Turkish Abstract: Anadolu’da Pleistosen buzullasmasinin en etkili oldugu yerlerden biri, Kuzey Anadolu Daglari’nin dogu kesimini olusturan Dogu Karadeniz Daglari’dir. En yuksek zirveyi olusturan Kackar (3932 m) ile birlikte, yukseltisi 3500 m’nin uzerine cikan cok sayida zirveye sahip olan bu daglarin, kuzeye bakan yamaclari basta olmak uzere, 2500 m’nin uzerindeki kisimlarda onemli bir buzullasma meydana gelmistir. Dogu Karadeniz dag siralarinin onemli doruklari; Kackar, Ucdoruk, Dilek, Goller ve Bulut-Altiparmak daglarinin, genellikle kuzeye bakan yamaclari buzullasma etkisinin en iyi gozlendigi alanlardir. Dogu Karadeniz Daglari’nin, bu yuksek zirveleri disindabolgede, yukseltileri daha az olan ve buzullasma sureclerinden goreceli olarak daha az etkilendigi dusunulen bazi alanlarda, yerel kosullardaki farkliliklara da bagli olarak onemli bir buzullasma meydana gelmistir. Dogu Karadeniz Daglari’nin kuzeydogusunda ve Coruh Vadisi’nin dogusunda yuksek bir kutle olusturan Karcal Daglari (3431 m),Pleistosen buzullasmasinin izlerini yansitanbuzul vadileri, cesitli glasyal sekiller ve buzul golleri yaninda kismen ortulu olarak gunumuze kadar ulasan buzullari barindirmaktadir. English Abstract: Eastern Black Sea Mountains which are eastern part of North Anatolian Mountains are one of the places where the Pleistocene glaciations took place heavily. There are major glaciations on the northern hillside and on the places with the height of over 2500 m of these mountains that has many peaks that are higher than 3500m and besides the highest peak Kackar (3932m). The northern hillside of the major peaks called Kackar, Ucdoruk, Dilek, Goller and Bulut-Altiparmak of North Anatolian Mountains are major places where the impact of glaciations could be recognized. Unlike these peaks of North Anatolian Mountains, there took place major glaciations on the places which, has lower heights than 2500 and is considered less impacted relatively by glaciations, based on the differences of local conditions. Karcal Mountains (3431m) with the Pleistocene glacial valleys that prove the glaciations and various glacial shapes and glacial lakes have partly debris covered glaciations which are still recognizable.