Çatakkaya Döküntü Örtülü Buzulu (Tatos Dağları)
The eastern part of the North Anatolian Mountains is the place where the Pleistocene glaciations is most effective.In these mountains, which have many summits over 3500 meters, especially the high parts above 2500 meters constitute a significant glacial area. Important peaks of the Eastern Black Sea...
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| Format: | Article |
| Language: | English |
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Ankara University
2019-04-01
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| Series: | Coğrafi Bilimler Dergisi |
| Subjects: | |
| Online Access: | https://dergipark.org.tr/tr/pub/aucbd/issue/44165/536616 |
| _version_ | 1827989917386407936 |
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| author | Gürcan Gürgen |
| author_facet | Gürcan Gürgen |
| author_sort | Gürcan Gürgen |
| collection | DOAJ |
| description | The eastern part of the North Anatolian Mountains is the place where the Pleistocene glaciations is most effective.In these mountains, which have many summits over 3500 meters, especially the high parts above 2500 meters constitute a significant glacial area. Important peaks of the Eastern Black Sea Mountains; Glaciers and glacier shapes on the northern slopes of Kaçkar, Verçenik, Tatos (Dilek), Göller(Hunut) and Bulut-Altiparmak have been subject to various investigations because of these features. In the Eastern Black Sea Mountains, there are also some glacial traces, glacial shapes, and even current cirque glaciers in the southern-facing parts of these summits. The southern part of the Tatos Mountains, which forms one of the highest peaks of the Eastern Black Sea Mountains, is also where glaciation is effective.The glacier valleys reflecting the traces of the Pleistocene glaciations, the various glacial shapes and glacier lakes together with the northward-facing Çatakkaya debris covered glacier, covered entirely with a rubble, detected at the steep slope of a glacial cirque is a significant finding that reveals the impact and significance of glaciation in this area. |
| first_indexed | 2024-04-10T00:27:50Z |
| format | Article |
| id | doaj.art-8683eb9eb8224b708203a8420ad3a395 |
| institution | Directory Open Access Journal |
| issn | 1303-5851 1308-9765 |
| language | English |
| last_indexed | 2024-04-10T00:27:50Z |
| publishDate | 2019-04-01 |
| publisher | Ankara University |
| record_format | Article |
| series | Coğrafi Bilimler Dergisi |
| spelling | doaj.art-8683eb9eb8224b708203a8420ad3a3952023-03-15T07:07:20ZengAnkara UniversityCoğrafi Bilimler Dergisi1303-58511308-97652019-04-0117121723610.33688/aucbd.536616Çatakkaya Döküntü Örtülü Buzulu (Tatos Dağları)Gürcan Gürgen0https://orcid.org/0000-0003-0224-1644Ankara Üniversitesi, Eğitim Bilimleri Fakültesi, İlköğretim BölümüThe eastern part of the North Anatolian Mountains is the place where the Pleistocene glaciations is most effective.In these mountains, which have many summits over 3500 meters, especially the high parts above 2500 meters constitute a significant glacial area. Important peaks of the Eastern Black Sea Mountains; Glaciers and glacier shapes on the northern slopes of Kaçkar, Verçenik, Tatos (Dilek), Göller(Hunut) and Bulut-Altiparmak have been subject to various investigations because of these features. In the Eastern Black Sea Mountains, there are also some glacial traces, glacial shapes, and even current cirque glaciers in the southern-facing parts of these summits. The southern part of the Tatos Mountains, which forms one of the highest peaks of the Eastern Black Sea Mountains, is also where glaciation is effective.The glacier valleys reflecting the traces of the Pleistocene glaciations, the various glacial shapes and glacier lakes together with the northward-facing Çatakkaya debris covered glacier, covered entirely with a rubble, detected at the steep slope of a glacial cirque is a significant finding that reveals the impact and significance of glaciation in this area.https://dergipark.org.tr/tr/pub/aucbd/issue/44165/536616glacial morphologyglaciationsdebris-covered glacierstatos mountains-turkey |
| spellingShingle | Gürcan Gürgen Çatakkaya Döküntü Örtülü Buzulu (Tatos Dağları) Coğrafi Bilimler Dergisi glacial morphology glaciations debris-covered glaciers tatos mountains-turkey |
| title | Çatakkaya Döküntü Örtülü Buzulu (Tatos Dağları) |
| title_full | Çatakkaya Döküntü Örtülü Buzulu (Tatos Dağları) |
| title_fullStr | Çatakkaya Döküntü Örtülü Buzulu (Tatos Dağları) |
| title_full_unstemmed | Çatakkaya Döküntü Örtülü Buzulu (Tatos Dağları) |
| title_short | Çatakkaya Döküntü Örtülü Buzulu (Tatos Dağları) |
| title_sort | catakkaya dokuntu ortulu buzulu tatos daglari |
| topic | glacial morphology glaciations debris-covered glaciers tatos mountains-turkey |
| url | https://dergipark.org.tr/tr/pub/aucbd/issue/44165/536616 |
| work_keys_str_mv | AT gurcangurgen catakkayadokuntuortulubuzulutatosdagları |