{"id":606,"date":"2006-03-30T15:47:00","date_gmt":"2006-03-30T12:47:00","guid":{"rendered":"https:\/\/www.xn--groymakhaber-dlb.com\/?p=606"},"modified":"2026-09-05T16:30:11","modified_gmt":"2026-09-05T13:30:11","slug":"guroymak-norsin-cografi-yapisi","status":"publish","type":"post","link":"https:\/\/www.xn--groymakhaber-dlb.com\/index.php\/2006\/03\/30\/guroymak-norsin-cografi-yapisi\/","title":{"rendered":"G\u00fcroymak (Nor\u015fin) Co\u011frafi yap\u0131s\u0131"},"content":{"rendered":"

G\u00fcroymak, Do\u011fu Anadolu B\u00f6lgesi’nde, Yukar\u0131 Murat Havzas\u0131’n\u0131n do\u011fusunda ve Van G\u00f6l\u00fc’n\u00fcn bat\u0131s\u0131nda, Mu\u015f Ovas\u0131’n\u0131n do\u011fu ucunda yer almaktad\u0131r. \u0130l\u00e7e, do\u011fu-bat\u0131 istikametinde uzanan iki da\u011f s\u0131ras\u0131n\u0131n aras\u0131nda, ova i\u00e7erisinde bulunan bir alan \u00fczerinde kurulmu\u015ftur.<\/p>\n

\u0130l\u00e7enin do\u011fusunda yer alan Nemrut Da\u011f\u0131 ve Krater G\u00f6l\u00fc ile bunlar\u0131n etekleri<\/strong>, \u00f6zellikle bat\u0131ya do\u011fru uzanarak il\u00e7enin kuzeyini \u00e7evrelemektedir. G\u00fcneyde yer alan Kilhar Da\u011f\u0131<\/strong> ise Do\u011fu Toroslar\u0131n uzant\u0131s\u0131 olup, il\u00e7enin bat\u0131s\u0131na do\u011fru hafif bir e\u011fimle ovaya uzanmaktad\u0131r.<\/p>\n

\"G\u00fcroymak'\u0131n<\/p>\n

\u0130klim ve Bitki \u00d6rt\u00fcs\u00fc<\/h3>\n

G\u00fcroymak’\u0131n iklim yap\u0131s\u0131 genel olarak Bitlis ilinin Akdeniz iklimi ile karasal iklim aras\u0131ndaki ge\u00e7i\u015f \u00f6zelli\u011fine benzemekle birlikte, \u00f6nemli farkl\u0131l\u0131klar da g\u00f6stermektedir.<\/p>\n

K\u0131\u015f ve bahar aylar\u0131nda, \u00f6zellikle yo\u011fun sis nedeniyle g\u00fcne\u015fli g\u00fcn say\u0131s\u0131 azd\u0131r. \u0130l\u00e7enin do\u011fusunda bulunan Rahva D\u00fczl\u00fc\u011f\u00fc<\/strong>, do\u011fal bir r\u00fczg\u00e2r koridoru olmas\u0131 nedeniyle b\u00fcy\u00fck tipi ve f\u0131rt\u0131nalara sahne olmaktad\u0131r.<\/p>\n

K\u0131\u015flar so\u011fuk ve yo\u011fun kar ya\u011f\u0131\u015fl\u0131, baharlar ise ya\u011fmurlu ge\u00e7mektedir. Yazlar k\u0131sa ve \u0131l\u0131k bir \u00f6zellik g\u00f6stermektedir.<\/p>\n

\u0130l\u00e7enin y\u00fcksek kesimlerinde yeti\u015fen me\u015fe ve kavak a\u011fa\u00e7lar\u0131n\u0131n tahrip edilerek kesilmesi nedeniyle da\u011fl\u0131k araziler b\u00fcy\u00fck \u00f6l\u00e7\u00fcde \u00e7\u0131plak kalm\u0131\u015f, seyrek \u00e7al\u0131larla kapl\u0131 otlaklar niteli\u011finde bir g\u00f6r\u00fcn\u00fcm ortaya \u00e7\u0131km\u0131\u015ft\u0131r.<\/p>\n

Ovadaki eski ormanlar\u0131n da tahrip olmas\u0131 sonucunda, yer yer sellerle kapl\u0131 bozk\u0131r niteli\u011finde bir arazi yap\u0131s\u0131 olu\u015fmu\u015ftur.<\/p>\n

\u0130l\u00e7enin deniz seviyesinden y\u00fcksekli\u011fi 1.320 metre<\/strong>, k\u00f6yleriyle birlikte y\u00fcz\u00f6l\u00e7\u00fcm\u00fc ise 650 km\u00b2<\/strong>dir.<\/p>\n

\n

Akarsu Kaynaklar\u0131<\/h2>\n

\u0130l\u00e7emizde, Nemrut Da\u011f\u0131 ve Nemrut Krater G\u00f6l\u00fc’n\u00fcn<\/strong> etkisiyle s\u0131cak su kaynaklar\u0131n\u0131n yan\u0131 s\u0131ra, kar sular\u0131na dayal\u0131 olduk\u00e7a g\u00fcr do\u011fal su kaynaklar\u0131 bulunmaktad\u0131r.<\/p>\n

Nemrut Da\u011f\u0131 Krater G\u00f6l\u00fc’nden etkilenerek il\u00e7e merkezinde bulunan K\u00fcmbet Mahallesi’nde<\/strong>, \u015eelale G\u00f6l\u00fc<\/strong> olarak adland\u0131r\u0131lan tatl\u0131 su kayna\u011f\u0131 olu\u015fmaktad\u0131r.<\/p>\n

Meydana gelen do\u011fal su kaynaklar\u0131n\u0131n olu\u015fturdu\u011fu akarsular, \u015fehir merkezi ve \u00e7evresinden bat\u0131 istikametine do\u011fru dere yataklar\u0131 i\u00e7erisinden akmaktad\u0131r.<\/p>\n

\u0130l\u00e7e merkezinin K\u00fcmbet mevkiinde bulunan \u015eelale G\u00f6l\u00fc’nden kaynayan su, bir dere h\u00e2linde bat\u0131ya do\u011fru uzanmakta; Germav (Kapl\u0131ca)<\/strong> b\u00f6lgesindeki kaynaklarla birle\u015ferek Karasu Nehri’nin ba\u015flang\u0131c\u0131n\u0131<\/strong> olu\u015fturmaktad\u0131r.<\/p>\n

Bu nedenle il\u00e7enin bat\u0131 k\u0131sm\u0131ndaki oval\u0131k alan yar\u0131 batakl\u0131k ve sazl\u0131k bir yap\u0131 g\u00f6stermektedir.<\/p>\n

\u0130l\u00e7enin Ta\u015f\u00fcst\u00fc, \u00c7ayaras\u0131 ve Yemi\u015fveren<\/strong> k\u00f6ylerinden de bol sulu p\u0131narlar kaynamakta ve ovaya do\u011fru akmaktad\u0131r. Karlar\u0131n erimesiyle birlikte A\u015fa\u011f\u0131 Kolba\u015f\u0131 K\u00f6y\u00fc’n\u00fcn<\/strong> g\u00fcneyinden gelen g\u00fc\u00e7l\u00fc bir dere de il\u00e7e merkezinden ge\u00e7erek akmaktad\u0131r.<\/p>\n

\n

G\u00fcroymak (Nor\u015fin-\u00c7ukur) S\u0131cak Su Kapl\u0131cas\u0131 ve G\u00f6l\u00fc<\/h2>\n

Van G\u00f6l\u00fc \u00e7evresinde kapl\u0131ca kaynaklar\u0131n\u0131n olu\u015fumuna etken fakt\u00f6rler bak\u0131m\u0131ndan, Van-Tatvan fay hatt\u0131n\u0131n kuzey ve g\u00fcney b\u00f6l\u00fcmleri birbirinden farkl\u0131 \u00f6zellikler g\u00f6stermektedir.<\/p>\n

Bu hatt\u0131n kuzeyinde kalan alanlarda, yak\u0131n zamanlardaki volkanik faaliyetlerin yo\u011fun olmas\u0131na ba\u011fl\u0131 olarak \u00e7ok say\u0131da s\u0131cak su kayna\u011f\u0131 bulunmaktad\u0131r. Buna kar\u015f\u0131l\u0131k hatt\u0131n g\u00fcneyi genel olarak ya\u015fl\u0131 jeolojik olu\u015fumlara sahip olup, s\u0131cak su kayna\u011f\u0131 bak\u0131m\u0131ndan fazla zengin de\u011fildir.<\/p>\n

\u0130ldeki kapl\u0131calar aras\u0131nda en \u00f6nemlisi G\u00fcroymak (Nor\u015fin-\u00c7ukur) S\u0131cak Su Kapl\u0131ca G\u00f6l\u00fc<\/strong>d\u00fcr. Yer ve konumu, ak\u0131m de\u011feri, fiziksel ve kimyasal \u00f6zellikleri bak\u0131m\u0131ndan olumlu \u00f6zelliklere sahiptir.<\/p>\n

G\u00fcroymak (Nor\u015fin-\u00c7ukur) S\u0131cak Su Kapl\u0131cas\u0131, Turizm Bakanl\u0131\u011f\u0131’n\u0131n \u00e7al\u0131\u015fmalar\u0131nda ve ilgili literat\u00fcrde b\u00f6lgesel \u00f6l\u00e7ekte \u00f6nem ta\u015f\u0131yan 2. derece \u00f6ncelikli kapl\u0131ca<\/strong> olarak tan\u0131mlanm\u0131\u015ft\u0131r.<\/p>\n

\u0130lde bulunan di\u011fer kapl\u0131ca, i\u00e7me ve maden sular\u0131 ise yerel ve y\u00f6resel \u00f6l\u00e7ekte kullan\u0131ma a\u00e7\u0131labilecek nitelikteki kaynaklard\u0131r.<\/p>\n

Bunlardan Nemrut Da\u011f\u0131 Kapl\u0131cas\u0131<\/strong>, ak\u0131m de\u011feri d\u00fc\u015f\u00fck, fiziksel ve kimyasal nitelikleri y\u00fcksek olmamakla birlikte, konumu nedeniyle \u00e7evresindeki do\u011fal de\u011ferlerle birlikte \u00f6nem kazanmaktad\u0131r.<\/p>\n

Bitlis ilindeki kaynaklardan G\u00fcroymak (Nor\u015fin-\u00c7ukur)<\/strong> ve Il\u0131cak (Germav)<\/strong> kapl\u0131calar\u0131n\u0131n fiziksel ve kimyasal analizleri yap\u0131lm\u0131\u015f ve nitelikleri belirlenmi\u015ftir.<\/p>\n

Yer ve Konumu<\/h3>\n

G\u00fcroymak (Nor\u015fin-\u00c7ukur) S\u0131cak Su Kapl\u0131cas\u0131 G\u00f6l\u00fc, Mu\u015f-Tatvan yolu \u00fczerinde yer alan G\u00fcroymak (Nor\u015fin) yerle\u015fimine 12 km<\/strong> uzakl\u0131kta ve Mu\u015f Ovas\u0131’n\u0131n kuzeydo\u011fu kenar\u0131nda bulunmaktad\u0131r.<\/p>\n

Fiziksel ve Kimyasal \u00d6zellikleri ve Etkili Oldu\u011fu Hastal\u0131klar<\/h3>\n

Su s\u0131cakl\u0131\u011f\u0131 38-39\u00b0C<\/strong>, pH de\u011feri ise yakla\u015f\u0131k 6,7<\/strong> olan G\u00fcroymak (Nor\u015fin) S\u0131cak Su Kapl\u0131cas\u0131 sular\u0131; bikarbonatl\u0131, sodyumlu, magnezyumlu, kalsiyumlu, demirli ve karbondioksitli bir bile\u015fime sahiptir.<\/p>\n

Banyo ve \u00e7amur banyosu uygulamalar\u0131na elveri\u015fli olan bu sular\u0131n; romatizmal, solunum yolu, sinir sistemi, sindirim sistemi, b\u00f6brek ve idrar yollar\u0131 ile metabolizma bozukluklar\u0131<\/strong> gibi hastal\u0131klara olumlu etki yapt\u0131\u011f\u0131 belirtilmektedir.<\/p>\n

Emniyet ve Yerle\u015fme Durumu<\/h3>\n

Yan yana bulunan iki kayna\u011f\u0131n da kaynak emniyet alan\u0131 korunmam\u0131\u015ft\u0131r. \u00c7evresi, yeni geli\u015fme ve yat\u0131r\u0131mlara uygundur.<\/p>\n

Yap\u0131 Durumu<\/h3>\n

Ula\u015f\u0131m durumu ve di\u011fer altyap\u0131 yat\u0131r\u0131mlar\u0131 yetersizdir. Tedavi tesisleri a\u00e7\u0131k havuzlar h\u00e2lindedir. Y\u00f6rede konaklama tesisi bulunmamaktad\u0131r. \u00c7ad\u0131r gelene\u011fi bulunmaktad\u0131r.<\/p>\n

Var olan konaklama yerlerinin kullan\u0131lmamas\u0131 nedeniyle ge\u00e7mi\u015fte \u00d6zel \u0130dare taraf\u0131ndan yap\u0131lm\u0131\u015f olan tesisler kullan\u0131lamaz durumdad\u0131r.<\/p>\n

Genel De\u011ferlendirme<\/h3>\n

Kesin ak\u0131m \u00f6l\u00e7\u00fcm\u00fc yap\u0131lamam\u0131\u015ft\u0131r. B\u00fcy\u00fck bir g\u00f6l kenar\u0131nda \u00e7\u0131k\u0131\u015f yapan kapl\u0131ca sular\u0131, yakla\u015f\u0131k 40 litre\/sn<\/strong> su verimine ve 9.874 ki\u015fi\/g\u00fcn\/banyo<\/strong> kapasitesine sahiptir.<\/p>\n

Kapl\u0131ca sular\u0131n\u0131n tam analizleri yap\u0131lm\u0131\u015ft\u0131r. B\u00f6lgesel ve y\u00f6resel \u00f6nem ta\u015f\u0131yan bu kapl\u0131ca sular\u0131 ve \u00e7evresinin planl\u0131 olarak geli\u015ftirilmesi uygun ve yararl\u0131 g\u00f6r\u00fclmektedir.<\/p>\n

Kapl\u0131ca \u00fczerine yap\u0131lacak konaklama ve tesis yat\u0131r\u0131mlar\u0131n\u0131n, kapl\u0131cadan daha fazla fayda sa\u011flanmas\u0131na katk\u0131 sunaca\u011f\u0131 i\u00e7in de\u011ferlendirilmesi b\u00fcy\u00fck yarar sa\u011flayacakt\u0131r.<\/p>\n

\n

G\u00fcroymak (Nor\u015fin) \u015eelale G\u00f6l\u00fc<\/h2>\n

G\u00fcroymak \u015eelale G\u00f6l\u00fc’n\u00fcn tarihi \u00e7ok eskiye dayanmaktad\u0131r.<\/p>\n

Nemrut Da\u011f\u0131’n\u0131n<\/strong> volkanik patlamas\u0131 sonucu il\u00e7e merkezi K\u00fcmbet Mahallesi mevkiinde meydana gelen G\u00fcroymak \u015eelale G\u00f6l\u00fc, il\u00e7eye 12 km uzakl\u0131kta bulunan G\u00fcroymak (Nor\u015fin-\u00c7ukur) S\u0131cak Su Kapl\u0131cas\u0131 ve G\u00f6l\u00fc<\/strong> ile birle\u015ferek Karasu Nehri’ni<\/strong> olu\u015fturmakta ve il\u00e7enin bat\u0131 istikametine do\u011fru akmaktad\u0131r.<\/p>\n

Ayr\u0131ca il\u00e7enin i\u00e7me suyu ihtiyac\u0131nda kullan\u0131lan do\u011fal kaynak suyunun il\u00e7e merkezinde bulunmas\u0131, il\u00e7e i\u00e7in g\u00fczel bir ticaret ve turizm alan\u0131 olu\u015fturmaktad\u0131r.<\/p>\n

\n

Nemrut Krater G\u00f6l\u00fc<\/h2>\n

Anadolu’da tarih\u00ee \u00e7a\u011flarda faaliyet g\u00f6steren birka\u00e7 yanarda\u011fdan biri de Nemrut Da\u011f\u0131’d\u0131r<\/strong>. Bu yanarda\u011f\u0131n en son 1441 y\u0131l\u0131ndaki faaliyetini, 15. y\u00fczy\u0131lda bu y\u00f6rede ya\u015fayan Wardan<\/strong> adl\u0131 bir yazar\u0131n eserinden \u00f6\u011frenmekteyiz.<\/p>\n

S\u00f6z konusu eserde verilen bilgiye g\u00f6re, 1441 y\u0131l\u0131nda Ahlat ile Bitlis aras\u0131nda bulunan Nemrut Da\u011f\u0131, g\u00f6k g\u00fcr\u00fclt\u00fcs\u00fcne benzeyen bir sesle g\u00fcrlemi\u015f ve insanlar\u0131 deh\u015fete d\u00fc\u015f\u00fcrm\u00fc\u015ft\u00fcr.<\/p>\n

Da\u011fdaki buzlar yar\u0131lm\u0131\u015f, yar\u0131klardan duman ve alev f\u0131\u015fk\u0131rmaya ba\u015flam\u0131\u015ft\u0131r. Alevlerin i\u00e7inde eriyen ta\u015flar ve kayalar, \u015fiddetli g\u00fcr\u00fclt\u00fclerle havaya u\u00e7mu\u015ftur.<\/p>\n

Ahlat \u015fehrinin y\u0131k\u0131laca\u011f\u0131ndan korkan \u015fehir halk\u0131 b\u00fcy\u00fck bir endi\u015fe ya\u015fam\u0131\u015f ve \u00e7evreye ka\u00e7m\u0131\u015ft\u0131r. Da\u011fdan \u00e7\u0131kan \u00f6ld\u00fcr\u00fcc\u00fc ve k\u00f6t\u00fc kokular insanlar\u0131n hastalanmas\u0131na neden olmu\u015ftur. Bu durumu \u00e7evre yerle\u015fim birimlerinde ya\u015fayanlar da a\u00e7\u0131k\u00e7a g\u00f6rm\u00fc\u015flerdir.<\/p>\n

Patlamalar neticesinde tepe k\u0131sm\u0131n\u0131 kaybedip kesik koni \u015feklini almas\u0131na ra\u011fmen Nemrut Da\u011f\u0131’n\u0131n y\u00fcksekli\u011fi, kalderan\u0131n kuzeyinde 3.050 metreye<\/strong> kadar ula\u015fmaktad\u0131r. Kalderan\u0131n \u00e7evresinde yer yer 2.800 metreyi<\/strong> a\u015fan y\u00fckseltiler bulunmaktad\u0131r.<\/p>\n

Nemrut Kalderas\u0131 i\u00e7erisinde s\u00fcrekli olarak iki g\u00f6l ile genellikle yaz mevsiminin sonlar\u0131na do\u011fru kuruyan \u00fc\u00e7 g\u00f6l daha bulunmaktad\u0131r. G\u00f6llerin beslenme kaynaklar\u0131 ya\u011f\u0131\u015flard\u0131r ve su seviyeleri y\u0131ll\u0131k ya\u011f\u0131\u015f miktar\u0131na g\u00f6re de\u011fi\u015fmektedir.<\/p>\n

G\u00f6llerin en b\u00fcy\u00fc\u011f\u00fc olan Nemrut Krater G\u00f6l\u00fc<\/strong>, kabaca hilal \u015feklinde bir g\u00f6r\u00fcn\u00fcme sahiptir. Y\u00fcz\u00f6l\u00e7\u00fcm\u00fc yakla\u015f\u0131k 12 km\u00b2<\/strong>dir. Ortalama derinli\u011fi ise yakla\u015f\u0131k 100 metre<\/strong> civar\u0131ndad\u0131r.<\/p>\n

G\u00f6l i\u00e7erisinde bol miktarda aynal\u0131 sazan ve az miktarda di\u011fer bal\u0131k t\u00fcrleri bulunmaktad\u0131r. G\u00f6l suyu tatl\u0131 ve so\u011fuktur.<\/p>\n

Al\u0131nan \u00f6rneklerin analizleri sonucunda suyun berrak, renksiz, kokusuz ve normal i\u00e7me suyu lezzetinde oldu\u011fu tespit edilmi\u015ftir.<\/p>\n

\n

Il\u0131g\u00f6l<\/h2>\n

Il\u0131g\u00f6l’\u00fcn<\/strong> y\u00fcz\u00f6l\u00e7\u00fcm\u00fc yakla\u015f\u0131k 1,2 km\u00b2<\/strong>dir.<\/p>\n

Gerek g\u00f6l taban\u0131ndan gerekse g\u00f6l\u00fcn \u00e7evresinden kar\u0131\u015fan s\u0131cak sular ve buhar nedeniyle g\u00f6l\u00fcn s\u0131cakl\u0131\u011f\u0131 k\u0131\u015f mevsiminde bile 40 dereceye<\/strong>, yaz mevsiminde ise 60 dereceye<\/strong> kadar ula\u015fmaktad\u0131r.<\/p>\n

Baz\u0131 asalaklar d\u0131\u015f\u0131nda canl\u0131 hayat\u0131na imk\u00e2n vermeyen bu g\u00f6l suyu, genellikle romatizma tedavisinde b\u00fcy\u00fck bir \u015fifa kayna\u011f\u0131 olarak g\u00f6r\u00fclmektedir.<\/p>\n

Yak\u0131n \u00e7evrelerden gelen ziyaret\u00e7ilerin, 3-4 g\u00fcn kadar \u00e7ad\u0131r ve kendi imk\u00e2nlar\u0131yla yapt\u0131klar\u0131 bar\u0131naklarda kalarak g\u00fcnde 2-3 kez g\u00f6lde banyo yapmak suretiyle tedavi olduklar\u0131 g\u00f6zlemlenmektedir.<\/p>\n

Il\u0131g\u00f6l civar\u0131ndaki \u00e7ok say\u0131da s\u0131cak su kayna\u011f\u0131na ek olarak, g\u00f6l\u00fcn yakla\u015f\u0131k 160 metre do\u011fusundaki<\/strong> kayal\u0131k bir alanda s\u0131cakl\u0131kla birlikte buhar \u00e7\u0131k\u0131\u015f\u0131 g\u00f6r\u00fclmektedir.<\/p>\n

Bu buhar\u0131n \u00f6zellikle ast\u0131m ve bron\u015fit gibi hastal\u0131klarda teneff\u00fcs yoluyla; b\u00f6brek ve romatizma hastalar\u0131nda ise v\u00fccudu buhar \u00e7\u0131kan yere tutmak suretiyle tedavi amac\u0131yla kullan\u0131ld\u0131\u011f\u0131 bilinmektedir.<\/p>\n

Il\u0131g\u00f6l civar\u0131ndaki s\u0131cak su kaynaklar\u0131n\u0131n varl\u0131\u011f\u0131 ve yer yer g\u00f6r\u00fclen buhar \u00e7\u0131k\u0131\u015flar\u0131, buran\u0131n \u00f6nemli bir jeotermal enerji potansiyeli<\/strong> ta\u015f\u0131d\u0131\u011f\u0131 g\u00f6r\u00fc\u015f\u00fcn\u00fc kuvvetlendirmektedir.<\/p>\n","protected":false},"excerpt":{"rendered":"

G\u00fcroymak, Do\u011fu Anadolu B\u00f6lgesi’nde, Yukar\u0131 Murat Havzas\u0131’n\u0131n do\u011fusunda ve Van G\u00f6l\u00fc’n\u00fcn bat\u0131s\u0131nda, Mu\u015f Ovas\u0131’n\u0131n do\u011fu ucunda yer almaktad\u0131r. \u0130l\u00e7e, do\u011fu-bat\u0131 istikametinde uzanan iki da\u011f s\u0131ras\u0131n\u0131n aras\u0131nda, ova i\u00e7erisinde bulunan bir alan \u00fczerinde kurulmu\u015ftur. \u0130l\u00e7enin do\u011fusunda yer alan Nemrut Da\u011f\u0131 ve Krater G\u00f6l\u00fc ile bunlar\u0131n etekleri, \u00f6zellikle bat\u0131ya do\u011fru uzanarak il\u00e7enin kuzeyini \u00e7evrelemektedir. G\u00fcneyde yer alan […]<\/p>\n","protected":false},"author":1,"featured_media":226,"comment_status":"open","ping_status":"open","sticky":true,"template":"","format":"standard","meta":{"jnews-multi-image_gallery":[],"jnews_single_post":{"format":"standard"},"jnews_primary_category":[],"jnews_social_meta":[],"jnews_review":[],"enable_review":"","type":"","name":"","summary":"","brand":"","sku":"","good":[],"bad":[],"score_override":"","override_value":"","rating":[],"price":[],"jnews_override_counter":[],"jnews_post_split":[],"footnotes":""},"categories":[1],"tags":[95,93,94,53,96,62],"class_list":["post-606","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-guroymak-norsin-hakkinda","tag-bitki-ortusu","tag-cografi-yapisi","tag-cografyasi","tag-guroymak","tag-iklimi","tag-norsin"],"_links":{"self":[{"href":"https:\/\/www.xn--groymakhaber-dlb.com\/index.php\/wp-json\/wp\/v2\/posts\/606","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.xn--groymakhaber-dlb.com\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.xn--groymakhaber-dlb.com\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.xn--groymakhaber-dlb.com\/index.php\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.xn--groymakhaber-dlb.com\/index.php\/wp-json\/wp\/v2\/comments?post=606"}],"version-history":[{"count":2,"href":"https:\/\/www.xn--groymakhaber-dlb.com\/index.php\/wp-json\/wp\/v2\/posts\/606\/revisions"}],"predecessor-version":[{"id":609,"href":"https:\/\/www.xn--groymakhaber-dlb.com\/index.php\/wp-json\/wp\/v2\/posts\/606\/revisions\/609"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.xn--groymakhaber-dlb.com\/index.php\/wp-json\/wp\/v2\/media\/226"}],"wp:attachment":[{"href":"https:\/\/www.xn--groymakhaber-dlb.com\/index.php\/wp-json\/wp\/v2\/media?parent=606"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.xn--groymakhaber-dlb.com\/index.php\/wp-json\/wp\/v2\/categories?post=606"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.xn--groymakhaber-dlb.com\/index.php\/wp-json\/wp\/v2\/tags?post=606"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}