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