131ndan tar\u0131msal verim olduk\u00e7a d\u00fc\u015f\u00fckt\u00fcr.Bu sebeple uygulamaya koyulan,G\u00fcneydo\u011fu Anadolu Projesi (GAP) ile tasarlanan Konya Ovas\u0131 Projesi (KOP) tamamland\u0131\u011f\u0131 takdirde tar\u0131msal \u00fcretimimiz birka\u00e7 kat\u0131na \u00e7\u0131kabilecektir.<\/p>\n","protected":false},"excerpt":{"rendered":"
Ovalar\u0131n tan\u0131m\u0131 ve yap\u0131sal \u00f6zellikleri Akarsularla fazla yar\u0131lmam\u0131\u015f,d\u00fcz ya da hafif egimli \u00e7ukur alan g\u00f6r\u00fcn\u00fcm\u00fcnde y\u00fczey \u015feklidir.B\u00fcy\u00fckl\u00fc\u011f\u00fc birka\u00e7 hektardan, y\u00fcz binlerce kilometrekareye kadar de\u011fi\u015febilen ovalar,\u00e7esitli y\u00fcksekliklerde yer alabilir.Y\u00fckseltisi 2000 metreye \u00e7ok yakla\u015fan ya da bu y\u00fckseltiyi de a\u015fan y\u00fcksek ovalar oldu\u011fu gibi, deniz seviyesinden y\u00fcksekligi \u00e7ok az olan ovalarda vard\u0131r. Y\u00fckseklik ne olursa olsun,ovalardan ge\u00e7en …<\/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":[3609,10183,10182,10179,3671,10181,10184,10185,10186,10180,10178,2875,3670,3004],"class_list":["post-4718","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-akarsular","tag-akdeniz-kiyilari","tag-bakircay-deltasi","tag-bozkir","tag-carsamba-ovasi","tag-delta-ovasi","tag-ergene-havzasi","tag-ergene-irmagi","tag-konya-ovasi-projesi","tag-otsu-bitkiler","tag-ovalar-ve-ovalarimiz","tag-tektonik","tag-yeryuzu","tag-yesilirmak"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/4718","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=4718"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/4718\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=4718"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=4718"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=4718"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}