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Late Glacial to Holocene dune development at southern Krakower See

  • The site at the southern shore of Krakower See shows the Quaternary geology of the surrounding area. The local Quaternary sequence comprises a thickness of 50–100m of Quaternary deposits while the surface morphology is dominated by the ice marginal position of the Pomeranian moraine, which passes through the area. The bathymetry of the lake basin of Krakower See indicates a predominant genesis by glaciofluvial erosion in combination with glacial exaration. Past research in this area has focussed on the reconstruction of Pleniglacial to Holocene environmental changes, including lake-level fluctuations, aeolian dynamics, and pedological processes and their modification by anthropogenic land use.

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Metadaten
Author: Sebastian LorenzORCiD, Henrik Rother, Michael Kenzler, Sara Kaphengst
URN:urn:nbn:de:gbv:9-opus-37084
DOI:https://doi.org/https://doi.org/10.5194/deuquasp-2-83-2019
ISSN:2625-8137
Parent Title (English):DEUQUA special publications
Publisher:Copernicus
Place of publication:Göttingen
Document Type:Article
Language:English
Date of first Publication:2019/08/14
Release Date:2020/05/06
First Page:83
Last Page:88
Faculties:Mathematisch-Naturwissenschaftliche Fakultät / Institut für Geographie und Geologie
Licence (German):License LogoCreative Commons - Namensnennung