Turkish Abstract: Turkiye, enlem etkisi nedeniyle, Pleistosen’deki kuvvetli buzullasma alanlarinin uzaginda kalmakla birlikte; guney Anadolu’da Toroslar, ic bolgelerde yuksek volkanik daglar ve Kuzey Anadolu Daglari’nin ozellikle yuksek dogu kesimlerindeki zirveler cevresi dikkat cekici oranda buzullarla kaplanmistir. Belirtilen buzullar, Postglasyal donemdeki iklim kosullarinin etkisiyle eriyerek, buyuk oranda ortadan kalkmistir. Bu alanlarda, ozel kosullarin da etkisiyle korunabilen buzullar ise cogunlukla sirk buzullarina donusmuslerdir. Kuzey Anadolu Daglari, gunumuzde dikkat cekici bir glasyal topografyaya ve onemli sayida guncel buzul varligina sahiptir. Bu daglarin en yuksek iki zirvesine sahip olan Kackar Dagi (3932 m) ve Vercenik Dagi (3709 m) civarinda yer alan buzullasma alanlari cesitli arastirmalara konu olmustur. Bu iki zirve arasinda kalan Tatos (Dilek) Dagi ise nispeten az arastirilan alanlardan biridir. Ancak, 2014 ve 2015 yillarinda gerceklestirilen arazi calismalari ve elde edilen glasyal bulgular, bu alanlarda daha ayrintili gozlem ve arastirmalarin yapilmasi gerektigini ortaya koymaktadir. English Abstract: Due to its latitude, the geographic region of Turkey did not experience episodes of heavy glaciations during the Pleistocene Epoch. Historically though, the mountainous landscapes in Turkey have been covered with a remarkably high rate of glaciers due in most part to the Taurus Mountains in the south, the high volcanic inland mountains, and especially the higher elevations in the eastern region of the North Anatolian Mountains. Because of the climatic conditions of the post-glacial period a majority of these glaciers have largely disappeared. The glaciers which remain are protected by unique climate conditions present in some regions, and for the most part have become circus glaciers. Nowadays, the North Anatolian Mountains are home to a remarkable glacial topography and a significant number of glaciers. Two of the highest peaks in the region are Kackar (3932 m) and Vercenik (3709 m) and the glaciated areas in these mountains have been the focus of multiple investigations. Conversely, Tatos Mountain, which lies between the Kackar and Vercenik peaks, has.