MARMARA B\u00d6LGES\u0130<\/p>\n
\u00c7anakkale \u0130li<\/p>\n
Gelibolu Yar\u0131madas\u0131 Tarihi Milli Park\u0131<\/p>\n
1973\u2019te kurulmu\u015f ve BM Milli Parklar ve Koruma Alanlar\u0131 listesinde olan park, \u00c7anakkale ili s\u0131n\u0131rlar\u0131 i\u00e7erisinde, Gelibolu Yar\u0131madas\u0131n\u0131n g\u00fcney ucunda, \u00c7anakkale bo\u011faz\u0131n\u0131n Avrupa yakas\u0131nda 33,000 hektarl\u0131k bir alan\u0131 kapsamaktad\u0131r.
\nBirinci D\u00fcnya Sava\u015f\u0131 \u00c7anakkale Deniz ve Kara Muhaberelerinin yap\u0131ld\u0131\u011f\u0131 yerler park i\u00e7erisindedir. Muharebe alanlar\u0131, sava\u015f mezarlar\u0131, an\u0131tlar ve sava\u015fla ilgili kal\u0131nt\u0131lar \u201ctarihi sit alan\u0131\u201d ve \u201ck\u00fclt\u00fcrel varl\u0131k\u201d olarak tescil edilmi\u015ftir. Ayr\u0131ca M.\u00d6.4000 tarihine dek giden bir\u00e7ok \u201cArkeolojik sit alan\u0131 ve an\u0131t\u0131\u201d vard\u0131r. \u00c7ok \u00e7e\u015fitli \u201cdo\u011fal sit alanlar\u0131 ve an\u0131tlar\u201d i\u00e7erisinde ise kumsallar, koyaklar, Akdeniz \u00e7al\u0131lar\u0131 (maki) ile kar\u0131\u015f\u0131k koru par\u00e7alar\u0131, \u00e7arp\u0131c\u0131 g\u00f6r\u00fcn\u00fcml\u00fc jeolojik ve jeomorfolojik olu\u015fumlar, bir tuz g\u00f6l\u00fc(yak\u0131n zamana kadar bir k\u0131y\u0131 g\u00f6l\u00fcyd\u00fc)ve 15,yy askeri mimarisinin e\u015fsiz \u00f6rneklerini i\u00e7eren ilgin\u00e7 bir \u201ck\u00fclt\u00fcrel miras\u201d koleksiyonu vard\u0131r.<\/p>\n
Trioya Tarihi Milli Park\u0131<\/p>\n
\u00c7anakkale ili Ezine il\u00e7e s\u0131n\u0131rlar\u0131 i\u00e7erisinde \u00c7anakkale bo\u011faz\u0131n\u0131n giri\u015finde yer almaktad\u0131r.
\nMilli park\u0131n ana kaynak de\u011ferini Trioya kenti olu\u015fturmaktad\u0131r. Trioya tarihi ve onunla ilgili \u00f6zellikler, Trias b\u00f6lgesinin yani Edremit k\u00f6rfezinin kuzeyinde Marmara denizinin g\u00fcney k\u0131y\u0131lar\u0131na kadar olan b\u00f6lgeyi kaplamaktad\u0131r. Milli park\u0131n ve \u00e7evresinin tabiat tarihi ile ilgili en \u00f6nemli \u00f6zelli\u011fi, jeolojik \u00f6zelli\u011fidir. Trioya ve \u00e7evresinde genel olarak jeolojik yap\u0131y\u0131, geni\u015f alanlar kaplayan neojen bi\u00e7imlenmeler meydana getirir.<\/p>\n
Bursa \u0130li<\/p>\n
Uluda\u011f Milli Park\u0131 <\/p>\n
Milli park, Marmara b\u00f6lgesinde Bursa ilinin g\u00fcneyinde y\u00fckselen Uluda\u011f \u00fczerinde yer al\u0131r.
\nYer k\u00fcrenin derinliklerinden gelen magman\u0131n k\u0131r\u0131klar ve \u00e7atlaklar boyunca yery\u00fcz\u00fcne do\u011fru y\u00fckselmesi ve kat\u0131la\u015fmas\u0131 sonunda meydana gelen Uluda\u011f\u2019\u0131n jeolojik yap\u0131s\u0131n\u0131 genellikle i\u00e7 p\u00fcsk\u00fcr\u00fck granit kaya\u00e7lar\u0131 olu\u015fturmaktad\u0131r. Da\u011f\u0131n bug\u00fcnk\u00fc \u015feklini kazanmas\u0131 tektonik hareketler ve farkl\u0131 a\u015f\u0131nma etkisi ile olu\u015fmu\u015ftur. Bursa ovas\u0131na k\u0131sa mesafede ve 2543 metre y\u00fckseklikte olan Uluda\u011f, Marmara b\u00f6lgesinin en y\u00fcksek noktas\u0131d\u0131r. Aras \u00e7a\u011flayan\u0131 ve doruklarda g\u00f6r\u00fclen buzul izleri Uluda\u011f\u2019\u0131n jeomorfolojik yap\u0131s\u0131n\u0131n ilgi \u00e7ekici \u00f6zellikleridir. Milli park\u0131n bir ba\u015fka \u00f6zelli\u011fi de Bursa ovas\u0131ndan Uluda\u011f\u2019\u0131n doruklar\u0131na do\u011fru de\u011fi\u015fen bitki topluluklar\u0131n\u0131n meydana getirdi\u011fi orman ku\u015faklar\u0131d\u0131r. Botanik bilimci MAYR\u2019\u0131n bitki ku\u015faklar\u0131n\u0131 muhtelif y\u00fcksekliklerde karakterize etmesi bak\u0131m\u0131ndan D\u00fcnya Ormanc\u0131l\u0131k literat\u00fcr\u00fcnde \u00f6zel bir \u00f6nemi vard\u0131r. Uluda\u011f kar kalitesiyle ve kal\u0131nl\u0131\u011f\u0131yla kayak yapmaya elveri\u015fli olup, T\u00fcrkiye\u2019nin en \u00f6nemli k\u0131\u015f sporlar\u0131 merkezidir.<\/p>\n
Bal\u0131kesir \u0130li<\/p>\n
Kazda\u011f\u0131 Milli Park\u0131<\/p>\n
Milli park, \u00c7anakkale\u2019ye 123 km., Bal\u0131kesir\u2019e 92 km. mesafededir.
\nKazda\u011f\u0131 tarih \u00f6ncesi y\u0131llarda da \u00e7e\u015fitli medeniyetleri bar\u0131nd\u0131rm\u0131\u015ft\u0131r. Bilinen tarihi M.\u00d6.2000 y\u0131llar\u0131nda ba\u015flar. \u0130da da\u011f\u0131n\u0131n her yerinde kaynaklar \u00e7\u0131kmaktad\u0131r.1500 m rak\u0131mda dahi yaz k\u0131\u015f suyu olan kaynaklar mevcuttur. Edremit, Ak\u00e7ay ve Alt\u0131noluk\u2019un buz gibi so\u011fuk olan i\u00e7me ve kullanma suyu Kazda\u011f\u0131\u2019n\u0131n eriyen kar sular\u0131d\u0131r. Kazda\u011flar\u0131ndan gelen orman havas\u0131 ile denizin iyotlu ve oksijen miktar\u0131 y\u00fcksek havas\u0131 birle\u015fince Alt\u0131noluk \u015eahinderesi bo\u011faz\u0131 civar\u0131 oksijen \u00e7ad\u0131r\u0131 \u015feklinde ifade edilmektedir. D\u00fcnyan\u0131n oksijen bollu\u011fu y\u00f6n\u00fcnden ilk \u00fc\u00e7 yerinden biri oldu\u011fu tespit edilmi\u015ftir.
\nEge b\u00f6lgesi ile Marmara b\u00f6lgesini birbirinden ay\u0131ran \u0130da da\u011f\u0131, Biga yar\u0131madas\u0131_
\nn\u0131n en y\u00fcksek k\u00fctlesidirKazda\u011f\u0131n\u0131n \u00fczerine yerle\u015fmi\u015f, kuzey-g\u00fcney istikametine uzanan derin vadi ve kanyonlar\u0131, flora ve hayvan varl\u0131\u011f\u0131 a\u00e7\u0131s\u0131ndan zengin bir potansiyel arz etmekte, \u00f6zellikle de bitki \u00f6rt\u00fcs\u00fcn\u00fcn ta\u015f\u0131d\u0131\u011f\u0131 biyolojik \u00e7e\u015fitlilik ana kaynak de\u011ferini olu\u015fturmaktad\u0131r. Da\u011f\u0131n \u00fcst tabakas\u0131nda 600\u2013700 rak\u0131mlar ars\u0131nda K\u0131z\u0131l\u00e7am hakimdir. \u00dcst rak\u0131mlarda Kara\u00e7am, Kay\u0131n, K\u00f6knar asil a\u011fa\u00e7 t\u00fcrleridir. Alt tabakada Sistus (Laden), Erika gibi t\u0131bbi bitkiler a\u00e7\u0131s\u0131ndan da \u00e7ok zengindir.<\/p>\n
Ku\u015f Cenneti Milli Park\u0131<\/p>\n
Bal\u0131kesir ili, Band\u0131rma il\u00e7e s\u0131n\u0131rlar\u0131 i\u00e7inde Ku\u015f G\u00f6l\u00fc\u2019n\u00fcn kuzeydo\u011fusunda yer al\u0131r.
\nG\u00f6l sular\u0131, s\u00f6\u011f\u00fct korusu ve sazl\u0131klar\u0131n sa\u011flad\u0131\u011f\u0131 beslenme, g\u00fcvenlik ve bar\u0131nma olanaklar\u0131 ile elveri\u015fli iklim \u015fartlar\u0131, Avrupa-Asya k\u0131talar\u0131 aras\u0131nda b\u00fcy\u00fck ku\u015f g\u00f6\u00e7lerini bu k\u00fc\u00e7\u00fck yurt k\u00f6\u015fesine y\u00f6nelterek, y\u00f6renin memleketler aras\u0131 \u00fcn kazanmas\u0131na neden olmaktad\u0131r. Kulu\u00e7ka yapan, k\u0131\u015flayan ve g\u00f6\u00e7 s\u0131ras\u0131nda u\u011frayan 239 ku\u015f t\u00fcr\u00fcnden 2\u20133 milyon ku\u015f her y\u0131l buraya u\u011framaktad\u0131r.
\nUluslararas\u0131 d\u00fczeyde \u00f6nem ta\u015f\u0131yan milli parktaki ku\u015f zenginli\u011fi ve milli park tan\u0131m\u0131 i\u00e7indeki ba\u015far\u0131l\u0131 koruma uygulamas\u0131 nedeniyle 1976 y\u0131l\u0131nda Avrupa Konseyince A s\u0131n\u0131f\u0131 Avrupa diplomas\u0131 verilmi\u015ftir.1981\u20131986\u20131991 ve 1996 y\u0131llar\u0131nda bu diploma yenilenmi\u015ftir. Ayr\u0131ca 15.04.1998 tarih ve 23314 say\u0131l\u0131 resmi gazetede yay\u0131mlanan kararla Ku\u015fcenneti, Romsan S\u00f6zle\u015fmesi(\u00d6zellikle Su Ku\u015flar\u0131 Ya\u015fama Ortam\u0131 Olarak Uluslar aras\u0131 \u00d6neme Sahip Sulak Alan Hakk\u0131nda S\u00f6zle\u015fme) kapsam\u0131na al\u0131nm\u0131\u015ft\u0131r.<\/p>\n
EGE B\u00d6LGES\u0130<\/p>\n
Afyon \u0130li<\/p>\n
Ba\u015fkomutan Tarihi Milli Park\u0131 <\/p>\n
\u0130\u00e7 bat\u0131 Anadolu\u2019da Afyon, K\u00fctahya ve U\u015fak illeri s\u0131n\u0131rlar\u0131 i\u00e7erisinde yer almaktad\u0131r.
\nKurtulu\u015f sava\u015f\u0131n\u0131n ge\u00e7ti\u011fi y\u00f6relerde ki tarihi olgular Ba\u015fkomutan Tarihi Milli Park\u0131n\u0131n ana kaynak de\u011ferini olu\u015fturur. Kocatepe ve Dumlup\u0131nar b\u00f6l\u00fcmlerinde yer yer
\nOrmanl\u0131k alanlar i\u00e7erisinde b\u00fct\u00fcn y\u0131l su bulunan vadi boylar\u0131, pek \u00e7ok endemik t\u00fcrleri kapsayan bitki \u00f6rt\u00fcs\u00fc ve yaban hayat\u0131 zenginlikleri milli park\u0131n di\u011fer de\u011ferlerini olu\u015fturur.<\/p>\n
Ayd\u0131n \u0130li<\/p>\n
B\u00fcy\u00fck Menderes Deltas\u0131 Milli Park\u0131<\/p>\n
Ayd\u0131n ili, Ku\u015fadas\u0131 ve S\u00f6ke il\u00e7eleri s\u0131n\u0131rlar\u0131nda yer al\u0131r.
\nSamsun da\u011f\u0131n\u0131n Ege denize do\u011fru uzant\u0131s\u0131yla \u015fekillenen Dilek Yar\u0131madas\u0131n\u0131n jeolojik yap\u0131s\u0131, paleozoik \u015fistler, mezozoik kalker ve mermerler ile neojen tortul k\u00fctlelerden meydana gelmi\u015f, Menderes mast\u0131n\u0131n bir par\u00e7as\u0131d\u0131r. Yar\u0131mada kumlu, killi, yat\u0131k ve y\u00fcksek k\u0131y\u0131 \u015fekillerini i\u00e7eren plajlar\u0131yla ilgi \u00e7ekici k\u0131y\u0131 \u00f6zelliklerine sahiptir. Milli park\u0131n \u00f6zellikle kuzey kesimi Akdeniz b\u00f6lgesinde ender g\u00f6r\u00fclen potansiyelde bitki \u00f6rt\u00fcs\u00fcne sahiptir. \u00d6zellikle defne ve kestane bitki ku\u015faklar\u0131 ile Akdeniz maki floras\u0131n\u0131n hemen b\u00fct\u00fcn bitki t\u00fcrleri yar\u0131madada en canl\u0131 ve sa\u011fl\u0131kl\u0131 \u00f6rnekleriyle yer almaktad\u0131r. Kuzey Anadolu ormanl\u0131k y\u00f6relerine has kestanenin, en g\u00fcneye indi\u011fi, \u00fclkemizde birka\u00e7 yerde bulunan kartopunun, Finike ard\u0131c\u0131n\u0131n k\u00fc\u00e7\u00fck bir topluluk meydana getirdi\u011fi, p\u0131rnal me\u015fesi, dall\u0131 selvilerin birlikte yeti\u015fti\u011fi tek yerdir.
\nMilli park\u0131n k\u0131y\u0131lar\u0131nda Akdeniz \u00fclkelerinde korunan t\u00fcrler aras\u0131nda da bulunan Akdeniz foku ve deniz kaplumba\u011falar\u0131 ya\u015fama ve \u00fcreme olana\u011f\u0131 bulmu\u015ftur.<\/p>\n
Denizli \u0130li<\/p>\n
Honaz Da\u011f\u0131 Milli Park\u0131<\/p>\n
Denizli ili Honaz il\u00e7esi s\u0131n\u0131rlar\u0131 i\u00e7erisinde yer almaktad\u0131r. Milli park\u0131n ana de\u011ferini Ege b\u00f6lgesinin en y\u00fcksek da\u011f\u0131 olan Honaz da\u011f\u0131 b\u00fcnyesindeki kaynaklar olu\u015fturmaktad\u0131r.
\nEge b\u00f6lgesinde Pleistosen d\u00f6neminde Periglasiyal ortam \u015fartlar\u0131n\u0131 h\u00fck\u00fcm s\u00fcrd\u00fc\u011f\u00fc az say\u0131da yerlerden birisi de Honaz da\u011f\u0131d\u0131r. Da\u011f \u00fczerinde bir\u00e7ok Periglasiyal ko\u015fullar\u0131 karakterize eden jeomorfolojik \u015fekil bulunmakta olup, ana \u015fekil grubu olarak ise; horst bi\u00e7imi y\u00fczeye hakim olmaktad\u0131r. D\u00fc\u015fey y\u00f6ndeki faylanmalar sonucu Honaz da\u011f\u0131 olduk\u00e7a dik bir g\u00f6r\u00fcn\u00fcm kazanm\u0131\u015ft\u0131r. Y\u00f6renin genel litolojik yap\u0131s\u0131 gnays ve mika\u015fistlerden meydana gelmekte olup, yer yer kristalize kire\u00e7 ta\u015flar\u0131na da rastlanmaktad\u0131r.
\nYo\u011fun bitki \u00f6rt\u00fcs\u00fcne sahip Honaz da\u011f\u0131 \u00fczerinde alt floraya ait endemik t\u00fcrler bulunmakta, Alp\u0131n floraya ait t\u00fcrler ise da\u011f\u0131n \u00fcst zonalar\u0131nda yer almaktad\u0131r. Orman bi\u00e7imi i\u00e7erisinde k\u0131z\u0131l\u00e7am (Pinus Brutia), kara\u00e7am (Pinus Nigra) ve ard\u0131\u00e7 hakim t\u00fcrlerdir. Yaban hayat\u0131 a\u00e7\u0131s\u0131ndan da zenginlik i\u00e7eren sahada \u00f6zellikle da\u011f ke\u00e7isi yo\u011fun olarak bulunmaktad\u0131r
\nHonaz da\u011f\u0131, gerek topokrafig \u00f6zellikleri ve uygun e\u011fim ko\u015fullar\u0131 gerekse kar ya\u011f\u0131\u015f\u0131n\u0131n yeterli d\u00fczeyde olmas\u0131 nedeniyle \u00fclkemizde kayak potansiyeli y\u00fcksek alanlardan birisidir. Y\u00f6re; arkeolojik \u00f6zelli\u011fi a\u00e7\u0131s\u0131ndan da zenginli\u011fe sahiptir.<\/p>\n
Manisa \u0130li<\/p>\n
Spil Da\u011f\u0131 Milli Park\u0131 <\/p>\n
Ege b\u00f6lgesinde Manisa ilinin yama\u00e7lar\u0131na yasland\u0131\u011f\u0131 Spil da\u011f\u0131 \u00fczerinde yer al\u0131r.
\nKanyon vadiler, inler, ma\u011faralar, dolinler ve lapyalar gibi karstik olu\u015fumlar\u0131 jeolojik yap\u0131s\u0131ndan kaynaklanan ilgi \u00e7ekici yer \u015fekilleridir. B\u00f6lgenin zengin bitki \u00f6rt\u00fcs\u00fc yan\u0131nda, milli parkta bilimsel ara\u015ft\u0131rmalarla belirlenen 20\u2019den fazla endemik bitki t\u00fcr\u00fc bulunmaktad\u0131r. Osmanl\u0131 \u0130mparatorlu\u011fu\u2019nun bir devrine ad\u0131n\u0131 veren ve Avrupa \u00fclkelerine de g\u00f6t\u00fcr\u00fclen Manisa laleleri de milli parkta tabii olarak yeti\u015fmektedir.
\nMilli park\u0131n tarihi ve mitolojik y\u00f6n\u00fc de zengindir. Mitolojiye g\u00f6re Spil da\u011f\u0131na ad\u0131n\u0131 veren zaman tanr\u0131s\u0131 Kronos\u2019un kar\u0131s\u0131 Kybele (Sipylena)\u2019dir. Ayr\u0131ca \u201cA\u011flayan Kaya\u201d olarak bilinen yer mitolojiye g\u00f6re 14 \u00e7ocu\u011funun tanr\u0131\u00e7a Leto\u2019nun \u00e7ocuklar\u0131 Apollon ve Artemis taraf\u0131ndan \u00f6ld\u00fcr\u00fclmesi sonucu, \u00e7ocuklar\u0131n\u0131n ard\u0131ndan a\u011flayan Niobe\u2019ye aittir. Arazinin jeomorfolojik yap\u0131s\u0131 da\u011fc\u0131l\u0131k tracking ve at\u0131c\u0131l\u0131k sporlar\u0131na uygundur.<\/p>\n
Mu\u011fla \u0130li<\/p>\n
Sakl\u0131kent Milli Park\u0131<\/p>\n
Mu\u011fla ili Fethiye il\u00e7esi ile Antalya ili Ka\u015f il\u00e7esi s\u0131n\u0131rlar\u0131 i\u00e7erisinde, E\u015fen \u00e7ay\u0131n\u0131n bir kolu \u00fczerinde yer almaktad\u0131r.
\nMilli park\u0131n ana \u00f6zelli\u011fini, Sakl\u0131kent Kanyonu olu\u015fturmaktad\u0131r. Kanyon iki havza ars\u0131nda uzanan Antesedan bir \u00f6zellik sunmaktad\u0131r. Y\u00f6redeki irili ufakl\u0131 kanyonlar\u0131n meydana gelmesinde tektonik emarelerin yan\u0131nda kast olu\u015fumunda \u00f6nemli rol oynad\u0131\u011f\u0131 g\u00f6r\u00fclmektedir. Y\u00f6redeki tektonik kontroll\u00fc bir jeomorfolojik geli\u015fimine sahip olup, \u00f6zellikle d\u00fc\u015fey y\u00f6nl\u00fc tektonizma Sakl\u0131kent kanyonunda geli\u015fme seyrini etkilemi\u015f ve bug\u00fcnk\u00fc g\u00f6r\u00fcn\u00fcm\u00fcn\u00fc almas\u0131nda Litolojik yap\u0131ya \u00f6nemli \u00f6l\u00e7\u00fcde yard\u0131mc\u0131 olmu\u015ftur. Milli park alan\u0131nda orman formasyonu k\u0131z\u0131l\u00e7am, kara\u00e7am ve sedir\u2019den olu\u015fur. Ayr\u0131ca Aktez yaylas\u0131n\u0131n g\u00fcneydo\u011fu kesimi, so\u011fanl\u0131 bitkilerin (S\u0131klemenlerin) endemik olarak yerle\u015ftikleri ve yeti\u015ftikleri sahad\u0131r.<\/p>\n
Marmaris Milli Park\u0131<\/p>\n
Milli park alan\u0131 Mu\u011fla ili, Marmaris il\u00e7esi s\u0131n\u0131rlar\u0131 i\u00e7erisinde yer almaktad\u0131r.
\nSahan\u0131n jeolojik yap\u0131s\u0131, genel olarak magmatik ve kalker kaya\u00e7lar\u0131 ile al\u00fcvyon ve yama\u00e7 molozlar\u0131ndan olu\u015fmu\u015ftur. Kuzey-Bat\u0131s\u0131nda mostra veren kretase ya\u015fl\u0131 magmatik kayalar\u0131n okside olmas\u0131 k\u0131z\u0131l renkli g\u00f6r\u00fcn\u00fcmlere yol a\u00e7m\u0131\u015ft\u0131r. Kalkerler ise sahan\u0131n do\u011fusunda geni\u015f mostra verirler. Kalker mostralar\u0131n\u0131n bat\u0131 k\u0131sm\u0131 tabakal\u0131, do\u011fu k\u0131sm\u0131 ise masif durumdad\u0131r.
\nMilli park\u0131n orman formasyonunu k\u0131z\u0131l\u00e7am olu\u015fturmaktad\u0131r. Bununla birlikte endemik bir t\u00fcr olan s\u0131\u011fla a\u011fac\u0131 sahan\u0131n belirli b\u00f6lgelerinde yay\u0131l\u0131m g\u00f6sterir. Zakkum ve defne gibi a\u011fa\u00e7\u00e7\u0131k formlu Akdeniz bitkileri de bu alanda geni\u015f yay\u0131l\u0131\u015f g\u00f6sterir. Saha yaban hayat\u0131 zenginli\u011fi i\u00e7ermektedir. Nesli t\u00fckenmekte olan hayvanlara burada rastlanmaktad\u0131r.
\nMilli park sahas\u0131nda; antik Physkos kenti yer almakta olup antik \u00e7a\u011fda bu b\u00f6lge Karia b\u00f6lgesi olarak an\u0131lmaktad\u0131r. Burada Rodos kolonisi izleri g\u00f6r\u00fclmektedir.<\/p>\n
AKDEN\u0130Z B\u00d6LGES\u0130<\/p>\n
Adana \u0130li<\/p>\n
Karatepe Aslanta\u015f Tarihi Milli Park\u0131<\/p>\n
Akdeniz b\u00f6lgesinin Osmaniye ilinin Kadirli il\u00e7esine 22 km. uzakl\u0131kta ve Ceyhan \u0131rma\u011f\u0131n\u0131n kenar\u0131nda yer al\u0131r.
\nBu y\u00f6re arkeolojik \u00f6nem ta\u015f\u0131maktad\u0131r. G\u00fcn\u00fcm\u00fcze kadar bir\u00e7ok medeniyete ev sahipli\u011fi yapm\u0131\u015f ve kal\u0131nt\u0131lar\u0131n\u0131 \u00e7a\u011f\u0131m\u0131za kadar ta\u015f\u0131m\u0131\u015ft\u0131r. Karatepe-Aslanta\u015f\u2019\u0131n di\u011fer \u00f6nemli \u00f6zelli\u011fi de yap\u0131lan kaz\u0131 ve ara\u015ft\u0131rmalarda Fenike alfabesi ile yaz\u0131lm\u0131\u015f Aram dilindeki \u00e7evirisi, Hitit hiyeroglif yaz\u0131s\u0131n\u0131n \u00e7\u00f6z\u00fclmesine imk\u00e2n vermi\u015f olmas\u0131d\u0131r.
\nK\u0131z\u0131l\u00e7am, \u0131lg\u0131n, me\u015fe t\u00fcrleri ve maki floras\u0131n\u0131n meydana getirdi\u011fi bitki \u00f6rt\u00fcs\u00fc ve bir\u00e7ok yaban hayvanlar\u0131 toplulu\u011fu ile Ceyhan nehrinde yay\u0131n ve sazan bal\u0131klar\u0131 bulunmaktad\u0131r. <\/p>\n
Isparta \u0130li<\/p>\n
K\u0131z\u0131lda\u011f Milli Park\u0131<\/p>\n
Isparta ili \u015eark\u00eekaraa\u011fa\u00e7 il\u00e7esi s\u0131n\u0131rlar\u0131nda yer alan milli park \u015eark\u00eekaraa\u011fa\u00e7\u2019a 5 km. Isparta\u2019ya 120 km. mesafededir.
\nMilli park\u0131n \u00fczerinde yer ald\u0131\u011f\u0131 K\u0131z\u0131lda\u011f ile Bey\u015fehir g\u00f6l\u00fcn\u00fcn kuzey k\u0131y\u0131lar\u0131 aras\u0131nda uzanan dalgal\u0131 arazi \u00fczerinde genellikle erozyonla a\u015f\u0131nm\u0131\u015f yer \u015fekilleri g\u00f6r\u00fclmektedir. Alan\u0131n jeolojik yap\u0131s\u0131n\u0131 kalker kaya\u00e7lar\u0131ndan meydana gelen formasyonlar meydana getirir. Milli park\u0131n bitki \u00f6rt\u00fcs\u00fcn\u00fc sedir ormanlar\u0131 ve bozuk maki topluluklar\u0131 meydana getirir. Bu ormanlar botanik \u00f6zellikleri kadar \u015eark\u00eekaraa\u011fa\u00e7 ve yak\u0131n \u00e7evresinin rekrasyonel ihtiya\u00e7lar\u0131n\u0131n kar\u015f\u0131lanmas\u0131 ile de \u00f6nem ta\u015f\u0131maktad\u0131r. Ayr\u0131ca amat\u00f6r da\u011fc\u0131lar, 1840 m. y\u00fckseklikteki B\u00fcy\u00fcksivri tepeye t\u0131rmanarak da\u011f sporu yapabilirler.
\nKovada G\u00f6l\u00fc Milli Park\u0131
\nAkdeniz b\u00f6lgesinin g\u00f6ller b\u00f6lgesinde yer al\u0131r.
\nKovada g\u00f6l\u00fcn\u00fcn meydana geli\u015fi, Bat\u0131 Toroslarda g\u00f6r\u00fclen karstik g\u00f6llere benzer. Havzaya d\u00fc\u015fen ya\u011fmur sular\u0131n\u0131n fiziksel ve kimyasal a\u015f\u0131nmas\u0131na eklenen tektonik yer hareketleriyle \u015fekillenen g\u00f6l, karstik bir polyedir. E\u011firdir g\u00f6l\u00fcn\u00fcn g\u00fcneye do\u011fru uzant\u0131s\u0131 olan Kovada g\u00f6l\u00fc, sonradan aradaki dar vadinin al\u00fcvyonlarla dolmas\u0131 sonunda bug\u00fcnk\u00fc \u015feklini alm\u0131\u015ft\u0131r.
\nG\u00f6l\u00fcn hayvan varl\u0131\u011f\u0131 olduk\u00e7a iyi durumdad\u0131r. K\u0131z\u0131l\u00e7am, me\u015fe, \u00e7\u0131nar a\u011fa\u00e7lar\u0131ndan meydana gelen bitki \u00f6rt\u00fcs\u00fc ve park\u0131n tabii g\u00fczellikleri Milli park\u0131n ana kaynak de\u011feri olan a\u00e7\u0131k hava dinlenme kullanma potansiyeline katk\u0131da bulunmaktad\u0131r.
\nSahan\u0131n meydana geli\u015fini haz\u0131rlayan karst morfolojisi, bakir do\u011fan\u0131n ara\u015ft\u0131r\u0131lmas\u0131, y\u00fcr\u00fcy\u00fc\u015f, manzara seyretme, t\u0131rmanma ve primativ kamp\u00e7\u0131l\u0131k imk\u00e2n\u0131 sa\u011flamaktad\u0131r. <\/p>\n
Antalya \u0130li<\/p>\n
Alt\u0131nbe\u015fik Ma\u011faras\u0131 Milli Park\u0131<\/p>\n
Milli park derin ve sarp Manavgat vadisinin bat\u0131 yamac\u0131nda yer almaktad\u0131r.
\nYatay ve k\u0131smen aktif bir ma\u011fara sistemi olan Alt\u0131nbe\u015fik ma\u011faras\u0131 ad\u0131n\u0131 \u00fcst k\u0131s\u0131mda yer alan Alt\u0131nbe\u015fik tepesinden almaktad\u0131r. Toroslar\u0131n bu b\u00f6lgesi hem jeolojik hem de jeomorfolojik y\u00f6nden \u00e7ok kar\u0131\u015f\u0131k bir yap\u0131ya sahiptir. Tersiyerortalar\u0131nda meydana gelen \u015fiddetli k\u0131vr\u0131mlar\u0131, bu d\u00f6nemin sonunda \u015fiddetli dikey y\u00fckselmeler izlemi\u015ftir. Jeolojik bindirmeler b\u00fcy\u00fck k\u0131vr\u0131klar ve derin kaz\u0131lm\u0131\u015f vadiler bu hareketli jeolojik ge\u00e7mi\u015fin sonucudur.
\nAlt\u0131nbe\u015fik ma\u011faras\u0131 \u00fcst Kresate ya\u015fl\u0131 kire\u00e7 ta\u015flar\u0131 i\u00e7inde k\u0131vr\u0131klar \u00fczerinde olu\u015fmu\u015ftur. Ma\u011fara \u00fcst \u00fcste 3 seviyede geli\u015fmi\u015ftir. En alttaki ve orta seviyedeki ya\u011f\u0131\u015fl\u0131 mevsimlerde aktif, en \u00fcst seviye ise devaml\u0131 kurudur.
\nAlt\u0131nbe\u015fik ma\u011faras\u0131 daha kuzeyde bulunan Eynif polyesinin ve civar\u0131ndaki bir dizi daha k\u00fc\u00e7\u00fck polyelerin yeralt\u0131na intikal eden sular\u0131n toplanarak tahliye edildi\u011fi bir ana yeralt\u0131 deresi g\u00f6revini g\u00f6rmektedir. G\u00fcz aylar\u0131nda ma\u011fara i\u00e7inde \u00e7ok miktarda durgun g\u00f6letler vard\u0131r. Ma\u011fara i\u00e7indeki kum ve \u00e7ak\u0131l birikintilerinden, kayalar \u00fczerindeki ak\u0131nt\u0131 oyuklar\u0131ndan bahar aylar\u0131nda orta ve alt seviyeden debisi kuvvetli yeralt\u0131 dereleri akt\u0131\u011f\u0131n\u0131 g\u00f6stermektedir.
\nAlt\u0131nbe\u015fik ma\u011faras\u0131n\u0131n aktivitelerini tamamen yitirmi\u015f olan \u00fcst seviyesinde, tabanda kaya bloklar\u0131 dikkati \u00e7eker, bunlar\u0131n yan\u0131nda dikit ve sark\u0131t olu\u015fumlar\u0131 da vard\u0131r. Orta seviyenin daha \u00e7ok dere yataklar\u0131 \u00f6zelli\u011fini ta\u015f\u0131r. Burada kaya bloklar\u0131 geni\u015f yerler kaplar, yer yer kum ve \u00e7ak\u0131l depolar\u0131 ile traverten olu\u015fumlar\u0131 g\u00f6r\u00fcl\u00fcr. Ma\u011faran\u0131n giri\u015finden itibaren ilk 2000 m. ma\u011faran\u0131n alt seviyesini olu\u015fturur ve buras\u0131 devaml\u0131 su alt\u0131ndad\u0131r. Alt seviyenin bitiminde 40 m.lik dik bir \u00e7\u0131k\u0131\u015f vard\u0131r. Bu \u00e7\u0131k\u0131\u015f ve biti\u015fik duvarlar beyaz renkli kal\u0131n travertenlerle kapl\u0131d\u0131r. Ayr\u0131ca, Alt\u0131nbe\u015fik ma\u011faras\u0131n\u0131n \u00e7evresindeki zengin flora ile karst topografyas\u0131n\u0131n vah\u015fi g\u00fczelli\u011fi milli park\u0131n peyzaj de\u011ferlerini olu\u015fturmaktad\u0131r.<\/p>\n
Beyda\u011flar\u0131 Sahil Milli Park\u0131<\/p>\n
Milli park Antalya-Kemer-Kumluca Devlet Karayolu k\u0131smen sahilden, k\u0131smen de i\u00e7eriden boydan boya kat eder.
\nBat\u0131 Toroslar\u0131n gen\u00e7 da\u011flar ku\u015fa\u011f\u0131n\u0131 i\u00e7ine alan y\u00f6renin jeolojik yap\u0131s\u0131 genellikle kalker ve serpantin kaya\u00e7lar\u0131ndan meydana gelir. Akdeniz b\u00f6lgesinin b\u00fct\u00fcn jeolojik \u015fartlar\u0131na sahip sahada, bitki \u00f6rt\u00fcs\u00fc deniz k\u0131y\u0131s\u0131nda f\u0131st\u0131k \u00e7amlar\u0131 ile ba\u015flar, y\u00fckseldik\u00e7e k\u0131z\u0131l\u00e7am, kara\u00e7am ve 1000 metrenin \u00fcst\u00fcnde sedir a\u011fa\u00e7lar\u0131 g\u00f6r\u00fcl\u00fcr.
\nPark\u0131n bitki t\u00fcr\u00fcnde 21 endemik bitki t\u00fcr\u00fc bulunur. Bu da milli park\u0131n t\u00fcr y\u00f6n\u00fcnden \u00e7e\u015fitlili\u011fini g\u00f6sterir. Alanda yaban hayat\u0131 vard\u0131r.
\nOlympos\u2019un birka\u00e7 km bat\u0131s\u0131ndaki da\u011fl\u0131k arazide kalker ve serpantin formasyonlar\u0131 konta\u011f\u0131ndaki \u00e7atlaklardan \u00e7\u0131kan ve \u201cLikya\u2019n\u0131n S\u00f6nmeyen Ate\u015fi\u201d diye adland\u0131r\u0131lan do\u011falgaz y\u00fczy\u0131llard\u0131r yanmakta ve Bellerophentes mitosuna Chimaira (yanan ta\u015f) ad\u0131yla ge\u00e7erek y\u00f6reye mitolojik de\u011fer kazand\u0131rmaktad\u0131r.
\nG\u00fcll\u00fck Da\u011f\u0131 Milli Park\u0131 (Termessos)
\nAkdeniz b\u00f6lgesinde, Antalya ili Korkuteli il\u00e7esi s\u0131n\u0131rlar\u0131 i\u00e7inde ve Toros da\u011flar\u0131 \u00fczerinde yer al\u0131r.
\n\u015eehrin sular\u0131, kuleler, kral yolu, Hadrian kap\u0131s\u0131 gymnasium, sistemi Termessos\u2019un en g\u00f6rkemli yap\u0131lar\u0131n\u0131n kal\u0131nt\u0131lar\u0131d\u0131r. Milli park\u2019ta; G\u00fcll\u00fck da\u011f\u0131n\u0131n sarp kayal\u0131klar\u0131, duvarlar\u0131 600 metreye kadar y\u00fckselen Mecine Kanyonu gibi jeomorfolojik g\u00fczellikleri yan\u0131nda Akdeniz iklimi tipinin bitki topluluklar\u0131n\u0131 sergileyen orman ve maki \u00f6rt\u00fcs\u00fc, bu ortamda ya\u015fayan da\u011f ke\u00e7isi, alageyik, \u015fah kartal gibi nadir yaban hayvan\u0131 t\u00fcrleri bulunmaktad\u0131r.<\/p>\n
\u0130\u00c7 ANADOLU B\u00d6LGES\u0130<\/p>\n
Yozgat \u0130li<\/p>\n
Yozgat \u00c7aml\u0131\u011f\u0131 Milli Park\u0131<\/p>\n
\u0130\u00e7 Anadolu b\u00f6lgesinde, Yozgat ilinin g\u00fcneyinde uzanan tepeler \u00fczerinde yer al\u0131r.
\nMilli park, \u0130\u00e7 Anadolu\u2019da insan etkisi ile meydana gelen (antropojen) step i\u00e7erisinde yer alan say\u0131l\u0131 orman adalar\u0131ndan biridir. Sahadaki arazinin morfolojik \u00f6zelliklerini tepeler, s\u0131rtta ve vadilerde par\u00e7alanm\u0131\u015f dalgal\u0131 d\u00fczl\u00fckler meydana getirmektedir.
\nKara\u00e7am, me\u015fe ve ard\u0131\u00e7 a\u011fa\u00e7 topluluklar\u0131 milli park bitki \u00f6rt\u00fcs\u00fcn\u00fc meydana getirmektedir. Bu orman par\u00e7as\u0131n\u0131n tabiat b\u00f6lgesi \u00f6zelli\u011fi yan\u0131nda rekreasyon ihtiyac\u0131n\u0131 kar\u015f\u0131lamas\u0131 bak\u0131m\u0131ndan b\u00fcy\u00fck \u00f6nemi bulunmaktad\u0131r.<\/p>\n
Ankara \u0130li<\/p>\n
So\u011fuksu Milli Park\u0131<\/p>\n
Kapl\u0131calar\u0131yla \u00fcnl\u00fc K\u0131z\u0131lcahamam il\u00e7esine 2 km. mesafede bulunur.
\n\u0130\u00e7 Anadolu stepinde Kuzey Anadolu\u2019nun g\u00fcr ve ye\u015fil ormanl\u0131k b\u00f6lgelerine ge\u00e7i\u015f ku\u015fa\u011f\u0131nda yer alan saha, iki ana vadiye a\u00e7\u0131lan pek \u00e7ok yan dere ve vadiler aras\u0131 d\u00fczl\u00fcklerden meydana gelen jeomorfolojik bir yap\u0131ya sahiptir. Andezit, bazalt, t\u00fcf ve anglomeralar jeolojik yap\u0131n\u0131n ana kaya\u00e7lar\u0131d\u0131r.
\nMilli parkta zengin bitki \u00f6rt\u00fcs\u00fc ve yaban hayvanlar\u0131 g\u00f6r\u00fclmektedir.<\/p>\n
\u00c7orum \u0130li<\/p>\n
Alacah\u00f6y\u00fck Tarihi Milli Park\u0131 <\/p>\n
\u0130\u00e7 Anadolu b\u00f6lgesinde, \u00c7orum ili Sungurlu il\u00e7esi s\u0131n\u0131rlar\u0131 i\u00e7erisinde yer almaktad\u0131r.
\nMilli park\u0131n ana de\u011feri, arkeolojik de\u011ferlerdir. Anadolu\u2019nun en \u00f6nemli medeniyetlerinden olan Hititlere ba\u015fkentlik yapm\u0131\u015f olan Bo\u011fazk\u00f6y (Hattu\u015fa\u015f) kentine ait kal\u0131nt\u0131lar bulunmaktad\u0131r. Saha, do\u011fal de\u011ferler a\u00e7\u0131s\u0131ndan; insan eliyle Anadolu platosu\u2019nun flora ve faunas\u0131na yap\u0131lan tahribat\u0131 g\u00f6stermesi sebebiyle \u00f6rnek bir g\u00f6r\u00fcn\u00fcm sunar. Orman \u00f6rt\u00fcs\u00fcn\u00fcn yerini antropojen step araziye b\u0131rakmas\u0131 sonucu hayvan varl\u0131\u011f\u0131 de\u011fi\u015fmi\u015ftir. Genel olarak saha, \u00e7iftlik ve otlatma i\u00e7in kullan\u0131lan hemen hemen a\u011fa\u00e7s\u0131z bir step g\u00f6r\u00fcnt\u00fcs\u00fc kazanm\u0131\u015ft\u0131r.<\/p>\n
Konya \u0130li<\/p>\n
Bey\u015fehir G\u00f6l\u00fc Milli Park\u0131 <\/p>\n
Konya ili Bey\u015fehir il\u00e7esi s\u0131n\u0131rlar\u0131 i\u00e7erisinde yer almaktad\u0131r.
\n\u00dclkemizin \u00fc\u00e7\u00fcnc\u00fc b\u00fcy\u00fck g\u00f6l\u00fc olan Bey\u015fehir g\u00f6l\u00fcn\u00fcn jeomorfolojik yap\u0131s\u0131 karstik arazi \u015fekillerinden, \u00e7ok say\u0131da d\u00fcden ve dolinlerin birle\u015fmesi sonucu olu\u015fan polye karakterindedir. Y\u00f6renin genel jeolojik yap\u0131s\u0131n\u0131 te\u015fkil eden kalkerlerin, sular\u0131n kimyasal reaksiyonu sonucu ezilmesi, bu karstik yer \u015fekillerinin kal\u0131nt\u0131lar\u0131 olan ve y\u00fckseklikleri 20-50 m. aras\u0131nda de\u011fi\u015fen \u00e7ok say\u0131da ada bulunmaktad\u0131r.
\nG\u00f6l suyu alkalin \u00f6zelliktedir. G\u00f6l i\u00e7erisinde irili ufakl\u0131 adalar vard\u0131r. Milli park\u0131n orman formasyonu ard\u0131\u00e7, kara\u00e7am, g\u00f6knar, sedir ve me\u015fe t\u00fcrleri olu\u015fturmakta a\u011fa\u00e7lar yer yer g\u00f6l kenar\u0131na kadar uzanarak Bey\u015fehir g\u00f6l\u00fcn\u00fcn koylar\u0131n\u0131 ve k\u00f6rfezlerini g\u00f6rsel a\u00e7\u0131dan e\u015fsiz manzara g\u00fczelliklerini kavu\u015ftururlar. <\/p>\n
Nev\u015fehir \u0130li<\/p>\n
G\u00f6reme Tarihi Milli Park\u0131<\/p>\n
\u0130\u00e7 Anadolu b\u00f6lgesinde Nev\u015fehir s\u0131n\u0131rlar\u0131 i\u00e7erisinde yer almaktad\u0131r.
\nMilli park Orta Anadolu\u2019nun Hasan da\u011f\u0131-Erciyes da\u011f\u0131 volkanik b\u00f6lgesinde kalmaktad\u0131r. Saha; platolar, ovalar, k\u00fc\u00e7\u00fck da\u011f bitkileri, y\u00fcksek tepeler, al\u00fcvyonla dolmu\u015f dere ve \u0131rmak vadileri, drenaj havzalar\u0131 ve erozyonlu dik yama\u00e7l\u0131 vadilerde birbirinden ayr\u0131lan y\u00fcksek d\u00fczl\u00fcklerden olu\u015fmu\u015ftur. Erciyes ve Hasan da\u011f\u0131n\u0131n b\u00fcy\u00fck volkanik konileri, kuzeyden K\u0131z\u0131l\u0131rmak vadisinin bir k\u0131sm\u0131, baz\u0131lar\u0131 bazaltla kapl\u0131 a\u015f\u0131nm\u0131\u015f t\u00fcf yataklar\u0131 araziye h\u00e2kim \u00f6zelliktedir.
\nAlan; volkanik t\u00fcften olu\u015fmu\u015f ilgi \u00e7ekici manzara yap\u0131s\u0131 i\u00e7erisinde Bizans kilise mimarisi ve dinsel sanat tarihinden \u00f6nemli bir devri sergilemektedir. Yukar\u0131da anlat\u0131lan; G\u00f6reme\u2019nin e\u015fsiz jeomorfolojik olu\u015fumu, estetik manzara yap\u0131s\u0131n\u0131n g\u00f6rsel de\u011ferleri ile tarihi ve etnolojik yap\u0131s\u0131 milli park\u0131n kaynak zenginli\u011finin ana ba\u015fl\u0131klar\u0131 say\u0131labilir.<\/p>\n
Ni\u011fde \u0130li<\/p>\n
Alada\u011flar Milli Park\u0131<\/p>\n
Ni\u011fde, Kayseri ve Adana illeri s\u0131n\u0131rlar\u0131 i\u00e7erisindedir.
\nJeolojik yap\u0131 a\u00e7\u0131s\u0131ndan Alada\u011flar milli park\u0131 de\u011fi\u015fik zamanlara ait formasyonlarla temsil edilmekle birlikte, en yayg\u0131n formasyon mezozoik ya\u015fl\u0131 kire\u00e7 ta\u015flar\u0131d\u0131r. Bunun yan\u0131nda sahada entr\u00fcsif volkanizman\u0131n \u00fcr\u00fcn\u00fc olan gabro, piroksenit gibi kaya\u00e7lara, suboflolitik metamorfiklere ve daha geni\u015f d\u00f6nemlerdi karakterize eden tersiyer ve kuaterner oluklar\u0131na da rastlanmaktad\u0131r.
\nAlada\u011flar y\u00f6resi \u00fclkemizin tektonik a\u00e7\u0131dan en faal b\u00f6lgelerinden birisidir. Y\u00f6re \u00f6zellikle Alp orojenezi s\u0131ras\u0131nda \u015faryaj ve bindirmelere sahne olmu\u015ftur. Tektonik literat\u00fcr\u00fcne \u201cEcemi\u015f Koridoru\u201d olarak da giren bu sahada d\u00fc\u015fey ve yatay at\u0131ml\u0131 bir\u00e7ok fay bulunmaktad\u0131r. Dokusuyla y\u00f6rede jeomorfolojik s\u00fcre\u00e7ler sonucu olu\u015fan naplar, klipler, pencereler ilgin\u00e7 yap\u0131sal unsurlar olarak dikkati \u00e7eker.
\nY\u00f6renin \u015fekillenmesinde yap\u0131 ile fl\u00fcvial ko\u015fullar ve Pleistosen buzulla\u015fmas\u0131 \u00f6nemli bir rol oynam\u0131\u015ft\u0131r. Y\u00f6rede bu \u00fc\u00e7 unsura ait de\u011fi\u015fik morfolojik birimlere rastlamak \u00e7ok ola\u011fand\u0131r. Y\u00f6renin belli ba\u015fl\u0131 jeomorfolojik karakteri vadilerle de bir \u015fekilde par\u00e7alanm\u0131\u015f olmas\u0131d\u0131r. Buzul mitolojisine ait bir\u00e7ok izlere rastlanmakta, \u00f6zellikle y\u00f6redeki bir\u00e7ok sirk g\u00f6lleri ve moraller bu morfolojinin k\u0131lavuz \u015fakileri olarak g\u00f6r\u00fcl\u00fcr. Buras\u0131 klimatik a\u00e7\u0131dan kendine has \u00f6zelliklere sahiptir. Alada\u011flar milli park\u0131 vejetasyon a\u00e7\u0131s\u0131ndan \u00e7ok zengin olup, orman\u0131 olu\u015fturan h\u00e2kim t\u00fcrler kara\u00e7am ve k\u0131z\u0131l\u00e7amd\u0131r. Orman\u0131n \u00fcst s\u0131n\u0131r\u0131ndan itibaren Alp\u0131n zon ba\u015flar.<\/p>\n
Karadeniz B\u00f6lgesi<\/p>\n
Trabzon ili<\/p>\n
Alt\u0131ndere Vadisi Milli Park\u0131 <\/p>\n
Do\u011fu Karadeniz B\u00f6lgesinde, Trabzon ili Ma\u00e7ka il\u00e7esi s\u0131n\u0131rlar\u0131 i\u00e7erisinde yer almaktad\u0131r.
\nMilli park\u0131n ana \u00f6zelli\u011fini S\u00fcmela Manast\u0131r\u0131 ile Alt\u0131ndere Vadisinin bitki zenginli\u011fi ve jeomorfolojik yap\u0131s\u0131 te\u015fkil etmektedir. Meryem ana ad\u0131na kurulan S\u00fcmela manast\u0131r\u0131, Alt\u0131ndere\u2019nin bat\u0131 yamac\u0131ndad\u0131r. Manast\u0131r; \u015fapel, kilise ve di\u011fer kompleksleriyle sanat tarihinde \u00f6nemli bir yer tutar.
\nMilli park, flora a\u00e7\u0131s\u0131ndan \u00e7ok zenginlik i\u00e7ermekte olup y\u00f6renin hakim bitki \u00f6rt\u00fcs\u00fcn\u00fc do\u011fu ladini olu\u015fturur. Zengin bitki \u00f6rt\u00fcs\u00fc \u00e7e\u015fitlili\u011fi g\u00f6r\u00fclmeye de\u011fer do\u011fal ortam\u0131n yaban hayat\u0131 i\u00e7in sundu\u011fu ya\u015fam \u015fartlar\u0131 bir\u00e7ok hayvan\u0131n ya\u015famas\u0131na ve \u00e7o\u011falmas\u0131na olanak sa\u011flam\u0131\u015ft\u0131r.<\/p>\n
Rize \u0130li<\/p>\n
Ka\u00e7kar Da\u011flar\u0131 Milli Park\u0131<\/p>\n
Rize ili, \u00c7aml\u0131hem\u015fin il\u00e7esi s\u0131n\u0131rlar\u0131 i\u00e7erisinde yer almaktad\u0131r.
\nKa\u00e7kar da\u011flar\u0131n\u0131n bat\u0131s\u0131ndaki F\u0131rt\u0131na deresi ve do\u011fusundaki Hem\u015fin deresi zengin bir flora ile kapl\u0131d\u0131r. Bu bitki \u00f6rt\u00fcs\u00fc karstik flora \u00f6zelli\u011finde olup gerek alt flora gerekse \u00fcst flora endemik t\u00fcrleri i\u00e7ermektedir. T\u00fcrkiye\u2019de Rhodendron\u2019lar\u0131n 3000 m. ye ula\u015ft\u0131\u011f\u0131 tek yer buras\u0131d\u0131r.
\n\u00dclkemizde Pleistosen\u2019e ait buzul izleriyle beraber akt\u00fcel buzla\u015fman\u0131n birlikte g\u00f6r\u00fcld\u00fc\u011f\u00fc ender yerlerden birisi de Ka\u00e7kar da\u011flar\u0131d\u0131r. Genel olarak granit ve granitik kaya\u00e7lardan meydana gelen jeolojik yap\u0131 \u00fczerinde Alp orojenezinin derin etkileri g\u00f6r\u00fclmektedir.<\/p>\n
Bolu \u0130li<\/p>\n
Yedig\u00f6ller Milli Park\u0131<\/p>\n
Milli park; Bat\u0131 Karadeniz b\u00f6lgesinde Bolu ilinin kuzeyinde Zonguldak ilinin g\u00fcneyinde yer al\u0131r.
\nYer yap\u0131s\u0131 serpantinlerden ve volkanik kaya\u00e7lardan olu\u015fan sahada zaman zaman g\u00f6\u00e7\u00fck yer hareketleri s\u00fcr\u00fcklenmeye haz\u0131r arazi yap\u0131s\u0131, g\u00f6llerin meydana gelmesini haz\u0131rlayan ba\u015fl\u0131ca fakt\u00f6rlerdir. G\u00f6ller, kayan kitlelerin, vadilerin \u00f6nlerini kapamas\u0131 sonucu arkada sular\u0131n birikti\u011fi set g\u00f6lleridir. Bunlardan baz\u0131lar\u0131 dip ka\u00e7aklar\u0131 ile birbirine ba\u011flant\u0131l\u0131d\u0131r.
\nMilli parka h\u00e2kim bitki \u00f6rt\u00fcs\u00fc kay\u0131n a\u011fa\u00e7lar\u0131d\u0131r. \u00dclkemizde ilk k\u00fclt\u00fcr alabal\u0131\u011f\u0131 \u00fcretme istasyonu 1969 y\u0131l\u0131nda bu milli parkta kurulmu\u015ftur. Dolay\u0131s\u0131yla rekrasyonel a\u00e7\u0131dan olta bal\u0131k\u00e7\u0131l\u0131\u011f\u0131na kaynak olmu\u015ftur. <\/p>\n
Artvin \u0130li<\/p>\n
Karag\u00f6l Sahara Milli Park\u0131<\/p>\n
Artvin ili \u015eav\u015fat il\u00e7esi s\u0131n\u0131rlar\u0131nda bulunan Karag\u00f6l Sahara Milli Park\u0131 iki ayr\u0131 sahadan olu\u015fmaktad\u0131r. Bunlar Karag\u00f6l ve Sahara yaylas\u0131d\u0131r.
\nKarag\u00f6l ve \u00e7evresinden genel olarak paleojen ve neojen arazileri yer al\u0131r. Kaya\u00e7lar genellikle sedimenter k\u00f6kenlidir. Karag\u00f6l rotasyon el olarak kayan k\u00fctlenin gerisindeki \u00e7anakta biriken sular\u0131n meydana getirdi\u011fi bir heyelan g\u00f6l\u00fcd\u00fcr. G\u00f6l \u00e7evresi ladin ve \u00e7amlar\u0131n meydana getirdi\u011fi yo\u011fun ormanlarla kapl\u0131d\u0131r.
\nSahara yaylas\u0131; y\u00f6renin genel olarak \u00f6rt\u00fc bazaltlar\u0131ndan meydana gelen jeolojik yap\u0131s\u0131 vard\u0131r. \u00d6rt\u00fc bazaltlar\u0131n\u0131n s\u0131yr\u0131ld\u0131\u011f\u0131 yerlerde tersiyer arazisi ortaya \u00e7\u0131kar. Orman \u00f6rt\u00fcs\u00fc ladin ve g\u00f6knarlardan meydana gelmi\u015ftir. Re\u015fat deresi kenar\u0131nda 1700\u20131800 m.lerde kademeli olarak yer alan d\u00fczl\u00fckler ayn\u0131 zamanda \u201cSahara Pancar \u015eenlikleri\u201dne saha olmaktad\u0131r. B\u00f6lge i\u00e7 turizm a\u00e7\u0131s\u0131ndan olduk\u00e7a b\u00fcy\u00fck ekonomik katk\u0131 sa\u011flamaktad\u0131r.
\nHat\u0131la Vadisi Milli Park\u0131
\nArtvin ili merkez il\u00e7e s\u0131n\u0131rlar\u0131 i\u00e7erisinde \u00c7oruh nehrinin ana kollar\u0131ndan birisi olan hat\u0131la vadisi ve bir\u00e7ok yan derelerini i\u00e7ermektedir.
\nVadi boyunca de\u011fi\u015fik kaya\u00e7 t\u00fcrleri g\u00f6r\u00fclmekle birlikte, bu kaya\u00e7lar\u0131n hemen hepsi derinlik volkanizmas\u0131n\u0131n bir \u00fcr\u00fcn\u00fcd\u00fcr. Hat\u0131la vadisinin genel karakteri; V tipi, dar tabanl\u0131, gen\u00e7 vadi \u00f6zelli\u011findedir. Vadi boyunca litolojik farkl\u0131l\u0131klardan kaynaklanan e\u011fim k\u0131r\u0131klar\u0131 ortaya \u00e7\u0131km\u0131\u015ft\u0131r. Yama\u00e7lar\u0131n gerek fiziksel par\u00e7alanma ve k\u00fctle hareketleri gerekse yan dere ve heyelanlarla i\u015flenmesi sonucu vadide, \u00e7ok ha\u015fin bit topografya ortaya \u00e7\u0131km\u0131\u015ft\u0131r.
\nVadinin orta ve yukar\u0131 a\u011fz\u0131nda \u00e7ok zengin ve yo\u011fun olan vejetetif \u00f6rt\u00fc; b\u00fcnyesindeki \u00e7ok \u00e7e\u015fitli bitki t\u00fcrlerini bar\u0131nd\u0131rmaktad\u0131r. Bitki \u00f6rt\u00fcs\u00fc genel olarak Akdeniz iklim karakteri g\u00f6stermektedir. Hat\u0131la vadisi zengin bir fauna da i\u00e7ermektedir.<\/p>\n
Kastamonu \u0130li<\/p>\n
Ilgaz Da\u011f\u0131 Milli Park\u0131<\/p>\n
Bat\u0131 Karadeniz b\u00f6lgesinde, \u00c7ank\u0131r\u0131 ve Kastamonu il s\u0131n\u0131rlar\u0131 i\u00e7erisinde yer almaktad\u0131r.
\nIlgaz da\u011fl\u0131k y\u00f6resinin arazi yap\u0131s\u0131 genellikle serpantinler, \u015fistler ve volkanik kaya\u00e7lardan meydana gelir. \u00dcst\u00fcn peyzaj g\u00fczellikleri sunan jeomorfolojik yap\u0131ya sahiptir. Ilgaz da\u011f\u0131n\u0131n eteklerinden doruklar\u0131na do\u011fru geli\u015fen kara\u00e7am, sar\u0131\u00e7am, g\u00f6knar h\u00e2kim a\u011fa\u00e7 t\u00fcrlerinden meydana gelen bitki \u00f6rt\u00fcs\u00fc, zengin ormanalt\u0131 toplulu\u011fu ile desteklenmektedir. Milli park\u0131n di\u011fer \u00f6nemli bir kayna\u011f\u0131 da k\u0131\u015f sporlar\u0131 imk\u00e2n\u0131d\u0131r.<\/p>\n
Do\u011fu Anadolu B\u00f6lgesi<\/p>\n
Tunceli \u0130li<\/p>\n
Munzur Vadisi Milli Park\u0131<\/p>\n
Do\u011fu Anadolu b\u00f6lgesinde Tunceli ili s\u0131n\u0131rlar\u0131 i\u00e7inde yer almaktad\u0131r.
\nKarasu ve Murat \u00e7\u00f6k\u00fcnt\u00fcs\u00fc alanlar\u0131 aras\u0131nda y\u00fckselen Munzur da\u011flar\u0131n\u0131n jeolojik yap\u0131s\u0131, metamorfik, volkanik ve tortul kaya\u00e7lardan meydana gelir.Mercan vadisinin 1.60 metreden yukar\u0131 kesimlerinde buzul g\u00f6lleri, da\u011flardan Ovac\u0131k d\u00fczl\u00fc\u011f\u00fcne gelindi\u011finde kaynayan g\u00f6zeler, vadi boyunca d\u00f6k\u00fclen k\u00fc\u00e7\u00fck \u015felaleler milli park\u0131n peyzaj\u0131nda ilgi \u00e7ekici \u00f6rnekleridir.Milli parkta tepeler ve yama\u00e7lar me\u015fe ormanlar\u0131 ile kapl\u0131d\u0131r.Burada nadir t\u00fcrlerinde bulundu\u011fu yaban hayat\u0131 vard\u0131r.<\/p>\n
Ad\u0131yaman \u0130li<\/p>\n
Nemrut Da\u011f\u0131 Milli Park\u0131<\/p>\n
Ad\u0131yaman ili; K\u00e2hta il\u00e7esi s\u0131n\u0131rlar\u0131 i\u00e7erisinde yer almaktad\u0131r.
\nNemrut da\u011f\u0131 ve Kommagene Kral\u0131 Anticohos\u2019a ait T\u00fcm\u00fcl\u00fcs, milli park\u0131n ana kaynak de\u011ferini te\u015fkil etmektedir. Anticohos\u2019un t\u00fcm\u00fcl\u00fcs\u00fc ve dev heykelleri, Arsameia (Eskikale), Yenikale, Karaku\u015f Tepe ve Cendere K\u00f6pr\u00fcs\u00fc milli park i\u00e7erisinde kalan k\u00fclt\u00fcrel de\u011ferlerdir. Nemrut da\u011f\u0131 doru\u011fundaki kal\u0131nt\u0131lar\u0131 yerle\u015fme yeri olmay\u0131p Anticohos\u2019un t\u00fcm\u00fcl\u00fcs\u00fc ve kutsal alanlard\u0131r. T\u00fcm\u00fcl\u00fcs, 2150 m. y\u00fcksekli\u011finde, F\u0131rat nehri ge\u00e7itlerine ve ovalar\u0131na h\u00e2kim tepe \u00fczerinde bulunmaktad\u0131r.
\nOrman formasyonu i\u00e7erisinde me\u015fe t\u00fcrleri ve a\u011fa\u00e7 alanlar\u0131 bulunur.\t<\/p>\n","protected":false},"excerpt":{"rendered":"
MARMARA B\u00d6LGES\u0130 \u00c7anakkale \u0130li Gelibolu Yar\u0131madas\u0131 Tarihi Milli Park\u0131 1973\u2019te kurulmu\u015f ve BM Milli Parklar ve Koruma Alanlar\u0131 listesinde olan park, \u00c7anakkale ili s\u0131n\u0131rlar\u0131 i\u00e7erisinde, Gelibolu Yar\u0131madas\u0131n\u0131n g\u00fcney ucunda, \u00c7anakkale bo\u011faz\u0131n\u0131n Avrupa yakas\u0131nda 33,000 hektarl\u0131k bir alan\u0131 kapsamaktad\u0131r. Birinci D\u00fcnya Sava\u015f\u0131 \u00c7anakkale Deniz ve Kara Muhaberelerinin yap\u0131ld\u0131\u011f\u0131 yerler park i\u00e7erisindedir. Muharebe alanlar\u0131, sava\u015f mezarlar\u0131, an\u0131tlar …<\/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":[2811,2808,2802,2804,2809,2805,2807,2801,2806,2810,2803],"class_list":["post-939","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-altindere-vadisi-milli-parki","tag-aluvyon","tag-canakkale-bogazi","tag-kazdagi-milli-parki","tag-kizildag-milli-parki","tag-kus-cenneti-milli-parki","tag-marmaris-milli-parki","tag-milli-parklarimiz","tag-saklikent-milli-parki","tag-sarkikaraagac","tag-uludag-milli-parki"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/939","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=939"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/939\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=939"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=939"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=939"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}