Reworked Middle Pleistocene deposits preserved in the core region of the Fennoscandian Ice Sheet
Quaternary Science Advances, 2020 During successive Pleistocene ice ages, Finnish Lapland lay under the cold-based centre of the Fennoscandian Ice Sheet (FIS). This area largely escaped deep glacial erosion by the fast-flowing wet-based ice streams that developed toward the periphery of ...
Niko Putkinen +5 more
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Coarsely crystalline cryogenic cave carbonate – a new archive to estimate the Last Glacial minimum permafrost depth in Central Europe [PDF]
Climate of the Past, 2012 Cryogenic cave carbonate (CCC) represents a specific type of speleothem whose precipitation is triggered by freezing of mineralized karst water. Coarsely crystalline CCC, which formed during slow freezing of water in cave pools, has been reported from 20
D. Scholz +6 more
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The development of a late Weichselian - early Holocene subaqueous ice-contact fan, Teikangas, SW Finland [PDF]
Bulletin of the Geological Society of Finland, 1996 The depositional environment of the Teikangas formation in southwestern Finland has been studied. The formation is an isolated, ice marginal accumulation of coarse-grained sediments north of the Hämeenkangas ridge, related to the Weichselian ice sheet ...
J.P. Lunkka, P. Alhonen
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Die Umgestaltung des glazigenen Reliefs der norddeutschen Altmoränengebiete am Beispiel des Uelzener Beckens [PDF]
Eiszeitalter und Gegenwart, 1965 The study deals with the influence of the Weichselian periglacial shaping on the modification of older moraine areas; the basin of Uelzen, which is part of the North German lowland, has been taken as an example.
J. Hagedorn
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Radiocarbon dates of mammoth finds in Finland compared with radiocarbon dates of Weichselian and Eemian deposits [PDF]
Bulletin of the Geological Society of Finland, 1979 In Finnish Lapland the Weichselian Peräpohjola Interstadial can be separated from the Eemian Interglacial with the help of the tree pollen composition of organic deposits between tills.
J. Donner, H. Jungner, B. Kurtén
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Till stratigraphy in southern and western Finland [PDF]
Bulletin of the Geological Society of Finland, 1992 This paper gives a review over the recent discoveries and results of Quaternary stratigraphical studies in southern and western Finland. The study of Quaternary stratigraphy has been very active and both Quaternary departments in Universities and ...
K. Nenonen
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Wirkungen des pleistözänen kaltzeitlichen Klimas, insbesondere des Bodenfrostes, in den Sedimenten des östlichen Ostfalen (Eiskeile, Löß-Flugsand, asymmetrische Täler) [PDF]
Eiszeitalter und Gegenwart, 1997 In the second part of the article with the title "Wirkungen des ..." a various documentation of pictures is presented to analyse the ice-wedge casts of the eastern part of Lower Saxony (Ostfalen).
K.-U. Brosche
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Журнал Белорусского государственного университета: География, геология, 2022 Within the bed of the Poozerie (Weichselian) ice sheet, which occupied the northern part of Belarus at the maximum stage and at the beginning of degradation, three concentric thermal zones were identified according to geological and geomorphological ...
Michail E. Komarovskiy +1 more
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Proposing a new conceptual model for the reconstruction of ice dynamics in the SW sector of the Scandinavian Ice Sheet (SIS) based on the reinterpretation of published data and new evidence from optically stimulated luminescence (OSL) dating [PDF]
Eiszeitalter und Gegenwart, 2020 We propose a new concept of the Weichselian ice dynamics in the south-western sector of the Baltic Sea depression. The review of existing geochronological data from Germany, Denmark and southernmost Sweden in combination with new optically stimulated ...
C. Lüthgens, J. Hardt, M. Böse
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Weichselian permafrost depth in the Netherlands: a comprehensive uncertainty and sensitivity analysis [PDF]
The Cryosphere, 2016 The Rupelian clay in the Netherlands is currently the subject of a feasibility study with respect to the storage of radioactive waste in the Netherlands (OPERA-project).
J. Govaerts, K. Beerten, J. ten Veen
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