TRACES OF GLACIAL ON MESCIT MOUNTAINS (NE TURKEY)

Mescit Mountains reveal traces of Pleistocene glaciation. The presence of glacier erosion formations in the form of the cirque at the crest of such mountainous mass were determined during the explorations performed previously. During the observation we conducted in the region, the moraine deposits w...

Descripción completa

Guardado en:

Detalles Bibliográficos
Autor principal:	Nurfeddin KAHRAMAN
Formato:	article
Lenguaje:	DE EN FR TR
Publicado:	Fırat University 2019
Materias:	mescit mountains eskiköy last glacial maximum pleistocene glaciation petekli village Social Sciences H Social sciences (General) H1-99
Acceso en línea:	https://doaj.org/article/17f9b5052bc441d4b6c68c547b920f1b
Etiquetas:	Agregar Etiqueta Sin Etiquetas, Sea el primero en etiquetar este registro!

id	oai:doaj.org-article:17f9b5052bc441d4b6c68c547b920f1b
record_format	dspace
spelling	oai:doaj.org-article:17f9b5052bc441d4b6c68c547b920f1b2021-11-24T09:20:55ZTRACES OF GLACIAL ON MESCIT MOUNTAINS (NE TURKEY)2148-416310.9761/JASSS2829https://doaj.org/article/17f9b5052bc441d4b6c68c547b920f1b2019-08-01T00:00:00Zhttps://jasstudies.com/index.jsp?mod=tammetin&makaleadi=204124881_3-Do%C3%A7.%20Dr.%20Nurfeddin%20KAHRAMAN.pdf&key=27412https://doaj.org/toc/2148-4163Mescit Mountains reveal traces of Pleistocene glaciation. The presence of glacier erosion formations in the form of the cirque at the crest of such mountainous mass were determined during the explorations performed previously. During the observation we conducted in the region, the moraine deposits were determined, which were consisted of till sedimentations in Eskiköy, located at the upper course of Petekli Brook located close to southwest of the crest section. Located at heights of 1,800 to 1,880 m., Eskiköy features formation of the mixtures of the glacier and stream, with a wavy appearance due to the moraine accumulations on the surface. The moraine sets are located under the slopes of mountain range facing to the south, which surrounds that plane from the south and south-east and east sections of it, at heights of about 1,830 m to 1,870 m. At sections below specified mountain, these sets haven’t deteriorated under natural or human factors. It had named as Büyük and Küçük Henegen, the moraine sets located at these sections imply that they are recently formed, considering that they preserve their initial formations. Mescit Mountains is located in south of the Eastern Black Sea Mountains. Mentioned mountain ranges is located in close to each other and these raises exceeds 3,000 meters. In this regard, the Pleistocene glaciation process showed similarities on these mountains. Moraine sets in Eskiköy was considerably to fall into ruin by natural and human reasons. This fall into ruin is further in the former glacier sets. The traces of accumulation of Pleistocene glaciations observed at the regions near to the summit of Mescit Mountains is depicted with this work for the first time.Nurfeddin KAHRAMANFırat Universityarticlemescit mountainseskiköylast glacial maximumpleistocene glaciationpetekli villageSocial SciencesHSocial sciences (General)H1-99DEENFRTRJournal of Academic Social Science Studies , Vol 8, Iss 34, Pp 41-51 (2019)
institution	DOAJ
collection	DOAJ
language	DE EN FR TR
topic	mescit mountains eskiköy last glacial maximum pleistocene glaciation petekli village Social Sciences H Social sciences (General) H1-99
spellingShingle	mescit mountains eskiköy last glacial maximum pleistocene glaciation petekli village Social Sciences H Social sciences (General) H1-99 Nurfeddin KAHRAMAN TRACES OF GLACIAL ON MESCIT MOUNTAINS (NE TURKEY)
description	Mescit Mountains reveal traces of Pleistocene glaciation. The presence of glacier erosion formations in the form of the cirque at the crest of such mountainous mass were determined during the explorations performed previously. During the observation we conducted in the region, the moraine deposits were determined, which were consisted of till sedimentations in Eskiköy, located at the upper course of Petekli Brook located close to southwest of the crest section. Located at heights of 1,800 to 1,880 m., Eskiköy features formation of the mixtures of the glacier and stream, with a wavy appearance due to the moraine accumulations on the surface. The moraine sets are located under the slopes of mountain range facing to the south, which surrounds that plane from the south and south-east and east sections of it, at heights of about 1,830 m to 1,870 m. At sections below specified mountain, these sets haven’t deteriorated under natural or human factors. It had named as Büyük and Küçük Henegen, the moraine sets located at these sections imply that they are recently formed, considering that they preserve their initial formations. Mescit Mountains is located in south of the Eastern Black Sea Mountains. Mentioned mountain ranges is located in close to each other and these raises exceeds 3,000 meters. In this regard, the Pleistocene glaciation process showed similarities on these mountains. Moraine sets in Eskiköy was considerably to fall into ruin by natural and human reasons. This fall into ruin is further in the former glacier sets. The traces of accumulation of Pleistocene glaciations observed at the regions near to the summit of Mescit Mountains is depicted with this work for the first time.
format	article
author	Nurfeddin KAHRAMAN
author_facet	Nurfeddin KAHRAMAN
author_sort	Nurfeddin KAHRAMAN
title	TRACES OF GLACIAL ON MESCIT MOUNTAINS (NE TURKEY)
title_short	TRACES OF GLACIAL ON MESCIT MOUNTAINS (NE TURKEY)
title_full	TRACES OF GLACIAL ON MESCIT MOUNTAINS (NE TURKEY)
title_fullStr	TRACES OF GLACIAL ON MESCIT MOUNTAINS (NE TURKEY)
title_full_unstemmed	TRACES OF GLACIAL ON MESCIT MOUNTAINS (NE TURKEY)
title_sort	traces of glacial on mescit mountains (ne turkey)
publisher	Fırat University
publishDate	2019
url	https://doaj.org/article/17f9b5052bc441d4b6c68c547b920f1b
work_keys_str_mv	AT nurfeddinkahraman tracesofglacialonmescitmountainsneturkey
_version_	1718415402659217408

TRACES OF GLACIAL ON MESCIT MOUNTAINS (NE TURKEY)

Ejemplares similares