Karada\u011f, Balkanlar’\u0131n bat\u0131s\u0131nda, Dinar Alpleri’nin g\u00fcney ucunda yer alan \u00fclkedir. Adriyatik Denizi ve H\u0131rvatistan (g\u00fcneybat\u0131), Bosna-Hersek (kuzeybat\u0131), S\u0131rbistan (kuzeydo\u011fu), Kosova (do\u011fu) ve Arnavutluk (g\u00fcneydo\u011fu) ile s\u0131n\u0131rlanm\u0131\u015ft\u0131r.<\/p>\n
Karada\u011f’\u0131n idari ba\u015fkenti Podgorica’d\u0131r, ancak k\u00fclt\u00fcrel merkezi tarihi ba\u015fkenti ve eski \u015fehri Cetinje’dir. 20. y\u00fczy\u0131l\u0131n b\u00fcy\u00fck bir b\u00f6l\u00fcm\u00fcnde Karada\u011f, Yugoslavya’n\u0131n bir par\u00e7as\u0131yd\u0131 ve 2003’ten 2006’ya kadar S\u0131rbistan ve Karada\u011f federe birli\u011finin bir par\u00e7as\u0131yd\u0131.<\/p>\n
Toprak<\/strong><\/p>\n \u00dclkenin adlar\u0131 – hem Karada\u011f (Venedik \u0130talyancas\u0131ndan) hem de Crna Gora – Adriyatik Denizi yak\u0131nlar\u0131ndaki tarihi merkezi ve y\u00fczy\u0131llard\u0131r s\u00fcren m\u00fccadelelerdeki kalesi olan Lov\u0107en Da\u011f\u0131’na (5.738 fit [1.749 metre]) at\u0131fta bulunularak “Kara Da\u011f” anlam\u0131na gelir. T\u00fcrklerle. Balkan \u00fclkeleri aras\u0131nda tek ba\u015f\u0131na Karada\u011f hi\u00e7bir zaman boyun e\u011fdirilmedi. Karada\u011f’\u0131n g\u00fcneybat\u0131daki eski kalbi, baz\u0131 ekilebilir alanlar\u0131n oldu\u011fu, \u00f6rne\u011fin Cetinje \u00e7evresi ve Zeta vadisi gibi, \u00e7o\u011funlukla kurak tepelerden olu\u015fan karstik bir b\u00f6lgedir. Dinar Alpleri’nin (Durmitor Da\u011f\u0131) bir b\u00f6l\u00fcm\u00fcn\u00fc i\u00e7eren do\u011fu b\u00f6lgeleri daha verimlidir ve geni\u015f ormanlara ve \u00e7imenli yaylalara sahiptir. Karada\u011f’\u0131n akarsu sistemi iki z\u0131t y\u00f6nde akmaktad\u0131r. Kuzeyde Piva, Tara ve Lim nehirleri, g\u00fcneyde Mora\u010da ve Zeta nehirleri izler.<\/p>\n Topografik Yap\u0131<\/strong><\/p>\n Karada\u011f’\u0131n arazisi, Kosova ve Arnavutluk s\u0131n\u0131rlar\u0131 boyunca uzanan y\u00fcksek da\u011flardan, Bat\u0131 Balkan Yar\u0131madas\u0131’n\u0131n Karst b\u00f6lgesinin bir b\u00f6l\u00fcm\u00fc boyunca, yaln\u0131zca 1 ila 4 mil (2 ila 6 km) geni\u015fli\u011findeki dar bir k\u0131y\u0131 ovas\u0131na kadar uzan\u0131r. Lov\u0107en Da\u011f\u0131 ve di\u011fer zirvelerin Kotor K\u00f6rfezi’nin giri\u015finden aniden y\u00fckseldi\u011fi kuzeyde k\u0131y\u0131 ovas\u0131 tamamen kaybolur. K\u0131y\u0131 b\u00f6lgesi sismik aktivite i\u00e7in not edilir.<\/p>\n Karada\u011f’\u0131n Karst b\u00f6l\u00fcm\u00fc genellikle deniz seviyesinden 3.000 fit (900 metre) y\u00fckseklikte yer al\u0131r – ancak baz\u0131 b\u00f6lgelerde 6.000 fit (1.800 metre) y\u00fckselir. En al\u00e7ak b\u00f6l\u00fcm, yakla\u015f\u0131k 1.500 fit (450 metre) y\u00fckseklikteki Zeta Nehri vadisindedir. Nehir, karstik b\u00f6lgelere \u00f6zg\u00fc d\u00fcz tabanl\u0131, uzun bir \u00e7\u00f6k\u00fcnt\u00fc olan Nik\u0161i\u0107 Polje’nin merkezini kaplar, t\u0131pk\u0131 d\u00fcdenler ve yer alt\u0131 ma\u011faralar\u0131 olu\u015fturmak i\u00e7in eriyen a\u011f\u0131rl\u0131kl\u0131 olarak kire\u00e7ta\u015f\u0131 alt\u0131ndaki kaya gibi.<\/p>\n Karada\u011f’\u0131n y\u00fcksek da\u011flar\u0131, Avrupa’daki en engebeli arazilerden baz\u0131lar\u0131n\u0131 i\u00e7erir ve ortalama y\u00fcksekli\u011fi 2.000 metreden fazlad\u0131r. Durmitor Da\u011flar\u0131’ndaki 2.522 metreye ula\u015fan ve \u00fclkenin en y\u00fcksek noktas\u0131 olan Bobotov Zirvesi dikkat \u00e7ekicidir. Karada\u011f da\u011flar\u0131, son buzul d\u00f6neminde Balkan Yar\u0131madas\u0131’n\u0131n en \u00e7ok buzla a\u015f\u0131nm\u0131\u015f b\u00f6l\u00fcm\u00fcyd\u00fc.<\/p>\n \u0130klim<\/strong><\/p>\n Karada\u011f’\u0131n a\u015fa\u011f\u0131 kesimlerinde yazlar\u0131 kurak, k\u0131\u015flar\u0131 \u0131l\u0131man ve ya\u011f\u0131\u015fl\u0131 olan Akdeniz iklimi g\u00f6r\u00fcl\u00fcr. S\u0131cakl\u0131k y\u00fckseklik ile b\u00fcy\u00fck \u00f6l\u00e7\u00fcde de\u011fi\u015fir. Deniz seviyesine yak\u0131n olan Podgorica, ortalama 81 \u00b0F (27 \u00b0C) ile \u00fclkedeki en s\u0131cak Temmuz s\u0131cakl\u0131klar\u0131na sahip olmas\u0131yla tan\u0131n\u0131r. Karst b\u00f6lgesinde 2.200 fit (670 metre) y\u00fckseklikte bulunan Cetinje’nin ortalama s\u0131cakl\u0131\u011f\u0131 5 \u00b0C (10 \u00b0F) daha d\u00fc\u015f\u00fckt\u00fcr. Ortalama Ocak s\u0131cakl\u0131klar\u0131 g\u00fcney k\u0131y\u0131s\u0131ndaki Bar’da 46 \u00b0F (8 \u00b0C) ile kuzey da\u011flar\u0131nda 27 \u00b0F (-3 \u00b0C) aras\u0131nda de\u011fi\u015fir.<\/p>\n Karada\u011f’\u0131n da\u011fl\u0131k b\u00f6lgeleri, Avrupa’daki en y\u00fcksek ya\u011f\u0131\u015f miktarlar\u0131ndan baz\u0131lar\u0131n\u0131 al\u0131yor. Kotor K\u00f6rfezi’nin yukar\u0131s\u0131ndaki Karst’taki Crkvice’de y\u0131ll\u0131k ya\u011f\u0131\u015f yakla\u015f\u0131k 200 in\u00e7tir (5.100 mm). Akdeniz k\u0131y\u0131s\u0131ndaki \u00e7o\u011fu b\u00f6lgede oldu\u011fu gibi, ya\u011f\u0131\u015flar esas olarak y\u0131l\u0131n so\u011fuk d\u00f6neminde meydana gelir, ancak daha y\u00fcksek da\u011flarda ikincil bir yaz maksimumu mevcuttur. Karada\u011f k\u0131y\u0131lar\u0131nda kar \u00f6rt\u00fcs\u00fc nadirdir, karstik polye \u00e7\u00f6k\u00fcnt\u00fclerinde ortalama 10 g\u00fcn ve daha y\u00fcksek da\u011flarda 120 g\u00fcne \u00e7\u0131kar.<\/p>","protected":false},"excerpt":{"rendered":" Karada\u011f, Balkanlar’\u0131n bat\u0131s\u0131nda, Dinar Alpleri’nin g\u00fcney ucunda yer alan \u00fclkedir. Adriyatik Denizi ve H\u0131rvatistan (g\u00fcneybat\u0131), Bosna-Hersek (kuzeybat\u0131), S\u0131rbistan (kuzeydo\u011fu), Kosova (do\u011fu) ve Arnavutluk (g\u00fcneydo\u011fu) ile s\u0131n\u0131rlanm\u0131\u015ft\u0131r. Karada\u011f’\u0131n idari ba\u015fkenti Podgorica’d\u0131r, ancak k\u00fclt\u00fcrel merkezi tarihi ba\u015fkenti ve eski \u015fehri Cetinje’dir. 20. y\u00fczy\u0131l\u0131n b\u00fcy\u00fck bir b\u00f6l\u00fcm\u00fcnde Karada\u011f, Yugoslavya’n\u0131n bir par\u00e7as\u0131yd\u0131 ve 2003’ten 2006’ya kadar S\u0131rbistan ve Karada\u011f […]<\/p>\n","protected":false},"author":2,"featured_media":23011,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[2,1,5,78],"tags":[306,307,311,309,308,315,310,304,319,318,303,314,312,313,305,317,316],"_links":{"self":[{"href":"https:\/\/maremont.me\/tr\/wp-json\/wp\/v2\/posts\/23006"}],"collection":[{"href":"https:\/\/maremont.me\/tr\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/maremont.me\/tr\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/maremont.me\/tr\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/maremont.me\/tr\/wp-json\/wp\/v2\/comments?post=23006"}],"version-history":[{"count":4,"href":"https:\/\/maremont.me\/tr\/wp-json\/wp\/v2\/posts\/23006\/revisions"}],"predecessor-version":[{"id":23029,"href":"https:\/\/maremont.me\/tr\/wp-json\/wp\/v2\/posts\/23006\/revisions\/23029"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/maremont.me\/tr\/wp-json\/wp\/v2\/media\/23011"}],"wp:attachment":[{"href":"https:\/\/maremont.me\/tr\/wp-json\/wp\/v2\/media?parent=23006"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/maremont.me\/tr\/wp-json\/wp\/v2\/categories?post=23006"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/maremont.me\/tr\/wp-json\/wp\/v2\/tags?post=23006"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}