Hatay ve \u00e7evresi yo\u011fun tektonizmaya maruz kald\u0131\u011f\u0131ndan yery\u00fcz\u00fc \u015fekilleri a\u00e7\u0131s\u0131ndan \u00e7e\u015fitlilik g\u00f6sterir. Ba\u015fl\u0131ca y\u00fczey \u015fekilleri; da\u011f, plato ve ovalardan olu\u015fur. En \u00f6nemli da\u011fl\u0131k alan, Amik Ovas\u0131\u2019n\u0131n i\u00e7inde yer ald\u0131\u011f\u0131 graben alan\u0131 ile Akdeniz aras\u0131nda adeta bir set gibi y\u00fckselen ve kuzeydo\u011fu-g\u00fcneybat\u0131 y\u00f6n\u00fcnde uzan\u0131\u015f g\u00f6steren Amanos Da\u011flar\u0131\u2019d\u0131r. Bu da\u011flar\u0131n il i\u00e7indeki en y\u00fcksek noktas\u0131n\u0131 Hassa\u2019n\u0131n bat\u0131s\u0131ndaki M\u0131\u011f\u0131r Tepe\u2019si (2240 m) olu\u015fturur.<\/p>\n\n\n\n
Amanos Da\u011flar\u0131\u2019n\u0131n do\u011fusunda, da\u011flar\u0131n uzan\u0131\u015f\u0131na paralel graben alan\u0131 yer al\u0131r. Bu grabenin taban\u0131nda Amik Ovas\u0131 bulunur. Bu ova ilin en \u00f6nemli ve en verimli tar\u0131m alan\u0131n\u0131 olu\u015fturur. \u0130ldeki di\u011fer \u00f6nemli ovalar ise; \u0130skenderun k\u00f6rfezinin do\u011fu ve kuzeydo\u011fu kesiminde s\u0131ralanm\u0131\u015f olan \u0130skenderun, D\u00f6rtyol, Payas ve Erzin Ovalar\u0131 ile Asi Nehri\u2019nin denize d\u00f6k\u00fcld\u00fc\u011f\u00fc yerde bulunan Asi Delta Ovas\u0131\u2019d\u0131r. \u0130lin g\u00fcneyinde, Asi Nehri ile Suriye s\u0131n\u0131r\u0131 aras\u0131nda kalan ve y\u00fckseltisi 400-900 metre aras\u0131nda de\u011fi\u015fen alan, Kuseyr Platosu\u2019nu olu\u015fturur. Plato \u00fczerinde yer yer tepelikler ve m\u00fcnferit Kelda\u011f (K\u0131l\u0131\u00e7 Da\u011f\u0131 1730 m) y\u00fckseltisi dikkat \u00e7eker.<\/p>\n\n\n\n
\u0130lde yazlar\u0131 s\u0131cak ve kurak, k\u0131\u015flar\u0131 ise \u0131l\u0131k ve ya\u011f\u0131\u015fl\u0131 karakteristik Akdeniz iklimi egemendir. Y\u0131ll\u0131k s\u0131cakl\u0131k ortalamalar\u0131n\u0131n 15-20 \u00b0C aras\u0131nda de\u011fi\u015fti\u011fi Hatay\u2019da ayl\u0131k s\u0131cakl\u0131k ortalamalar\u0131 yaz aylar\u0131nda en fazla, k\u0131\u015f aylar\u0131nda ise en d\u00fc\u015f\u00fck de\u011ferlere ula\u015f\u0131r.<\/p>\n\n\n\n
\u0130lde y\u0131ll\u0131k ortalama toplam ya\u011f\u0131\u015f miktar\u0131 562,2\u20131216,3 mm aras\u0131nda de\u011fi\u015fir. En fazla ya\u011f\u0131\u015f k\u0131\u015f aylar\u0131nda, en az ya\u011f\u0131\u015f yaz aylar\u0131nda d\u00fc\u015fer. Ya\u011f\u0131\u015fta dikkat \u00e7eken bir di\u011fer \u00f6zellik ise D\u00f6rtyol\u2019un do\u011fusundaki Amanos Da\u011flar\u0131\u2019n\u0131n denizden gelen hava ak\u0131mlar\u0131na dik uzan\u0131\u015f g\u00f6stermesidir ve buna ba\u011fl\u0131 olu\u015fan orografik ya\u011f\u0131\u015flardan dolay\u0131 y\u0131ll\u0131k ortalama 1500 mm civar\u0131nda ya\u011f\u0131\u015f almas\u0131d\u0131r.<\/p>\n","protected":false},"excerpt":{"rendered":"
Hatay ve \u00e7evresi yo\u011fun tektonizmaya maruz kald\u0131\u011f\u0131ndan yery\u00fcz\u00fc \u015fekilleri a\u00e7\u0131s\u0131ndan \u00e7e\u015fitlilik g\u00f6sterir. Ba\u015fl\u0131ca y\u00fczey \u015fekilleri; da\u011f, plato ve ovalardan olu\u015fur. En \u00f6nemli da\u011fl\u0131k alan, Amik Ovas\u0131\u2019n\u0131n i\u00e7inde yer ald\u0131\u011f\u0131 graben alan\u0131 ile Akdeniz aras\u0131nda adeta bir set gibi y\u00fckselen ve kuzeydo\u011fu-g\u00fcneybat\u0131 y\u00f6n\u00fcnde uzan\u0131\u015f g\u00f6steren Amanos Da\u011flar\u0131\u2019d\u0131r. Bu da\u011flar\u0131n il i\u00e7indeki en y\u00fcksek noktas\u0131n\u0131 Hassa\u2019n\u0131n bat\u0131s\u0131ndaki […]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":123,"menu_order":1,"comment_status":"closed","ping_status":"closed","template":"","meta":{"spay_email":""},"yoast_head":"\n