\n Ege B\u00f6lgesi 85.000km2 dolay\u0131ndaki y\u00fcz\u00f6l\u00e7\u00fcm\u00fcyle T\u00fcrkiye topraklar\u0131n\u0131n yakla\u015f\u0131k %11\u2019ini kaplayan, kuzeyde Marmara B\u00f6lgesi\u2019ne, do\u011fuda \u0130\u00e7 Anadolu B\u00f6lgesi\u2019ne, g\u00fcneydo\u011fuda Akdeniz B\u00f6lgesi\u2019ne kom\u015fu olan b\u00f6lgemiz bat\u0131da da Ege Denizi\u2019yle \u00e7evrilidir (ad\u0131n\u0131 kom\u015fu oldu\u011fu denizden al\u0131r). Marmara B\u00f6lgesi\u2019yle olan s\u0131n\u0131r\u0131 bat\u0131da Baba Burnu\u2019ndan ba\u015flayarak Edremit K\u00f6rfezi\u2019nin kuzeyinde y\u00fckselen Kaz Da\u011f\u0131\u2019na uzan\u0131r. \u0130\u00e7 Anadolu B\u00f6lgesi\u2019yle olan s\u0131n\u0131r\u0131 ise \u0130n\u00f6n\u00fc\u2019n\u00fcn g\u00fcneybat\u0131s\u0131ndan ba\u015flay\u0131p Sultan Da\u011flar\u0131\u2019n\u0131n kuzey ucuna ula\u015f\u0131r. O noktadan ba\u015flayarak Ege B\u00f6lgesi Akdeniz B\u00f6lgesi\u2019ne kom\u015fu olur ve bu b\u00f6lgeyle olan s\u0131n\u0131r ise K\u00f6yce\u011fiz G\u00f6l\u00fc\u2019n\u00fcn bat\u0131s\u0131na kadar uzan\u0131r.
\nEge B\u00f6lgesi as\u0131l Ege ve \u0130\u00e7bat\u0131 Anadolu olmak \u00fczere iki b\u00f6l\u00fcme ayr\u0131l\u0131r. Ege B\u00f6l\u00fcm\u00fc\u2019ndeki illerimiz; \u0130zmir, Manisa, Ayd\u0131n, Denizli,Mu\u011fla\u0130\u00e7bat\u0131 Anadolu\u2019daki iller; U\u015fak, K\u00fctahya, Afyon\u2019dur.<\/p>\n
N\u00fcfus<\/p>\n
Ege B\u00f6lgesi s\u0131k n\u00fcfuslanm\u0131\u015f\u0131r. 1990 say\u0131m\u0131na g\u00f6re b\u00f6lge n\u00fcfusu 8.2 milyondur. N\u00fcfus yo\u011funlu\u011fu bak\u0131m\u0131ndan Marmara B\u00f6lgesi\u2019den sonra ikinci s\u0131rada yer al\u0131r. B\u00f6lge n\u00fcfusunun yar\u0131s\u0131ndan \u00e7o\u011fu kentlerde ya\u015famaktad\u0131r.
\n B\u00f6lge n\u00fcfusunun \u00f6nemli bir b\u00f6l\u00fcm\u00fc, k\u0131y\u0131 kesimi ile \u00e7\u00f6k\u00fcnt\u00fc ovalar\u0131nda toplanm\u0131\u015ft\u0131r. K\u0131y\u0131 kesiminde de n\u00fcfus da\u011f\u0131l\u0131\u015f\u0131 bak\u0131m\u0131ndan y\u00f6reler aras\u0131nda \u00f6nemli farkl\u0131l\u0131klar g\u00f6r\u00fcl\u00fcr. Ovalarda n\u00fcfus yo\u011fun, ovalar\u0131 ay\u0131ran da\u011fl\u0131k kesimlerde n\u00fcfus seyrektir. G\u00fcneydeki Mente\u015fe y\u00f6resi T\u00fcrkiye\u2019nin en az n\u00fcfuslanm\u0131\u015f yerlerindendir. \u0130\u00e7bat\u0131 Anadolu ise genel olarak az n\u00fcfuslanm\u0131\u015ft\u0131r.<\/p>\n
Y\u00fczey \u015eekilleri<\/p>\n
Ege B\u00f6l\u00fcm\u00fc\u2019nde ba\u015fl\u0131ca da\u011f s\u0131ralar\u0131 ve bunlar\u0131 birbirinden ay\u0131ran vadi oluklar\u0131, do\u011fu-bat\u0131 do\u011frultulu \u00e7ukurluklar olu\u015fturur. Bu \u00e7ukurluklar, aralar\u0131nda kalan do\u011fu-bat\u0131 do\u011frultulu y\u00fcksek k\u00fctlelere da\u011f s\u0131ralar\u0131 g\u00f6r\u00fcn\u00fcm\u00fc kazand\u0131r\u0131r. \u00c7ukurluklar\u0131n bat\u0131 u\u00e7lar\u0131 yak\u0131n bir d\u00f6nemde deniz basmas\u0131yla koy ya da k\u00f6rfez bi\u00e7imini alm\u0131\u015f ama daha sonra k\u0131smen ya da tamamen al\u00fcvyonlarla dolmu\u015ftur ve par\u00e7al\u0131 bir yap\u0131 g\u00f6sterir. Yer yer 2000m\u2019yi ge\u00e7en da\u011f k\u00fctleleri g\u00f6r\u00fcl\u00fcr. Bunlar \u0130\u00e7bat\u0131 Anadolu\u2019nun 1000m\u2019yi ge\u00e7ebilen d\u00fczl\u00fcklerinden daha al\u00e7ak olan Ege B\u00f6l\u00fcm\u00fc\u2019ndeki ovalar \u00fczerinde heybetli bir g\u00f6r\u00fcn\u00fcm kazan\u0131r.
\n Ege B\u00f6lgesi\u2019nde yerin temelini jeologlaron Menderes Masifi ad\u0131n\u0131 verdikleri Saruhan-Mente\u015fe eski k\u00fctlesi olu\u015fturur. Paleozoyik zaman ortalar\u0131nda k\u0131vr\u0131lmalara u\u011fram\u0131\u015f daha sonra a\u015f\u0131narak d\u00fczle\u015fmi\u015f olan bu eski temel, Tersiyer D\u00f6nem i\u00e7inde yeniden yer hareketlerine u\u011fray\u0131nca, bir daha k\u0131vr\u0131lamay\u0131p k\u0131r\u0131lm\u0131\u015ft\u0131r. Belli k\u0131r\u0131k \u00e7izgileri boyunca baz\u0131 par\u00e7alar\u0131n \u00e7\u00f6kmesiyle s\u00f6z\u00fc edilen oluk bi\u00e7imli \u00e7ukurlar (graben) ortaya \u00e7\u0131km\u0131\u015f, bunlar\u0131n aras\u0131nda da sert ve kristalli kaya\u00e7lardan olu\u015fan eski da\u011f k\u00fctleleri (horst) y\u00fckselmi\u015ftir. Bu eski k\u00fctle yeniden k\u0131vr\u0131lmamakla birlikte, \u00e7evresinde biriken deniz dibi tortullar\u0131 k\u0131vr\u0131l\u0131rken onlara kal\u0131p olmu\u015ftur.
\n Do\u011fu-bat\u0131 do\u011frultulu \u00e7ukur alanlarla bunlar\u0131 ay\u0131ran ayn\u0131 do\u011frultulu y\u00fcksek alanlar kuzeyden g\u00fcneye do\u011fru \u015f\u00f6yle s\u0131ralan\u0131r: Edremit K\u00f6rfezi ve Edremit Ova\u2019s\u0131 \u00e7ukur alan\u0131, Bak\u0131r\u00e7ay Ovas\u0131\u2019ndan Madra Da\u011f\u0131 (1.334m) ve Kozak K\u00fctlesi\u2019yle (1.051m) ayr\u0131l\u0131r. Bak\u0131r\u00e7ay Ova\u2019s\u0131 ile Gediz Ovas\u0131 aras\u0131nda Yunt Da\u011f\u0131 (1.075m) yer al\u0131r; Gediz Ovas\u0131\u2019na kuzeyden Akhisar, g\u00fcneyden de Nif (Kemalpa\u015fa) Ovalar\u0131 birer k\u00f6rfez gibi kat\u0131l\u0131r. Gediz Ova\u2019s\u0131 ile daha g\u00fcneydeki K\u00fc\u00e7\u00fck Menderes Ova\u2019s\u0131 aras\u0131na Bozda\u011flar (2.159m) girer. Bu k\u00fctle do\u011fu kesiminde g\u00fcneydeki Ayd\u0131n Da\u011flar\u0131\u2019yla birle\u015fir, bat\u0131 kesiminde ise Nif Da\u011f\u0131\u2019na (1.506m) ve kuzeydek Spil Da\u011f\u0131\u2019na (1.513m) ba\u011flan\u0131r. Daha g\u00fcneyde K\u00fc\u00e7\u00fck Menderes ve B\u00fcy\u00fck Menderes Ovalar\u0131 aras\u0131nda Ayd\u0131n Da\u011flar\u0131 (1.819m) uzan\u0131r. Bu da\u011flar bat\u0131ya do\u011fru b\u00fck\u00fcl\u00fcp incelenerek Samsun (Dilek) Da\u011f\u0131 (1.237m) \u00fczerinden kom\u015fu Sisam (Samos) Adas\u0131na ge\u00e7er. Geni\u015f bir alan\u0131 kaplayan B\u00fcy\u00fck Menderes Ova\u2019s\u0131 Mente\u015fe y\u00f6resi i\u00e7ine \u00c7ine ve Bozdo\u011fan Ovalar\u0131yla sokulur.En g\u00fczeydeki \u00e7ukur alan\u0131, Bodrum ve Dat\u00e7a yar\u0131madalar\u0131 aras\u0131nda yer alan G\u00f6kova K\u00f6rfezi\u2019dir.
\n Bat\u0131 Anadolu\u2019da yer alan ovalar, genellikle d\u00f6rd\u00fcnc\u00fc jeolojik zamanda meydana gelen epirojenik hareketlerle olu\u015fmu\u015ftur. Bu hareketler sonucunda baz\u0131 alanlar y\u00fckselmi\u015f (horst) ve bug\u00fcnk\u00fc da\u011fl\u0131k alanlar\u0131 meydana getirmi\u015f, baz\u0131 alanlar ise \u00e7\u00f6km\u00fc\u015f (graben) ve \u00e7\u00f6k\u00fcnt\u00fc alanlar\u0131 olu\u015fmu\u015ftur. Bu \u00e7\u00f6k\u00fcnt\u00fc alanlar\u0131n\u0131n akarsular taraf\u0131nda al\u00fcvyonlarla doldurulmas\u0131 sonucunda da g\u00fcn\u00fcm\u00fczdeki ovalar olu\u015fmu\u015ftur. B\u00f6lgemizdeki en \u00f6nemli ovalar ise Bak\u0131r\u00e7ay, Gediz, K\u00fc\u00e7\u00fck ve B\u00fcy\u00fck Menderes, Bal\u0131kesir ve Akhisar ovalar\u0131d\u0131r. 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.
\n Meri\u00e7 deltas\u0131, h\u0131zl\u0131 ilerleyen ta\u015fk\u0131n alanlar\u0131na sahip bir ovad\u0131r. Meri\u00e7 Irma\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. K\u00fc\u00e7\u00fck ve B\u00fcy\u00fck Menderes Deltalar\u0131 da birer \u00e7\u00f6k\u00fcnt\u00fc alan\u0131n\u0131n(graben) ucunda olu\u015fan birikinti ovalar\u0131d\u0131r. B\u00fcy\u00fck ve K\u00fc\u00e7\u00fck Menderes Irmaklar\u0131, Ege Denizi\u2019nin seviye de\u011fi\u015fikliklerine de ba\u011fl\u0131 olarak tarihi d\u00f6nemlerde h\u0131zla denizi doldurmu\u015ftur. \u00d6yle ki, \u0130lk\u00e7a\u011f\u2019da bir liman kenti olan Milet, B\u00fcy\u00fck Menderes\u2019in denizi doldurmas\u0131 ile bu g\u00fcn k\u0131y\u0131dan bir hayli ileride kalm\u0131\u015ft\u0131r.
\nB\u00f6lgenin \u0130\u00e7bat\u0131 Anadolu B\u00f6l\u00fcm\u00fc\u2019nde da\u011f s\u0131ralar\u0131 yerine aral\u0131kl\u0131 da dizileri g\u00f6r\u00fcl\u00fcr. Bu da\u011flar, g\u00fcneydo\u011fu-kuzeybat\u0131 do\u011frultusunda birka\u00e7 dizi olu\u015ftur. Bu dizilerden en do\u011fuda yer alan Emir Da\u011flar\u0131 (2.307m), T\u00fcrkmen (1.826m), Domani\u00e7 (1.845m) Da\u011flar\u0131 b\u00f6lge s\u0131n\u0131rlar\u0131 d\u0131\u015f\u0131ndaki Uluda\u011f\u2019a kadar uzan\u0131r. Bu da\u011flar dizisi bat\u0131da ayn\u0131 do\u011frultudaki Afyon-Karahisar-K\u00fctahya-Orhaneli \u00fczerinden ge\u00e7en bir \u00e7ukur alanla izlenir. Bu \u00e7ukur alan\u0131n bat\u0131s\u0131nda Kumalar (2.247m), Ah\u0131r(1.915m), Murat (2.309m), \u015eaphane (2.120m), Akda\u011f (2.089m), E\u011frig\u00f6z (1.931m) da\u011flar\u0131 yer al\u0131r. Bu dizinin daha bat\u0131s\u0131na gidildik\u00e7e geni\u015f bir plato uzan\u0131r. Gediz Ovas\u0131\u2019na dik yama\u00e7larla inen ve y\u00fcksekli\u011fi kuzeydo\u011fuda 1.000m\u2019yi a\u015fan bu platoya G\u00f6rdes-U\u015fak Plato\u2019su ad\u0131 verilir. Platonun g\u00fcney kenar\u0131ndaki Kula kenti \u00e7evresinde s\u00f6nm\u00fc\u015f volkan konileri ve yeni lav ak\u0131nt\u0131lar\u0131 g\u00f6r\u00fcl\u00fcr.
\n Ege Denizi\u2019ne d\u00f6k\u00fclen akarsular\u0131m\u0131z; Bat\u0131 Anadolu akarsular\u0131, geni\u015f \u00e7\u00f6k\u00fcnt\u00fc hendeklerine yerle\u015fmi\u015ftir. Bu \u00e7\u00f6k\u00fcnt\u00fc alanlar\u0131 boyunca bat\u0131ya do\u011fru akarak Ege Denizi\u2019ne d\u00f6k\u00fcl\u00fcrler. Denize ula\u015ft\u0131klar\u0131 alandaki koy ve k\u00f6rfezlerde geni\u015f delta ovalar\u0131 olu\u015fturmu\u015flard\u0131r. Bu akarsular b\u00f6lgemiz ve \u00fclkemiz tar\u0131m\u0131 i\u00e7in olduk\u00e7a b\u00fcy\u00fck de\u011fer ta\u015f\u0131r. Bunlar\u0131n ba\u015fl\u0131calr\u0131 Bak\u0131r\u00e7ay, Gediz, K\u00fc\u00e7\u00fck ve B\u00fcy\u00fckMenderes\u2019tir. <\/p>\n
\u0130klim<\/p>\n
Ege B\u00f6lgesi genellikle yazlar\u0131 s\u0131cak ve kurak, k\u0131\u015flar\u0131 \u0131l\u0131k ve ya\u011f\u0131\u015fl\u0131 olan Akdeniz ikliminin etkisi alt\u0131ndad\u0131r. Bu genel durum daha \u00e7ok Ege B\u00f6l\u00fcm\u00fc i\u00e7in ge\u00e7erlidir. \u0130\u00e7bat\u0131 Anadolu\u2019da ise denizden uzakl\u0131k ve y\u00fckselti nedenleriyle iklim ko\u015fullar\u0131nda de\u011fi\u015fiklik g\u00f6r\u00fcl\u00fcr. Kuzey kesimlerinde s\u0131k s\u0131k so\u011fuk bask\u0131nlar\u0131 g\u00f6r\u00fcl\u00fcr. Y\u0131ll\u0131k ortalama s\u0131cakl\u0131kta co\u011frafi enlemin etkisiyle g\u00fcneyden kuzeye ve y\u00fcksekli\u011fin etkisiyle bat\u0131dan do\u011fuya do\u011fru azalma g\u00f6r\u00fcl\u00fcr. En so\u011fuk ay genellikle ocak, en s\u0131cak ay ise temmuz ay\u0131 olarak tespit edilmi\u015ftir.
\nEge Denizi k\u0131y\u0131lar\u0131 boyunca tam bir Akdeniz ya\u011f\u0131\u015f rejimi g\u00f6r\u00fcl\u00fcr. Yazlar kurak ge\u00e7er; ya\u011f\u0131\u015flar k\u0131\u015f aylar\u0131nda toplanm\u0131\u015ft\u0131r. A\u015fa\u011f\u0131 yukar\u0131 b\u00fct\u00fcn meteoroloji istasyonlar\u0131 da y\u0131ll\u0131k ortalama ya\u011f\u0131\u015f tutar\u0131 500 mm\u2019nin \u00fcst\u00fcnde, genellikle de 1000 mm\u2019nin alt\u0131nda olarak saptam\u0131\u015flard\u0131r. <\/p>\n
Bitki \u00d6rt\u00fcs\u00fc <\/p>\n
Ege B\u00f6lgesi\u2019nde k\u0131y\u0131dan itibaren 600-800 m y\u00fcksekliklere kadar maki topluluklar\u0131 ile akr\u0131\u015f\u0131k olarak k\u0131z\u0131l\u00e7am ormanlar\u0131 g\u00f6r\u00fcl\u00fcr. Makilerin c\u0131l\u0131zla\u015ft\u0131\u011f\u0131 ve toprak \u00f6rt\u00fcs\u00fcn\u00fcn inceldi\u011fi alanlarda, \u00e7o\u011funlukla dikenli \u00e7al\u0131lardan olu\u015fan ve \u201cgarik\u201d ad\u0131 verilen bir bitki toplulu\u011fu g\u00f6r\u00fcl\u00fcr ve genellikle \u0130zmir civar\u0131 ile Karaburun yar\u0131madas\u0131 ve Bodrum civar\u0131nda yayg\u0131nd\u0131r. Orman alanlar\u0131 Ege B\u00f6l\u00fcm\u00fc\u2019n\u00fcn al\u00e7ak kesimlerinde makiliklerin, \u0130\u00e7bat\u0131 Anadolu\u2019da ise step g\u00f6r\u00fcn\u00fc\u015fl\u00fc alanlar\u0131 \u00fcst\u00fcnde yer al\u0131r. Ormanlar\u0131n alt basamaklar\u0131nda \u00e7e\u015fitli me\u015felere rastlan\u0131r;i\u011fne yaprakl\u0131 ormanlar aras\u0131nda en yayg\u0131n t\u00fcr k\u0131z\u0131l\u00e7am ve kara\u00e7amd\u0131r. Ayr\u0131ca Kozak Da\u011f\u0131\u2019nda f\u0131st\u0131k \u00e7am\u0131 yayg\u0131nd\u0131r. T\u00fcrkiye\u2019nin en \u00f6nemli \u00e7amf\u0131st\u0131\u011f\u0131 \u00fcretim alan\u0131d\u0131r. B\u00fct\u00fcn k\u0131y\u0131 kesimlerde zeytinliklere rastlan\u0131r. Kuzeyden gelen so\u011fuk hava etkilerinden korunan turun\u00e7giller b\u00f6lgenin g\u00fcneyine s\u0131\u011f\u0131nm\u0131\u015ft\u0131r. Ayr\u0131ca kekik, ada\u00e7ay\u0131, lavanta \u00e7i\u00e7e\u011fi gibi kokulu bitkiler ve Akdeniz iklimine uyan kakt\u00fcsler, frank inciri gibi bitkilerde yayg\u0131nd\u0131r. Maki t\u00fcrleri aras\u0131nda \u00e7e\u015fitli me\u015fe t\u00fcrleri (p\u0131rnal me\u015fesi, palamut me\u015fesi) kocayami\u015f, mersin a\u011fac\u0131, defne, yabani zeytinlere rastlan\u0131r.<\/p>\n
Kentler Ve \u00d6zellikleri<\/p>\n
B\u00f6lgenin en kalabal\u0131k n\u00fcfusl\u0131 kenti \u0130zmir; \u0130stanbul ve Ankara\u2019dan sonra T\u00fcrkiye\u2019nin \u00fc\u00e7\u00fcnc\u00fc b\u00fcy\u00fck yerle\u015fme merkezidir. Karalar i\u00e7ine derin bi\u00e7imde sokulan ve ayn\u0131 ad\u0131 ta\u015f\u0131yan bir k\u00f6rfezin bitim yerinde kurulmu\u015f olan \u0130zmir, co\u011frafi konumu sayesinde Bat\u0131 Anadolu\u2019da \u00e7ok geni\u015f bir alan\u0131n ticaret liman\u0131 (\u0130zmir\u2019e gelen mallar, gemilere y\u00fcklenmeden \u00f6nce kentte i\u015flenir) ve \u00fclkemizin \u0130stanbul \u2018dan sonra ikinci b\u00fcy\u00fck ticaret merkezi haline gelmi\u015ftir. Kent \u0130zmir K\u00f6rfezi bitiminde bir ay\u00e7e (hilal) bi\u00e7iminde yay\u0131l\u0131r; kuzeyde Bostanl\u0131\u2019dan ba\u015flayan bu ay\u00e7e, 27 km\u2019yi a\u015fk\u0131n bir e\u011fri olu\u015fturarak, k\u00f6rfezin g\u00fcneyinde \u00dc\u00e7kuyular\u2019da sona erer; daha sonra, Bal\u00e7ova, \u0130nciralt\u0131 gibi yerle\u015fmelerde bat\u0131ya do\u011fru uzan\u0131r.
\n Eski\u00e7a\u011f\u2019da \u0130onia\u2019dan gelen g\u00f6\u00e7menlerin Bayrakl\u0131 ve Bornova aras\u0131nda, o zamanlar deniz k\u0131y\u0131s\u0131nda bulunan bir tepe \u00fcst\u00fcnde kurduklar\u0131 san\u0131lan kent (Smyrna) Pagoa Da\u011f\u0131 (Kadife Kale) ete\u011finde ikinci kez kurulmu\u015f, Roma ve Bizans egemenliklerinden sonra 1424\u2019te Osmanl\u0131 topraklar\u0131na kat\u0131lm\u0131\u015f, 1919\u2019da Yunanl\u0131lar taraf\u0131ndan i\u015fgal edilmi\u015f, 1922\u2019de de kurtar\u0131lm\u0131\u015ft\u0131r.
\n B\u00f6lgenin ikinci b\u00fcy\u00fck kenti Denizli\u2019nin topraklar\u0131n\u0131n b\u00fcy\u00fck bir b\u00f6l\u00fcm\u00fc, Pamukkale havzas\u0131nda ve \u00e7evresindeki tepelik, da\u011fl\u0131k alanda yer al\u0131r. Selefkilerden Antiokhos 2\u2019nin kar\u0131s\u0131n\u0131n ad\u0131 (Laokide) ad\u0131 verilerek kurulan kent, Selefkiler ve Bizansl\u0131lardan sonra da g\u00fcn\u00fcm\u00fczdeki yerine ta\u015f\u0131nm\u0131\u015f, yeni kuruldu\u011fu yerde bulunan Do\u011fuzlu K\u00f6y\u00fc\u2019n\u00fcn ad\u0131 zamanla Denizli\u2019ye \u00e7evrilmi\u015ftir.
\n B\u00f6lgenin \u00fc\u00e7\u00fcnc\u00fc, \u0130\u00e7bat\u0131 Anadolu B\u00f6l\u00fcm\u00fc\u2019\u00fcnde ba\u015fl\u0131ca kenti olan K\u00fctahya, Eski\u00e7a\u011f\u2019da, geni\u015f bir ovan\u0131n kenar\u0131nda y\u00fckselen Yellice Da\u011f\u0131 eteklerinde, Hisar Tepesi ad\u0131 verilen yerde kurulmu\u015f, Orta\u00e7a\u011f\u2019da Bizans d\u00f6neminde Kotyaion ad\u0131yla olduk\u00e7a geli\u015fmi\u015ftir. G\u00fcn\u00fcm\u00fczde hisar kal\u0131nt\u0131lar\u0131n\u0131n bulundu\u011fu tepenin eteklerinden kuzeydeki ovaya do\u011fru yay\u0131lan kentin etkinlik merkezi, Hisar tepesi \u00f6n\u00fcnde yer al\u0131r. \u00d6nemli sanayi ve havac\u0131l\u0131k merkezidir. B\u00f6lgenin d\u00f6rd\u00fcnc\u00fc b\u00fcy\u00fck kenti Manisa, Eski\u00e7a\u011f\u2019da ayn\u0131 ad\u0131 ta\u015f\u0131yan da\u011f\u0131n (Magnesia) kuzey eteklerinde kurulmu\u015f, Roma d\u00f6neminde geli\u015fmi\u015f, Bizansl\u0131lardan 14.yy ba\u015flar\u0131nda Saruhano\u011fullar\u0131\u2019na k\u0131sa bir s\u00fcre sonra da Osmanl\u0131lara ge\u00e7mi\u015f, bir s\u00fcre \u015fehzadelerin valilik yapt\u0131klar\u0131 bir merkez olmu\u015f ve \u00f6nemli an\u0131tlarla s\u00fcslenmi\u015ftir.<\/p>\n
\u0130KT\u0130SAT VE SANAY\u0130<\/p>\n
TARIM: Ege B\u00f6lgesi\u2019nde n\u00fcfusun \u00e7o\u011funlu\u011fu iklim toprak ko\u015fullar\u0131 ve ula\u015f\u0131m kolayl\u0131klar\u0131n\u0131n da elveri\u015flili\u011fiyle ge\u00e7imini tar\u0131mdan sa\u011flar. Ege b\u00f6l\u00fcm\u00fcnde Akdeniz iklimine uygun baz\u0131 bitkiler (zeytin,\u00fcz\u00fcm, vb.) a\u011f\u0131r basar. Ege b\u00f6l\u00fcm\u00fcnden, \u0130\u00e7bat\u0131 Anadolu b\u00f6l\u00fcm\u00fcne ge\u00e7ildik\u00e7e, tar\u0131m\u0131n niteli\u011fi de\u011fi\u015fir; tah\u0131l ekimi artar ve hayvanc\u0131l\u0131k ge\u00e7imde daha \u00f6nemli yer tutar. Tah\u0131l ekiminde bu\u011fday ba\u015fta gelir, onu arpa ve m\u0131s\u0131r izler. Bu\u011fday \u00f6zellikle Afyon ve Denizli\u2019de \u00fcretilir bu illeri \u0130zmir, Ayd\u0131n ve Mu\u011fla izler. Arpa ise Afyon ve Manisa illerinde, m\u0131s\u0131r\u0131n da ba\u015fl\u0131ca ekim alan\u0131 Manisa\u2019d\u0131r. Pirin\u00e7 ekimine ovalarda az miktarda yer verilir. B\u00f6lgede ya\u015f ve kuru sebze \u00fcretimine de \u00f6nem verilir. \u0130klim ko\u015fullar\u0131 uygun oldu\u011fu i\u00e7in, turfanda sebze (domates, fasulye vb.) yeti\u015ftirilerek \u00f6b\u00fcr b\u00f6lgelere yollan\u0131r. So\u011fan ve patates ekimi yayg\u0131nd\u0131r; baklagillerden en \u00e7ok nohut ekilir. Kavun ve karpuz \u00fcretimi de yayg\u0131n bi\u00e7imde yap\u0131lmaktad\u0131r.
\n B\u00f6lgede yati\u015ftirilen sanayi bitkileri aras\u0131nda t\u00fct\u00fcn, pamuk, susam, keten ve \u015fekerpancar\u0131 ba\u015f s\u0131ralarda yer al\u0131r. Edrmit K\u00f6rfezi k\u0131y\u0131lar\u0131 ya\u011f zeytini \u00fcretimi kesir a\u011fa\u00e7 say\u0131s\u0131 bak\u0131m\u0131ndan ba\u015fta gelir bak\u0131m\u0131ndan \u00f6nemlidir. \u00dcz\u00fcm ba\u011flar\u0131na da b\u00f6lgenin her yerinde rastlan\u0131r. \u00dcz\u00fcm ayr\u0131ca \u015farap ve pekmez yap\u0131m\u0131nda da kullan\u0131l\u0131r. Kuru \u00fcz\u00fcm \u0130zmir y\u00f6resinde, k\u0131\u015f so\u011funa dayanamayan incir ise k\u0131y\u0131 kesimlerde yeti\u015fir. \u00dclkemizdeki incir a\u011fa\u00e7lar\u0131n\u0131n yakla\u015f\u0131k olarak %81\u2019i Ege B\u00f6lgesi\u2019ndedir. Turun\u00e7giller b\u00f6lgenin \u00f6zellikle g\u00fcney kesiminde yeti\u015fir; Bodrum\u2019da mandalina; Ayd\u0131n ve Nazilli aras\u0131nda portakal yeti\u015fir. <\/p>\n
HAYVANCILIK: Ege b\u00f6lgesinde hayvanc\u0131l\u0131k \u00e7ok geli\u015fmemi\u015ftir. \u00dcstelik yak\u0131n d\u00f6nemde otlaklar\u0131n daralmas\u0131 nedeniyle, hayvan say\u0131s\u0131nda azalma g\u00f6zlenmektedir. K\u0131y\u0131 kesimde daha \u00e7ok k\u0131l ke\u00e7isi, tiftik ke\u00e7isi ve koyun, i\u00e7 kesimlerde s\u0131\u011f\u0131r ve manda besicili\u011fi yayg\u0131nd\u0131r. Bal\u0131k\u00e7\u0131l\u0131k ise eski \u00f6nemini kaybetmi\u015ftir \u00f6zellikle \u0130zmir K\u00f6rfezi\u2019nin sular\u0131n\u0131 pis olmas\u0131ndan dolay\u0131. Yine eski \u00f6nemini yitirmi\u015f olmakla birlikte Bodrum k\u0131y\u0131lar\u0131nda s\u00fcnger avc\u0131l\u0131\u011f\u0131 yap\u0131lmaktad\u0131r. <\/p>\n
YERALTI KAYNAKLARI: Ege B\u00f6lge\u2019si yeralt\u0131 kaynaklar\u0131 bak\u0131m\u0131ndan olduk\u00e7a zengindir; ama madenlerin bir\u00e7o\u011fu \u0130lk\u00e7a\u011f\u2019dan beri i\u015fletildi\u011finden, t\u00fckenmi\u015ftir. B\u00f6lgede yayg\u0131n olan linyit yataklar\u0131, K\u00fctahya ve Soma y\u00f6relerinde toplanm\u0131\u015ft\u0131r. K\u00fctahya y\u00f6resindeki linyitlerin i\u015fletilmesi K\u00fctahya-Bal\u0131kesir demiryolunun yap\u0131lmas\u0131yla kolayla\u015fm\u0131\u015ft\u0131r. \u0130\u015fletilen yataklardan biri De\u011firmisaz havzas\u0131d\u0131r; Tun\u00e7bilek b\u00f6lgesindeki yataklarsa daha \u00f6nemlidir. Soma\u2019dan da olduk\u00e7a iyi nitelikli linyit k\u00f6m\u00fcr\u00fc \u00e7\u0131kar\u0131lmaktad\u0131r. Demire kat\u0131larak \u00e7elik elde etmeye yarayan krom, K\u00fctahya ve Bal\u0131kesir aras\u0131ndaki yataklardan \u00c7ard\u0131\u2019da \u00e7\u0131kar\u0131l\u0131rken, g\u00fcn\u00fcm\u00fczde bu ocak t\u00fckendi\u011fi i\u00e7in b\u0131rak\u0131lm\u0131\u015f, onun yerine Da\u011fard\u0131 ve Dursunbey dolaylar\u0131ndaki ocaklar i\u015fletilmeye a\u00e7\u0131lm\u0131\u015ft\u0131r. B\u00f6lgedeki \u00e7ok say\u0131da demir yata\u011f\u0131n\u0131n ba\u015fl\u0131calar\u0131 Edremit y\u00f6resinde, Ayval\u0131k\u2019\u0131n g\u00fcneyinde ve Simav \u00e7evresinde yer al\u0131r; Sel\u00e7uk, U\u015fak ve Tire\u2019de z\u0131mpara yataklar\u0131 i\u015fletilir. Ayr\u0131ca \u00e7e\u015fitli mermer, civa, bor, manganez yataklar\u0131 vard\u0131r. T\u00fcrkiye\u2019nin en \u00f6nemli maden suyu Afyon dolaylar\u0131nda K\u0131z\u0131lay taraf\u0131ndan i\u015fletilmekte \u0130zmir\u2019in \u00c7amalt\u0131 tuzlalar\u0131ndan da T\u00fcrkiye\u2019nin toplam tuz \u00fcr\u00fcn\u00fcn 3\/5\u2019\u00fc elde edilmektedir.<\/p>\n
SANAY\u0130 ETK\u0130NL\u0130KLER\u0130: Ege b\u00f6lgesi T\u00fcrkiye\u2019de Marmara B\u00f6lgesi\u2019nden sonra ikinci s\u0131rada yer al\u0131r. \u00d6zellikle \u0130zmir\u2019de toplanm\u0131\u015f olan ba\u015fl\u0131ca sanayi kollar\u0131 aras\u0131nda dokumac\u0131l\u0131k, makine ve madeni e\u015fya yap\u0131m\u0131, besin sanayisi (un, makarna, konserve fabrikalar\u0131), t\u00fct\u00fcn i\u015fletmecili\u011fi say\u0131labilir. Pamuklu, dokumac\u0131l\u0131k, \u0130zmir\u2019in yan\u0131 s\u0131ra Ayd\u0131n, Nazilli, Denizli, ve U\u015fak\u2019ta geli\u015fmi\u015ftir. Ya\u011f sanayisi tesisleri \u00f6zellikle Edremit-Ayval\u0131k y\u00f6resinde, \u015feker fabrikalar\u0131 U\u015fak, K\u00fctahya ve Afyon\u2019da yer al\u0131r. U\u015fak, Kula, G\u00f6rdes ve Simav\u2019da hal\u0131c\u0131l\u0131k geli\u015fmi\u015ftir.<\/p>\n
ULA\u015eIM: Ege B\u00f6lgesi ula\u015f\u0131m bak\u0131m\u0131ndan T\u00fcrkiye\u2019nin i\u015flek b\u00f6lgelerindendir. Do\u011fu-bat\u0131 do\u011frultulu vadi oluklar\u0131, karayollar\u0131n\u0131n i\u00e7 kesimlere kadar ula\u015fmas\u0131na olanak verir. B\u00f6lge \u00e7e\u015fitli demiryolu hatlar\u0131yla \u00f6b\u00fcr b\u00f6lgelere ba\u011flan\u0131r. (\u00dclkemizde ilk demiryolu hatt\u0131 olan \u0130zmir-Ayd\u0131n hatt\u0131, 1856\u2019da Ege B\u00f6lgesi\u2019nde hizmete girmi\u015ftir). Karayollar\u0131 ve demiryollar\u0131, \u0130\u00e7bat\u0131 Anadolu\u2019da Afyon ve K\u00fctahya\u2019da d\u00fc\u011f\u00fcmlenir. Denizyollar\u0131 a\u00e7\u0131s\u0131ndan \u0130zmir liman\u0131 (ticaret etkinlikleri bu limanda toplanm\u0131\u015ft\u0131r) d\u0131\u015f\u0131nda \u00f6nemli liman yoktur. Turizm bak\u0131m\u0131ndansa Bodrum, Ku\u015fadas\u0131, G\u00fcll\u00fck, Dat\u00e7a ve Marmaris limanlar\u0131 \u00f6nemlidir. \u0130zmir d\u00fczenli hava seferleriyle de \u0130stanbul ve Ankara\u2019yla ba\u011flant\u0131 kurmaktad\u0131r. <\/p>\n
DO\u011eAL VE TAR\u0130HSEL G\u00dcZELL\u0130KLER, TUR\u0130ZM OLANAKLARI<\/p>\n
Ege B\u00f6lgesi\u2019nin turizm bak\u0131m\u0131ndan zengin bir do\u011fal ve k\u00fclt\u00fcrel yap\u0131s\u0131 vard\u0131r. Da\u011flar\u0131n k\u0131y\u0131ya dik olarak uzanmas\u0131, son derece girintili \u00e7\u0131k\u0131nt\u0131l\u0131 bir k\u0131y\u0131 \u015feridi yaratm\u0131\u015ft\u0131r ( Ege denizi k\u0131y\u0131lar\u0131n\u0131n toplam uzunlu\u011fu 593km\u2019dir) ve do\u011fal kumsallar\u0131n denize girmeye son derece elveri\u015fli olmalar\u0131n\u0131n yan\u0131 s\u0131ra, y\u00fcksek k\u0131y\u0131larda da \u00e7ekici g\u00f6r\u00fcn\u00fcmleriyle ilgi toplarlar. Ayr\u0131ca y\u00f6redeki b\u00fck (Akb\u00fck, G\u00f6k\u00e7eler b\u00fck\u00fc, De\u011firmen b\u00fck\u00fc, Palamut b\u00fck\u00fc, Karg\u0131b\u00fck, vb.), \u00f6zellikle son y\u0131llarda iyice yayg\u0131nla\u015fan yat turizminde, yatlara do\u011fal liman i\u015flevi g\u00f6ren; \u201cMavi Yolculuk\u201d ad\u0131yla yayg\u0131nla\u015fan ve k\u0131y\u0131n\u0131n Ku\u015fadas\u0131\u2019ndan Antalya\u2019ya kadar olan koylar\u0131n\u0131 dola\u015fan yat turizmi, b\u00f6lgeye \u00f6nemli miktarda yerli ve yabanc\u0131 turist \u00e7ekmektedir; \u00fclkemizin ba\u015fl\u0131ca \u00fc\u00e7 yat liman\u0131 (Ku\u015fadas\u0131, \u00c7e\u015fme ve Bodrum yat limanlar\u0131) da bu k\u0131y\u0131lardad\u0131r.
\n Ege B\u00f6lgesi\u2019nde egemen olan Akdeniz ikliminin yumu\u015fak niteli\u011fi de, turizme son derece elveri\u015flidir: K\u0131\u015flar\u0131n ge\u00e7 ge\u00e7mesi, yaz\u0131n g\u00fcne\u015flenme olanaklar\u0131, deniz suyu s\u0131cakl\u0131klar\u0131n\u0131n uygunlu\u011fu \u00e7ok say\u0131da turist \u00e7eker. Ege Denizi\u2019nde deniz suyu s\u0131cakl\u0131klar\u0131, kuzeyden g\u00fcneye do\u011fru artar ve denize girme s\u00fcresi de bu do\u011frultuda uzar: K\u0131y\u0131larda kuzeyden \u0130zmir\u2019e kadar y\u0131lda be\u015f ay olan denize girme s\u00fcresi, Ku\u015fadas\u0131\u2019ndan sonra artmaya ba\u015flar ve Bodrum\u2019da sekiz ay\u0131 bulur.
\n Ege B\u00f6lgesi\u2019nde yer alan kapl\u0131ca ve i\u00e7mecelerde sa\u011fl\u0131k turizmi a\u00e7\u0131s\u0131ndan da ilgi g\u00f6rmektedir: Denizli\u2019de Karahay\u0131t ve Pamukkale kapl\u0131calar\u0131; \u0130zmir\u2019de Bal\u00e7ova, Dikili, Davutlar, \u00c7e\u015fme ve \u015eifne kapl\u0131calar\u0131; Seferhisar\u2019\u0131n g\u00fcneyinde Do\u011fanbey kapl\u0131cas\u0131; K\u00fctahya\u2019da Simav-Gediz, Yoncal\u0131, Harlek ve Murat Da\u011f\u0131 kapl\u0131calar\u0131 ve i\u00e7meceleri ile Eynal kapl\u0131calar\u0131d\u0131r., Manisa\u2019da Kur\u015funlu kapl\u0131cas\u0131 ve Sart kapl\u0131cas\u0131; Afyon Sand\u0131kl\u0131\u2019da Sand\u0131kl\u0131, Gazl\u0131g\u00f6l ve H\u00fcdayi kapl\u0131calar\u0131 ve i\u00e7meceleri yer al\u0131r; \u0130zmir\u2019de Urla i\u00e7meceleri. \u00d6zellikle Pamukkale s\u0131caksu kaynaklar\u0131, \u00e7ok eski d\u00f6nemlerden bu yana bilinmekte ve ilgi \u00e7ekmektedir. Pamukkale\u2019nin \u00f6zelliklerinden biri de travertenleridir: S\u0131cak maden sular\u0131, a\u015fa\u011f\u0131 d\u00f6k\u00fcld\u00fckleri da\u011f\u0131n yama\u00e7lar\u0131n\u0131 beyaz traverten tara\u00e7alar\u0131 haline getirmi\u015ftir (y\u00f6reye Pamukkale ad\u0131, suyun kapsad\u0131\u011f\u0131 kalsiyum karbonat nedeniyle olu\u015fan beyazl\u0131ktan \u00f6t\u00fcr\u00fc verilmi\u015ftir). Travertenleri sayesinde \u00e7ok say\u0131da turisti \u00e7eker.
\n B\u00f6lgede do\u011fal ve tarihsel g\u00fczellikleri korumak amac\u0131yla iki Ulusal park d\u00fczenlenmi\u015ftir. Bunlardan Dilek Yar\u0131madas\u0131 Ulusal Park\u0131, Ayd\u0131n ilinin Ku\u015fadas\u0131 ve S\u00f6ke il\u00e7eleri s\u0131n\u0131rlar\u0131 i\u00e7inde yer al\u0131r ve Akdeniz bitki \u00f6rt\u00fcs\u00fcn\u00fcn en g\u00fczel \u00f6rneklerini kapsar. Ayr\u0131ca \u0130onial\u0131lar\u2019dan kalma kal\u0131nt\u0131lar, arkeoloji a\u00e7\u0131s\u0131ndan \u00f6nemlidir. Manisa ilinin yama\u00e7lar\u0131na yaslad\u0131\u011f\u0131 Spilda\u011f\u0131 \u00fcst\u00fcndeki Spilda\u011f\u0131 Ulusal Park\u0131\u2019ysa, 1500m\u2019yi bulan y\u00fckseltisiyse yaz\u0131n Manisa\u2019n\u0131n s\u0131ca\u011f\u0131ndan ka\u00e7anlara bar\u0131nak olu\u015fturur (Osmanl\u0131lar d\u00f6neminde bir devre ad\u0131n\u0131 veren Manisa lalesi, burada do\u011fal olarak yeti\u015fir). Ayr\u0131ca bu ulusal park da, Eski\u00e7a\u011f kal\u0131nt\u0131lar\u0131n\u0131 kapsar. B\u00f6lgenin \u00e7e\u015fitli illerinde d\u00fczenlenmi\u015f Ormani\u00e7i Dinlenme Yeri de, yerli ve yabanc\u0131 turistlere \u00e7e\u015fitli hizmetler sunar.
\n Ege B\u00f6lgesi, arkeoloji ve tarih \u00f6zellikleriyle de bol bol turist \u00e7eker.: \u0130zmir\u2019de Efes ve Bergama; Denizli\u2019de Pamukkale (Hierapolis); Ayd\u0131n\u2019da Priene, Miletos, Didim, Afrodisias, Dat\u00e7a\u2019da Knidos: Bodrum\u2019da Halikarnassos; Manisa\u2019da Sart y\u0131k\u0131nt\u0131lar\u0131. D\u00fcnyan\u0131n yedi harikas\u0131ndan ikisi Ege B\u00f6lgesi\u2019ndedir (Efes Artemis tap\u0131na\u011f\u0131 ve Halikarnassos Mausoleion\u2019u). Ayr\u0131ca, Sel\u00e7uk\u2019ta Meryem Ana\u2019n\u0131n Evi ve Sen Jan Kilisesi, Didim\u2019de Apollon tap\u0131na\u011f\u0131, \u00e7ok say\u0131da yabanc\u0131 turist \u00e7ekmektedir. G\u00fcn\u00fcm\u00fczde Ege Denizi k\u0131y\u0131s\u0131ndaki Ak\u00e7ay, \u00d6ren, Ayval\u0131k, Fo\u00e7a, \u00c7e\u015fme, Ku\u015fadas\u0131, Didim, G\u00fcll\u00fck, Bodrum, Dat\u00e7a, Marmaris gibi yerle\u015fim merkezlerimiz, yaz mevsiminde ger\u00e7ek birer turizm oda\u011f\u0131 haline gelmi\u015ftir. <\/p>\n
EGE DEN\u0130Z\u0130<\/p>\n
Kuzeyden g\u00fcneye yakla\u015f\u0131k 660km uzan\u0131r; geni\u015fli\u011fi kuzeyde 270, ortada 150, g\u00fcneyde ise 400km kadard\u0131r. Balkan yar\u0131madas\u0131n\u0131n do\u011fu b\u00f6l\u00fcm\u00fc ile Anadolu aras\u0131nda yer alan deniz. \u00c7anakkale Bo\u011faz\u0131 arac\u0131l\u0131\u011f\u0131yla Marmara Denizi\u2019ne ve Karadeniz\u2019e ba\u011flanan Ege Denizi\u2019i y\u00fcz\u00f6l\u00e7\u00fcm\u00fc 214000km2\u2019dir.
\nEge Denizi, yak\u0131n bir ge\u00e7mi\u015fte \u201cAegeis\u201d ya da \u201cEgeid\u201d ad\u0131 verilen bir kara par\u00e7as\u0131n\u0131n, b\u00fcy\u00fck bir b\u00f6l\u00fcm\u00fcn\u00fcn sular alt\u0131nda kalmas\u0131yla olu\u015fmu\u015ftur (ad\u0131 da buradan gelir); \u00fcst\u00fcndeki adalar\u0131n \u00e7oklu\u011fu nedeniyle \u201cAdalar Denizi\u201ddiye an\u0131l\u0131r. K\u0131y\u0131lar son derece girintitli \u00e7\u0131k\u0131nt\u0131l\u0131d\u0131r.
\n Ege\u2019de gelgit \u00f6nemsizdir ve yol a\u00e7t\u0131\u011f\u0131 d\u00fczey geni\u015fli\u011fi ancak baz\u0131 dar bo\u011fazlarda, r\u00fczgarlarla meydana gelen y\u0131\u011f\u0131lmalar\u0131n da etkisiyle 30-40cm\u2019yi bulur. Adalar aras\u0131ndaki baz\u0131 dar ve dolamba\u00e7l\u0131 bo\u011fazlar \u015fiddetli ve karma\u015f\u0131k yerel ak\u0131nt\u0131lara neden olur. Bunlar\u0131n en \u00fcnl\u00fcs\u00fc E\u011fribo\u011faz K\u00f6rfezi\u2019nde g\u00f6r\u00fcl\u00fcr.
\nEge Denizi\u2019nde, kuzeyde Saros K\u00f6rfezi\u2019nden ba\u015flayarak g\u00fcneye do\u011fru \u201cS\u201d bi\u00e7iminde uzanan, taban\u0131n\u0131n derinli\u011fi yer yer 1000m\u2019yi a\u015fan bir oluk yer al\u0131r. Ege Denizi\u2019nde \u00e7ok say\u0131da ada (toplam y\u00fcz\u00f6l\u00e7\u00fcmleri yakla\u015f\u0131k olarak 23000km2 olan bu adalar, her yana serpilmi\u015f gibi g\u00f6r\u00fcnmelerine kar\u015f\u0131n, belli bir d\u00fczen ve grupla\u015fma g\u00f6sterirler.
\n Ege Denizi \u00fcst\u00fcnde egemen olan Akdeniz iklimi, bu b\u00fcy\u00fck su k\u00fctlesinin etkisiyle baz\u0131 de\u011fi\u015fikliklere u\u011frar: Ege Denizi\u2019nin etkisi, donlu g\u00fcnlerin say\u0131s\u0131n\u0131 azalt\u0131r. Denizi suyu s\u0131cakl\u0131klar\u0131 da genelde kuzeyden g\u00fcneye do\u011fru artar. Bu art\u0131\u015f k\u0131\u015f\u0131n daha \u00e7ok belirlidir. K\u0131y\u0131 ve adalarda k\u0131\u015flar\u0131 ya\u011f\u0131\u015fl\u0131 bir Akdeniz iklimi g\u00f6r\u00fcl\u00fcr.
\n Ege Denizi\u2019nde y\u0131ll\u0131k ya\u011f\u0131\u015f tutar\u0131 kuzeyden g\u00fcneye gidildik\u00e7e azal\u0131r. Ya\u011f\u0131\u015flar genellikle k\u0131\u015f aylar\u0131nda toplanm\u0131\u015ft\u0131r. Kom\u015fu karalarda oldu\u011fu gibi, Ege Denizi alan\u0131nda da yazlar \u00e7ok kurakt\u0131r. Yaz\u0131n Ege Denizi\u2019nin her yan\u0131nda, kuzeyden ve kuzeydo\u011fudan \u201cetezyen\u201d ad\u0131 verilen \u015fiddetli bir r\u00fczgar eser. Ege Denizi, biyoloji ve hidroloji \u00f6zellikleri bak\u0131m\u0131ndan Karadeniz ile Akdeniz aras\u0131nda bir ge\u00e7i\u015f alan\u0131 olu\u015fturur.
\n \u00c7anakkale Bo\u011faz\u0131\u2019ndan \u00fcst ak\u0131nt\u0131s\u0131yla gelen ve besin tuzlar\u0131, oksijen ve plankton bak\u0131m\u0131ndan zengin olan Karadeniz sular\u0131, kuzeydeki bal\u0131k ya\u015fam\u0131n\u0131 olumlu y\u00f6nde etkiler. Ege Denizi, oksijen bak\u0131m\u0131ndan zengin olmas\u0131na kar\u015f\u0131n, fosfat ve nitrat bak\u0131m\u0131ndan yoksuldur. Bu y\u00fczden g\u00fcney b\u00f6l\u00fcm\u00fc, d\u00fcnyan\u0131n bal\u0131k bak\u0131m\u0131ndan en yoksul denizlerindendir.
\n Son y\u0131llarda Ege Denizi\u2019nde, denzi kirlenmesi ve \u00f6teki konulardaki bilimsel ara\u015ft\u0131rmalar yo\u011funla\u015fm\u0131\u015ft\u0131r. <\/p>\n","protected":false},"excerpt":{"rendered":"
Ege B\u00f6lgesi 85.000km2 dolay\u0131ndaki y\u00fcz\u00f6l\u00e7\u00fcm\u00fcyle T\u00fcrkiye topraklar\u0131n\u0131n yakla\u015f\u0131k %11\u2019ini kaplayan, kuzeyde Marmara B\u00f6lgesi\u2019ne, do\u011fuda \u0130\u00e7 Anadolu B\u00f6lgesi\u2019ne, g\u00fcneydo\u011fuda Akdeniz B\u00f6lgesi\u2019ne kom\u015fu olan b\u00f6lgemiz bat\u0131da da Ege Denizi\u2019yle \u00e7evrilidir (ad\u0131n\u0131 kom\u015fu oldu\u011fu denizden al\u0131r). Marmara B\u00f6lgesi\u2019yle olan s\u0131n\u0131r\u0131 bat\u0131da Baba Burnu\u2019ndan ba\u015flayarak Edremit K\u00f6rfezi\u2019nin kuzeyinde y\u00fckselen Kaz Da\u011f\u0131\u2019na uzan\u0131r. \u0130\u00e7 Anadolu B\u00f6lgesi\u2019yle olan s\u0131n\u0131r\u0131 ise \u0130n\u00f6n\u00fc\u2019n\u00fcn …<\/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":[2921,2926,2919,2924,2923,2793,2925,2920,2922],"class_list":["post-979","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-akdeniz","tag-bitki-ortusu","tag-ege-bolgesi","tag-graben","tag-horst","tag-ic-anadolu","tag-iklim","tag-marmara","tag-nufus"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/979","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=979"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/979\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=979"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=979"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=979"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}