TY  - JOUR
TT  - Tatos Pathway glacier (Rize Turkey)
AU  - Gürgen, Gürcan
PY  - 2015
DA  - August
DO  - 10.1501/Cogbil_0000000169
JF  - Coğrafi Bilimler Dergisi
JO  - CBD
PB  - Ankara Üniversitesi
WT  - DergiPark
SN  - 1303-5851
SP  - 161
EP  - 172
VL  - 13
IS  - 2
KW  - Tatos Dağları
KW  - Tatos Gediği
KW  - buzul
KW  - döküntü örtülü buzul
KW  - Rize
N2  - 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 Kaçkar (3932 m) and Verçenik (3709 m) and the glaciated areas in these mountains have been the focus of multiple investigations. Conversely, Tatos Mountain, which lies between the Kaçkar and Verçenik peaks, has
CR  - Çiner, A. (2003) “Türkiye’nin güncel buzulları ve Geç Kuvaterner buzul çökelleri”, Türk. Jeo. Bül.Cilt:46, Sayı: 1.
CR  - Doğu, A.F.; Somuncu, M.; Çiçek, İ.; Tunçel, H.; Gürgen, G. (1993), ”Kaçkar Dağında buzul şekilleri, yaylalar ve turizm”
CR  - A.Ü. Türkiye Coğrafyası Araştırma ve Uygulama Merkezi Dergisi Sayı:2, s.157–184. Doğu, A. F.; Çiçek, İ.; Gürgen, G. ve Tunçel, H. (1996) “Üçdoruk (Verçenik) dağında buzul şekilleri, yaylalar ve turizm”,
CR  - A.Ü, Türkiye Coğ. Araşt. ve Uyg. Merk. Derg. No:5. Erinç, S. (1945) Doğu Karadeniz Dağlarında Glasyalmorfoloji Araştırmaları, İst. Üniv.Ed. Fak. Yay. Coğ. Ens. Dok. Tez. Ser. No: 1, İstanbul.
CR  - Erinç S. (1949) “Kaçkardağı Grubunda Diluviyal ve Bu günkü Glasyasyon (Eiszeitliche und gegenwartige Vergletsche-rung in der Kaçkardag-Gruppe)”, İst. Üniv. Fen Fak. Mec. Seri. B.C. XIV. S.3, s.243-245.
CR  - Erinç, S. (1952) “The present glaciation in Turkey”, General Assembly and 17th International Congress of the International
CR  - Geographical Union, 8th Proceedings, Washington. Gall, H. (1966) Gletscherkundliche Beobachtungen im Hochgebirge von Lasistan (Nordostanatolisches Randgebirge).
CR  - Mitteilungen der Osterreichischen Geographischen Gesellschaft, 108, Heft II/III. Gürgen, G. ve Yeşilyurt, S., (2012) “Karçal Dağı Buzulları (Artvin)”, Coğrafi Bilimler Dergisi, 10, 1, 91-104.
CR  - Gürgen, G. (2015) “Verçenik Dağı Buzulları (Rize)” TÜCAUM VIII. Coğrafya Sempozyumu Bildiriler Kitabı, s.73-86.
CR  - Krenek, L. (1932) “Gletscher im Pontischen Gebirge. (Lasistan)”, Zeitschrift f. Gletscherkunde. Bd. 20, S. 129-131, Bildtafel XV u. XVI.
CR  - Kurter, A. (1991) Glaciers of the Middle East and Africa-glaciers of Turkey. (Richard,S.; Williams, R. S.; and Ferrigno, J. G. editors), Satellite image atlas of glaciers of the world. United States Geological Survey Professional Paper G-1,1-30.
CR  - Koch, K.H.E. (1846) Reise im Pontischen Gebirge.Weimar.
CR  - Sstebnitski, J. (1882) Das Pontische Gebirge, Pett. Mitt.
CR  - Leutelt, R. (1934) “Im Hochgebirge von Lasistan”, Osterr Alpenzeitung Wien, Falge 1145, S. 127 - 140.
CR  - Leutelt, R. (1935) “Glazialgeologische Beobachtungen im Lasistanischen”, Hochgebirge. z. f, Gletscherkde. 23, S. 67 - 80.
CR  - Loffler, E. (1970) Untersuchungen zum eiszeitlichen und rezenten klimagenetischen Formenschatz in den Gebirgen
Nordostanatoliens: Heidelberg Geographische Arbeiten Heft: 27, Heidelberg.
UR  - https://doi.org/10.1501/Cogbil_0000000169
L1  - https://dergipark.org.tr/tr/download/article-file/690716
ER  -