{"id":32180,"date":"2025-03-05T00:23:23","date_gmt":"2025-03-04T21:23:23","guid":{"rendered":"https:\/\/www.bilgiajansi.net\/?p=32180"},"modified":"2025-03-05T00:23:23","modified_gmt":"2025-03-04T21:23:23","slug":"yanardag-volkan-olusumu-yanardaglarin-ozellikleri-yanardag-puskurmesi","status":"publish","type":"post","link":"https:\/\/buradasin.com.tr\/kutuphane\/yanardag-volkan-olusumu-yanardaglarin-ozellikleri-yanardag-puskurmesi\/","title":{"rendered":"Yanarda\u011f Volkan Olu\u015fumu, Yanarda\u011flar\u0131n \u00d6zellikleri, Yanarda\u011f P\u00fcsk\u00fcrmesi"},"content":{"rendered":"
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<\/i> Payla\u015f<\/b><\/span><\/i><\/i><\/i><\/i><\/i><\/i><\/i><\/div>\n<\/div>\n
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Yanarda\u011f (volkan)<\/strong>, olu\u015fumlar\u0131 tektonik hareketlere ba\u011fl\u0131 olarak yeralt\u0131ndaki ergimi\u015f kayalar\u0131n, kaya par\u00e7alar\u0131n\u0131n ve gazlar\u0131n yer kabu\u011fundaki zay\u0131f noktalardan yer y\u00fcz\u00fcne p\u00fcsk\u00fcrtt\u00fc\u011f\u00fc s\u0131cak lav (erimi\u015f kaya) par\u00e7alar\u0131d\u0131r. Yer y\u00fcz\u00fcne yay\u0131larak ilerleyen bu par\u00e7ac\u0131klar\u0131n \u00fcst \u00fcste birikmesiyle olu\u015fan bu birikintiler so\u011fumaya ba\u015flamas\u0131yla kat\u0131la\u015f\u0131r ve yanar da\u011f ismini y\u00fckseltilerinden al\u0131rlar. \u00a0Depremler gibi yanarda\u011flar\u0131n da \u00e7o\u011fu levha s\u0131n\u0131rlar\u0131na yak\u0131n yerlerde bulunur.\u00d6te yandan, nas\u0131l ki, levha s\u0131n\u0131rlar\u0131na uzak yerlerde de zaman zaman deprem olursa, baz\u0131 yanarda\u011flar da levhalar\u0131n i\u00e7 b\u00f6l\u00fcmlerinde bulunur.<\/p>\n

\"\"yanarda\u011f nedir, volkan nas\u0131l p\u00fcsk\u00fcr\u00fcr, yanarda\u011f volkan olu\u015fumu, magma nedir, lav, yanarda\u011f volkanlar\u0131n \u00f6zellikleri, t\u00fcrkiyenin bilinen aktif yanarda\u011flar\u0131, p\u00fcsk\u00fcrme \u015fekilleri, k\u00fcl bulutlar\u0131, yanarda\u011f volkan patlamas\u0131<\/p>\n

Yay\u0131lma S\u0131rtlar\u0131:<\/strong><\/p>\n

Okyanus dibinde. \u0130ki levhan\u0131n birbirinden uzakla\u015fmakta oldu\u011fu s\u0131n\u0131rda ,okyanus ortas\u0131 s\u0131rtlar\u0131 ya da yay\u0131lma s\u0131rtlar\u0131 ad\u0131 verilen yanarda\u011flardan olu\u015fan s\u0131ra da\u011flar vard\u0131r. Levha birbirinden ayr\u0131ld\u0131klar\u0131nda astenosfer \u00fczerindeki bas\u0131n\u00e7 azal\u0131r.Bunun sonucunda, levha s\u0131n\u0131r\u0131n\u0131n alt\u0131nda bulunan kat\u0131 durumdaki minareler tanecikleri ergiyerek magmaya d\u00f6n\u00fc\u015f\u00fcr.Y\u00fckselmeye ba\u015flayan yeni magman\u0131n \u00e7o\u011fu levha kenarlar\u0131nda kat\u0131la\u015f\u0131p kal\u0131r, y\u00fczeye ula\u015fan b\u00f6l\u00fcm\u00fc ise okyanus taban\u0131nda yanarda\u011flar olu\u015fturur.<\/p>\n

Plastik Kayalar:<\/strong><\/p>\n

Bilim adamlar\u0131, astenosferi genellikle \u201cplastik\u201d olarak tan\u0131mlarlar.Bunun nedeni, astenosferin b\u00fcy\u00fck bir b\u00f6l\u00fcm\u00fcn yumu\u015fsak olmas\u0131na kar\u015f\u0131n , s\u0131v\u0131dan \u00e7ok k\u00fc\u00e7\u00fck miktarlarda magma bulunan kat\u0131 mineral taneciklerinden olu\u015ftu\u011funu d\u00fc\u015f\u00fcn\u00fcyorlar.Astenosferdeki s\u0131cakl\u0131\u011f\u0131n , minerallerin \u00e7o\u011funu ergitmeye yetecek kadar y\u00fcksek olmas\u0131na kar\u015f\u0131n ,\u00fcsteki litosfer katman\u0131n neden oldu\u011fu yo\u011fun bas\u0131n\u00e7 bunu engeller.<\/p>\n

Dalma-Batma B\u00f6lgesi Yanarda\u011flar\u0131:<\/strong><\/p>\n

Yanarda\u011flar, iki levhan\u0131n \u00e7arp\u0131\u015fmas\u0131 sonucu birinin di\u011feri alt\u0131na dald\u0131\u011f\u0131 levha s\u0131n\u0131rlar\u0131nda olu\u015fur.Dalan levha, 100-200 km derinlikte bulunan ve dalma-batma b\u00f6lgesi ad\u0131 verilen b\u00f6lgede ergimeye ba\u015flar ve magmaya d\u00f6n\u00fc\u015f\u00fcr.Bu magma, levhan\u0131n \u00fczerinde biriken tortullar ve ergimi\u015f durumdaki okyanusal litosferden olu\u015fur.Magma ,tortullarla birlikte yerin derinliklerine \u00e7ekilen su i\u00e7erir.Olu\u015fan yeni magma ,\u00e7atlaklardan ge\u00e7erek y\u00fczeye p\u00fcsk\u00fcr\u00fcr ve \u00fcstteki levhan\u0131n \u00fczerinde yanarda\u011flar\u0131n olu\u015fuma yol a\u00e7ar.Bu \u00e7atlaklar ,levhalar\u0131n hareketi sonucunda olu\u015fur. \u00dcstteki levhan\u0131n okyanusal litosfer levhas\u0131 olmas\u0131 durumunda ,yanarda\u011flar\u0131n su y\u00fczeyinin \u00fczerinde kalan b\u00f6l\u00fcmleri bir dizi volkanik ada olu\u015fturur.<\/p>\n

Magma:<\/strong><\/p>\n

Magma, ergimi\u015f durumdaki de\u011fi\u015fik mineraller ve baz\u0131 mineral kristallerinde olu\u015fan lapa benzeri, yo\u011fun bir s\u0131v\u0131d\u0131r.K\u0131vam\u0131, su ve buz kristalleri i\u00e7eren yar\u0131 erimi\u015f durumdaki kar gibidir.Bilim adamlar\u0131 ,magman\u0131n b\u00fcy\u00fck \u00e7o\u011funlu\u011funun astenosferde bulunmakla birlikte bir b\u00f6l\u00fcm\u00fcn\u00fcn de alt mantonun baz\u0131 b\u00f6lgelerinde geldi\u011fini d\u00fc\u015f\u00fcn\u00fcyorlar.<\/p>\n

S\u0131cak Noktalar:<\/strong><\/p>\n

Bir\u00e7ok yanarda\u011f\u0131n olu\u015fumunun levha s\u0131n\u0131rlar\u0131ndaki hareketle ba\u011flant\u0131l\u0131 olmas\u0131na kar\u015f\u0131n baz\u0131lar\u0131 bu s\u0131n\u0131rlara uzak yerlerde ortaya \u00e7\u0131kabilir.Bu yanarda\u011flar\u0131n s\u0131cak noktalar olarak adland\u0131r\u0131lan ola\u011fan\u00fcst\u00fc s\u0131cak b\u00f6lgelerin varl\u0131\u011f\u0131 sonucunda olu\u015ftuklar\u0131 d\u00fc\u015f\u00fcn\u00fcl\u00fcyor.<\/p>\n

Bilim adamlar\u0131, s\u0131cak noktalar\u0131n astenosfer ve alt mantoda bulundu\u011fu varsay\u0131l\u0131yor.S\u0131cak noktalarda, \u0131s\u0131 ak\u0131mlar\u0131n\u0131n mantonun i\u00e7inden ge\u00e7erek y\u00fckseldi\u011fi tahmin ediliyor.Bu ola\u011fan\u00fcst\u00fc \u0131s\u0131n\u0131n bas\u0131nc\u0131n etkisini ortadan kald\u0131r\u0131lmas\u0131 sonucunda da magma olu\u015fur.Y\u00fczeye do\u011fru \u00e7\u0131kan magma, litosferden ge\u00e7i\u015f s\u0131ras\u0131nda, yolunun \u00fczerindeki kaya k\u00fctlelerini ergiterek kendisine yol a\u00e7ar.Magman\u0131n y\u00fczeye \u00e7\u0131kt\u0131\u011f\u0131 yerlerde zamanla yanarda\u011flar olu\u015fur.<\/p>\n

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YANARDA\u011e P\u00dcSK\u00dcRMELER\u0130:<\/strong><\/p>\n

Magman\u0131n yerkabu\u011fundan y\u00fckselerek y\u00fczeye \u00e7\u0131kmas\u0131na yanarda\u011f p\u00fcsk\u00fcrmesi ad\u0131 verilir.Yanarda\u011f bir kez olu\u015ftuktan sonra yeralt\u0131ndan magma geldi\u011fi s\u00fcrece p\u00fcsk\u00fcrmeler devam eder.\u0130ki p\u00fcsk\u00fcrme aras\u0131nda onlarca, y\u00fczlerce, hatta binlerce y\u0131l ge\u00e7bilir.<\/p>\n

Magma Y\u00fckseli\u015fi:<\/strong><\/p>\n

Astenosferdeki magma, ancak yeterince b\u00fcy\u00fck bir \u201ckabarc\u0131k\u201d olu\u015fturacak bi\u00e7imde birikti\u011fi zaman litosfere do\u011fru y\u00fckselir.Magman\u0131n y\u00fckselmesine yol a\u00e7an s\u00fcre\u00e7, bozuk bir musluktan suyun damlamas\u0131na(ancak ters y\u00f6nde) benzer.Bozuk bir muslukta su s\u00fcrekli bi\u00e7imde muslu\u011fun a\u011fz\u0131nda birikir fakat damla halinde d\u00fc\u015fmesi ancak yeterli a\u011f\u0131rl\u0131\u011fa ula\u015fmas\u0131 ile ger\u00e7ekle\u015fir.Magma da yeralt\u0131nda yeterli derecede birikti\u011finde ve yo\u011funlu\u011fu \u00e7evresindeki kaya k\u00fctlelerinden daha d\u00fc\u015f\u00fck oldu\u011funda yukar\u0131 do\u011fru \u00e7\u0131kmaya ba\u015flar.\u00c7o\u011fu yanarda\u011f\u0131n alt\u0131nda (yerkabu\u011funun i\u00e7inde ya da alt\u0131nda) magman\u0131n birikti\u011fi bir magma odas\u0131 vard\u0131r.<\/p>\n

yanarda\u011f\u0131n Alt\u0131:<\/strong><\/p>\n

Magma odas\u0131 il yanarda\u011f\u0131n y\u00fczeyi aras\u0131nda kanal ya da baca olarak adland\u0131r\u0131lan geni\u015flemi\u015f \u00e7atlaklar bulunur.Bunlar bir \u00f6nceki patlamalardan arta kalan kat\u0131la\u015fm\u0131\u015f magma ile doludur.baz\u0131 yanarda\u011flarda, magma odas\u0131ndan \u00e7\u0131kan \u00e7ok say\u0131da baca olmak ile birlikte bunlar\u0131n hepsi y\u00fczeye ula\u015fmayabilir.Bir bacan\u0131n a\u00e7\u0131ld\u0131\u011f\u0131 yere a\u011f\u0131z denir.Yanarda\u011f a\u011f\u0131zlar\u0131 yuvarlak ya da ince uzun bi\u00e7imde olabilir.Baz\u0131 a\u011f\u0131zlar, krater ad\u0131 verilen derin \u00e7ukurlar\u0131n i\u00e7inde bulunur.Bir p\u00fcsk\u00fcrme s\u0131ras\u0131nda, magma, birikti\u011fi magma odas\u0131ndan y\u00fczeye \u00e7\u0131kan bacalardan birinden ge\u00e7erek,yanarda\u011f\u0131n tepesindeki a\u011f\u0131za ula\u015f\u0131r ve buradan d\u0131\u015far\u0131 f\u0131\u015fk\u0131r\u0131r. Baz\u0131 durumlarda ise magma ,yanarda\u011f\u0131n yamac\u0131ndaki bir a\u011f\u0131zdan \u00e7\u0131kar.<\/p>\n

Lav:<\/strong><\/p>\n

P\u00fcsk\u00fcrme s\u0131ras\u0131nda y\u00fczeye \u00e7\u0131kan magma lav ad\u0131n\u0131 al\u0131r.yanarda\u011f\u0131n yama\u00e7lar\u0131ndan, lavdan olu\u015fan bir nehir gibi akan lav ak\u0131nt\u0131s\u0131n\u0131n zaman so\u011fuyup kat\u0131la\u015fmas\u0131yla volkanik kayalar olu\u015fur.\u00c7e\u015fitli t\u00fcrlerde lav bulunmakla birlikte bunlar\u0131n t\u00fcm\u00fc nerdeyse di\u011fer mineral elementlerinin yan\u0131 s\u0131ra bir silisyum ve oksijen kar\u0131\u015f\u0131m\u0131 olan silisyum dioksit (SiO2) i\u00e7erir. Lav\u0131n yo\u011funlu\u011fu ,i\u00e7indeki silisyum dioksit oran\u0131na g\u00f6re de\u011fi\u015fir.Yo\u011fun olmayan lav bal k\u0131vam\u0131ndad\u0131r.Yo\u011fun lav ise \u015fekerlenmi\u015f bal gibi koyu ve yap\u0131\u015fkand\u0131r.Bir patlama s\u0131ras\u0131nda yanarda\u011fdan farkl\u0131 yo\u011funlukta lavlar p\u00fcsk\u00fcrebilir.<\/p>\n

Bir yanarda\u011f\u0131n bi\u00e7imi, b\u00fcy\u00fck oranda, lav\u0131n yo\u011funluna ba\u011fl\u0131d\u0131r.Yo\u011fun olmayan lav kat\u0131la\u015f\u0131ncaya kadar daha geni\u015f bir \u00e7evreye yay\u0131ld\u0131\u011f\u0131ndan ,bu T\u00fcr lavdan olu\u015fan yanar da\u011flar\u0131n yama\u00e7lar\u0131 yumu\u015fak e\u011fimli olur.Kalkan bi\u00e7imli olarak tan\u0131mlanan Bu yanarda\u011flar, \u00e7o\u011fu zaman s\u0131cak noktalar ve yay\u0131lma s\u0131rtlar\u0131nda bulunur.Bu yanarda\u011flar\u0131n lav\u0131 \u00e7o\u011funlukla bazalttan olu\u015fur.Yo\u011fun lav,y\u00fcksek oranda silisyum dioksit i\u00e7erir ve genellikle dalma-batma b\u00f6lgelerinin \u00fczerindeki yanarda\u011flardan p\u00fcsk\u00fcr\u00fcr.\u00c7ok koyu oldu\u011fu i\u00e7in a\u011f\u0131zdan fazla uzakla\u015fmadan kat\u0131la\u015fan bu lav\u0131n olu\u015fturdu\u011fu yanarda\u011flar \u00e7o\u011fu zaman koni bi\u00e7imindedir.<\/p>\n

P\u00fcsk\u00fcrme Tipleri:<\/strong><\/p>\n

yanarda\u011f\u0131n p\u00fcsk\u00fcrmeleri, lav\u0131n \u00e7\u0131k\u0131\u015f bi\u00e7imine g\u00f6re s\u0131n\u0131fland\u0131r\u0131l\u0131r.Bu da lav\u0131n yo\u011funlu\u011funa ve lav\u0131n i\u00e7erdi\u011fi gazlar\u0131n ne kadar kolayl\u0131kla kurtulabilmelerine ba\u011fl\u0131d\u0131r.Yo\u011fun olmayan lavdan kolayca kurtulabilen gazlar, yo\u011fun lavdan ancak b\u00fcy\u00fck patlamalarla kurtulabilirler.<\/p>\n

Magma, y\u00fczeye yakla\u015ft\u0131k\u00e7a \u00fczerindeki bas\u0131n\u00e7 azal\u0131r ve t\u0131pk\u0131 bir gazoz \u015fi\u015fesinin kapa\u011f\u0131 a\u00e7\u0131ld\u0131\u011f\u0131 zaman bas\u0131nc\u0131n azalmas\u0131 sonucu gazozun i\u00e7inde hava kabarc\u0131klar\u0131n\u0131n olu\u015fmas\u0131 gibi volkanik gazlar magman\u0131n i\u00e7inde k\u00fc\u00e7\u00fck kabarc\u0131klar olu\u015fturur.<\/p>\n

Farkl\u0131 p\u00fcsk\u00fcrme tipleri:<\/strong><\/p>\n

\u2013 Hawaii tipi p\u00fcsk\u00fcrmeler genellikle hafif \u015fiddetedir.lav\u0131n \u00e7ok ak\u0131\u015fkan oldu\u011fu ve i\u00e7inde gazlar\u0131n kolayca kurtuldu\u011fu durumlarda bu t\u00fcr p\u00fcsk\u00fcrmeler olur.Kimi zaman magma, yanarda\u011f\u009fdan d\u0131\u015far\u0131, bir f\u0131skiyeden f\u0131\u015fk\u0131ran su gibi \u00e7\u0131kar.<\/p>\n

\u2013 Stromboli tipi p\u00fcsk\u00fcrmeler, lav\u0131n biraz daha yo\u011fun olmas\u0131 durumunda g\u00f6r\u00fcl\u00fcr.S\u0131k\u0131\u015fm\u0131\u015f gazlar, yanarda\u011f a\u011fz\u0131n\u0131n \u00e7evresine s\u0131v\u0131 halde lav k\u00fctlerinin f\u0131\u015fk\u0131rmas\u0131na neden olan, k\u00fc\u00e7\u00fck patlamalarla a\u00e7\u0131\u011fa \u00e7\u0131kar.<\/p>\n

\u2013 Vulkona tipi p\u00fcsk\u00fcrmeler, lav\u0131n daha yo\u011fun oldu\u011fu durumlarda g\u00f6r\u00fcl\u00fcr.S\u0131k\u0131\u015fm\u0131\u015f gazlar g\u00fcr\u00fclt\u00fcl\u00fc patlamalarla a\u00e7\u0131\u011fa \u00e7\u0131kar ve yanarda\u011f\u0131n a\u011fz\u0131na iri kaya par\u00e7alar\u0131 ile \u00e7ok miktarlarda volkanik k\u00fcl p\u00fcsk\u00fcr\u00fcr.<\/p>\n

\u2013 Pilinius tipi p\u00fcsk\u00fcrmeler, lav\u0131n \u00e7ok yo\u011fun olmas\u0131 durumunda g\u00f6r\u00fcl\u00fcr.S\u0131k\u0131\u015fm\u0131\u015f gazlar, \u00e7ok b\u00fcy\u00fck patlamalarla kurtulur.yanarda\u011f\u0131n p\u00fcsk\u00fcrmeleri s\u0131ras\u0131nda b\u00fcy\u00fck miktarlarda volkanik k\u00fcl g\u00f6ky\u00fcz\u00fcne f\u0131rlat\u0131l\u0131r.<\/p>\n

LAV AKINTILARI, BLOKLAR VE BOMBALAR:<\/strong><\/p>\n

P\u00fcsk\u00fcren bir yanarda\u011fdan akan lavlar ,yollar\u0131 yak\u0131p y\u0131kmas\u0131n kar\u015f\u0131n ,\u00e7ok ender olarak \u00f6l\u00fcm yada yaralanmalara yol a\u00e7ar.Bunun nedeni, lav ak\u0131nt\u0131s\u0131n\u0131n yava\u015f ilerlemesi ve insanlar\u0131n ondan ka\u00e7ma ola\u011fan\u0131 bulabilmeleridir.<\/p>\n

Pahoehoe\u00e2 ve iki farkl\u0131 lav ak\u0131ns\u0131na Hawaii dilinde verilen adlard\u0131r.Bunlar birbirlerinden , volkanik gazlar\u0131n lavdan \u00e7\u0131k\u0131\u015f bi\u00e7imiyle ayr\u0131l\u0131r.<\/p>\n

Pahoehoe lav ak\u0131nt\u0131lar\u0131:<\/strong><\/p>\n

Pahoehoe lav ak\u0131nt\u0131lar\u0131n\u0131n y\u00fczeyi genellikle d\u00fcz ya da hafif k\u0131r\u0131\u015f\u0131k olur.Bu t\u00fcr ak\u0131nt\u0131lar\u0131n koyu k\u0131vam\u0131 de\u011fildir yani ak\u0131\u015fkand\u0131r.Lav so\u011fumaya ba\u015flad\u0131\u011f\u0131nda y\u00fczeyinde d\u00fczg\u00fcn kabuk olu\u015fur.Lav ak\u0131nt\u0131s\u0131n\u0131n i\u00e7 k\u0131sm\u0131 ergimi\u015f durumda kalarak akmay\u0131 s\u00fcrd\u00fcr\u00fcrken so\u011fumakta olan y\u00fczeyde zaman zaman halat benzeri k\u0131vr\u0131mlar olu\u015fturabilir.<\/p>\n

Aa lav ak\u0131nt\u0131lar\u0131:<\/strong><\/p>\n

Aa lav ak\u0131nt\u0131lar\u0131nda p\u00fcr\u00fczl\u00fc ve \u00e7atlakl\u0131 bir y\u00fczeyi vard\u0131r.Bu ak\u0131nt\u0131lar, daha yo\u011fun lavdan olu\u015fur ve pahoehoe lava k\u0131yasla daha yava\u015f akar.Lav akarken ,y\u00fczeyi iri par\u00e7alar bi\u00e7iminde k\u0131r\u0131l\u0131r ve i\u00e7indeki gazlar a\u00e7\u0131\u011fa \u00e7\u0131kar.K\u0131r\u0131lan par\u00e7alar ,s\u0131v\u0131 durumu koruyan lav ak\u0131nt\u0131s\u0131n\u0131n i\u00e7 k\u0131sm\u0131 ile birlikte s\u00fcr\u00fcklenir.<\/p>\n

Bir aa ak\u0131nt\u0131s\u0131s\u0131n kenarlar\u0131 ve \u00f6n\u00fc tank paletlerine benzer bir bi\u00e7imde ilerler: Ak\u0131nt\u0131n\u0131n \u00f6n\u00fcndeki so\u011fumu\u015f par\u00e7alar d\u00f6nerek lav\u0131n alt\u0131na girer, ilerlemekte olan lav bunlar\u0131n \u00fcst\u00fcnden ge\u00e7er.Kat\u0131la\u015fm\u0131\u015f aa lav\u0131n\u0131n y\u00fczeyi p\u00fcr\u00fczl\u00fcd\u00fcr ve yanm\u0131\u015f k\u00f6m\u00fcr y\u0131\u011f\u0131nlar\u0131n\u0131 hat\u0131rlat\u0131r.<\/p>\n

Yurdumuzdaki Yanarda\u011flar<\/strong><\/p>\n

A\u011fr\u0131 Da\u011f\u0131 (5.137 m)
\nUlu Doruk (Re\u015fko Doru\u011fu) Cilo Da\u011flar\u0131 (4.135 m)
\nSuppa Durek , Cilo Da\u011flar\u0131 (4.060 m)
\nS\u00fcphan Da\u011f\u0131 (4.058 m)
\nKa\u00e7kar Da\u011f\u0131 (3.932 m)
\nErciyes Da\u011f\u0131 (3.917 m)
\nKarae\u011fri Sivrisi , Cilo Da\u011flar\u0131 (3.900 m)
\nK\u00fc\u00e7\u00fck A\u011fr\u0131 Da\u011f\u0131 (3.896 m)
\nMaunsell Sivrisi , Cilo Da\u011flar\u0131 (3.850 m)
\nSamdi Da\u011f\u0131 , Sat Da\u011flar\u0131 (3.810 m)
\nMorda\u011f , Hakkari Da\u011flar\u0131 (3.807 m)
\nOrta D\u00fcrek , Cilo Da\u011flar\u0131 (3.770 m)
\nDemirkaz\u0131k Doru\u011fu , Ala da\u011flar (3.756 m)
\nKarak\u00fclah Doruhu , Cilo Da\u011flar\u0131 (3.750 m)
\nKald\u0131 Doru\u011fu , Ala da\u011flar (3.748 m)
\nK\u0131z\u0131lkaya Doru\u011fu , Ala da\u011flar (3.725 m)
\nEmler Doru\u011fu , Ala da\u011flar (3.720 m)
\nVer\u00e7enik Doru\u011fu , Rize Da\u011flar\u0131 (3.711 m)
\nKoca Sarp , Ala da\u011flar (3570 m)
\nBe\u015f Parmak , Ala da\u011flar (3520 m)
\nMedetsiz , Bolkarlar (3514 m)
\nDirek ta\u015f , Ala da\u011flar (3510 m)
\nG\u00fczeller , Ala da\u011flar (3041 m)<\/p>\n<\/div>\n<\/div>\n

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