Quaternary glaciations of Turkey

Mehmet Akif Sarikaya; Attila Çiner; Marek Zreda

doi:10.1016/B978-0-444-53447-7.00030-1

Quaternary glaciations of Turkey

Mehmet Akif Sarikaya^*, Attila Çiner, Marek Zreda

^*Corresponding author for this work

Research output: Contribution to journal › Article › peer-review

78 Citations (Scopus)

Abstract

The cosmogenic exposure ages obtained from glacial landforms in several Turkish mountains provided a basis to reconstruct glacio-chronology and paleoclimate of Turkey. Glacier-related landforms occur in three major regions of Turkey; (1) the Taurus Mountains, along the Mediterranean coast and southeast Turkey, (2) mountain ranges along the Eastern Black Sea Region, and (3) volcanoes and independent mountain chains scattered across the Anatolian Plateau. ¹⁰Be ²⁶Al and ³⁶Cl ages show that the oldest and most extensive mountain glaciers were developed during the Last Glacial Maximum. Unusual Early Holocene glaciations, dated to 9 ka-10 ka, were also reported from Mount Erciyes and Aladaĝlar.

Original language	English
Pages (from-to)	393-403
Number of pages	11
Journal	Developments in Quaternary Science
Volume	15
DOIs	https://doi.org/10.1016/B978-0-444-53447-7.00030-1
Publication status	Published - 2011
Externally published	Yes

Keywords

Cosmogenic surface dating
Early Holocene
Glacier
Last Glacial Maximum
Turkey

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10.1016/B978-0-444-53447-7.00030-1

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title = "Quaternary glaciations of Turkey",

abstract = "The cosmogenic exposure ages obtained from glacial landforms in several Turkish mountains provided a basis to reconstruct glacio-chronology and paleoclimate of Turkey. Glacier-related landforms occur in three major regions of Turkey; (1) the Taurus Mountains, along the Mediterranean coast and southeast Turkey, (2) mountain ranges along the Eastern Black Sea Region, and (3) volcanoes and independent mountain chains scattered across the Anatolian Plateau. 10Be 26Al and 36Cl ages show that the oldest and most extensive mountain glaciers were developed during the Last Glacial Maximum. Unusual Early Holocene glaciations, dated to 9 ka-10 ka, were also reported from Mount Erciyes and Aladaĝlar.",

keywords = "Cosmogenic surface dating, Early Holocene, Glacier, Last Glacial Maximum, Turkey",

author = "Sarikaya, {Mehmet Akif} and Attila {\c C}iner and Marek Zreda",

year = "2011",

doi = "10.1016/B978-0-444-53447-7.00030-1",

language = "English",

volume = "15",

pages = "393--403",

journal = "Developments in Quaternary Science",

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TY - JOUR

T1 - Quaternary glaciations of Turkey

AU - Sarikaya, Mehmet Akif

AU - Çiner, Attila

AU - Zreda, Marek

PY - 2011

Y1 - 2011

N2 - The cosmogenic exposure ages obtained from glacial landforms in several Turkish mountains provided a basis to reconstruct glacio-chronology and paleoclimate of Turkey. Glacier-related landforms occur in three major regions of Turkey; (1) the Taurus Mountains, along the Mediterranean coast and southeast Turkey, (2) mountain ranges along the Eastern Black Sea Region, and (3) volcanoes and independent mountain chains scattered across the Anatolian Plateau. 10Be 26Al and 36Cl ages show that the oldest and most extensive mountain glaciers were developed during the Last Glacial Maximum. Unusual Early Holocene glaciations, dated to 9 ka-10 ka, were also reported from Mount Erciyes and Aladaĝlar.

AB - The cosmogenic exposure ages obtained from glacial landforms in several Turkish mountains provided a basis to reconstruct glacio-chronology and paleoclimate of Turkey. Glacier-related landforms occur in three major regions of Turkey; (1) the Taurus Mountains, along the Mediterranean coast and southeast Turkey, (2) mountain ranges along the Eastern Black Sea Region, and (3) volcanoes and independent mountain chains scattered across the Anatolian Plateau. 10Be 26Al and 36Cl ages show that the oldest and most extensive mountain glaciers were developed during the Last Glacial Maximum. Unusual Early Holocene glaciations, dated to 9 ka-10 ka, were also reported from Mount Erciyes and Aladaĝlar.

KW - Cosmogenic surface dating

KW - Early Holocene

KW - Glacier

KW - Last Glacial Maximum

KW - Turkey

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U2 - 10.1016/B978-0-444-53447-7.00030-1

DO - 10.1016/B978-0-444-53447-7.00030-1

M3 - Article

AN - SCOPUS:79959827273

SN - 1571-0866

VL - 15

SP - 393

EP - 403

JO - Developments in Quaternary Science

JF - Developments in Quaternary Science

ER -

Quaternary glaciations of Turkey

Abstract

Keywords

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