A rare piedmont glaciation in the Mediterranean: insights from cosmogenic 36Cl dating of Davraz hummocky moraine field (SW Türkiye)

dc.contributor.author Altınay, Onur
dc.contributor.author Sarıkaya, Mehmet Akif
dc.contributor.author Wilcken, Klaus M.
dc.contributor.authorID orcid.org/0000-0003-1821-6814
dc.contributor.department Katı Yer Bilimleri
dc.date.accessioned 2025-01-02T12:23:10Z
dc.date.available 2025-01-02T12:23:10Z
dc.date.issued 2024
dc.description.abstract Piedmont glaciers (lobes), typically found in high latitudes and large mountainous regions, extend from ice sheets and ice caps to lower altitudes. However, they can also occur, although less commonly, on mid-latitude mountains. When these fan-like glaciers retreat, they leave behind hummocky moraines scattered in a chaotic pattern. In this study, we have mapped one of these mid-latitude sites and established a Terrestrial cosmogenic nuclide (TCN) glacial chronology on Mount Davraz, namely Davraz hummocky moraine field (37°46′00″N, 30°43′15″E). Our findings indicate that the glaciers in this area started receding from the early local Last Glacial Maximum (LGM) period (21.8 ± 2.4 ka) to the early Late-glacial period (17.7 ± 2.2 ka), and eventually disappearing. The deglaciation of the Mt. Davraz palaeoglacier matches nearby mountains, supported by southerly winds as significant for regional glaciation. Our discoveries reveal a robust connection between southerly winds and nearby glaciation, contributing to our understanding of how climate influences glaciers. Likewise, the glacial timelines of the neighbouring mountains align with the glacial history of Mt. Davraz.
dc.description.sponsorship This work was supported by Istanbul Technical University, Türkiye, BAP Project [grant number MDK–2022–43674] and Türkiye Bilimsel ve Teknolojik Araştırma Kurumu [grant number 118Y052]. Financial support from the Australian Nuclear Science and Technology Organisation (#AP11366) through the National Collaborative Research Infrastructure Strategy (NCRIS).
dc.identifier.citation Altınay, O., Sarıkaya, M.A. & Wilcken, K.M. (2024). "A rare piedmont glaciation in the Mediterranean: Insights from cosmogenic 36Cl dating of Davraz hummocky moraine field (SW Türkiye)", Earth Surface Processes and Landforms, 49 (7): 2047–2066. https://doi.org/10.1002/esp.5815
dc.identifier.endpage 2066
dc.identifier.issue 7
dc.identifier.startpage 2047
dc.identifier.uri https://doi.org/10.1002/esp.5815
dc.identifier.uri http://hdl.handle.net/11527/26077
dc.identifier.volume 49
dc.language.iso en_US
dc.publisher Wiley
dc.relation.ispartof Earth Surface Processes and Landforms
dc.rights.license CC BY 4.0
dc.sdg.type none
dc.subject cosmogenic dating
dc.subject hummocky moraines
dc.subject Piedmont glaciers
dc.subject glaciers
dc.subject Mediterranean glaciations
dc.subject Davraz Dağı
dc.subject Mount Davraz
dc.title A rare piedmont glaciation in the Mediterranean: insights from cosmogenic 36Cl dating of Davraz hummocky moraine field (SW Türkiye)
dc.type Article
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