Results 11 to 20 of about 465 (165)

Chronological and sedimentological investigations of the Late Pleistocene succession in Osterbylund (Schleswig-Holstein, Germany) [PDF]

open access: yesEiszeitalter und Gegenwart, 2023
The age of the push moraine complex Wallsbüll-Böxlund, Schleswig-Holstein, is unclear despite investigations in this area for decades. To address the timing of formation of both the push moraine complex and the peat and soils found in its depressions, an
C. Thiel   +5 more
doaj   +1 more source

Weichselian glaciation southeast of the Baltic Sea [PDF]

open access: yesEstonian Journal of Earth Sciences, 2010
Volli Kalm
doaj   +2 more sources

Chronology of Late Saalian and Middle Weichselian episodes of ice-free lacustrine sedimentation recorded in the Arumetsa section, southwestern Estonia [PDF]

open access: yesEstonian Journal of Earth Sciences, 2010
The information obtained from a 21 m thick open-pit section of silty-clayey sediments in the Arumetsa bedrock valley, southwestern Estonia, revealed that lacustrine to glaciolacustrine sedimentation at the site started prior to 151 ka ago and lasted to ...
Maris Rattas   +6 more
doaj   +1 more source

Patterns of Late Glacial vegetation in The Netherlands [PDF]

open access: yesEiszeitalter und Gegenwart, 1997
The Weichselian Late Glacial (ca. 13,000 - 10,000 years BP) marks the transition from the cold Weichsel Late Pleniglacial to the warmer Holocene. During this period the climate rapidly changed as did the vegetation and the abiotic landscape.
W. Z. Hoek
doaj   +1 more source

Weichselian Glaciation of the Faroe Islands

open access: yesBulletin of the Geological Society of Denmark, 2023
This paper presents a new complete field mapping of glacial landscapes, landforms and sediments in the Faroe Islands, supplemented by observations from bathymetric maps of the Faroe Shelf. In addition, previous investigations of Quaternary and espe-cially the Weichselian glaciation of the archipelago are reviewed.
Ole Humlum   +4 more
openaire   +1 more source

Marjamurto, an interstadial site in a till covered esker area of central Ostrobothnia, western Finland [PDF]

open access: yesBulletin of the Geological Society of Finland, 1989
Till-covered glaciofluvial deposits, presumably eskers, are common in Central Ostrobothnia (Pohjanmaa) within a zone more than 50 km broad, in which no exposed eskers are present.
H. Peltoniemi   +3 more
doaj   +1 more source

Eemian to Early Weichselian organic deposits in the watershed kettle-hole basins in central Poland [PDF]

open access: yesBulletin of the Geological Society of Finland, 2018
In the examined part of central Poland, there are numerous kettle-hole basins filled with mineral and biogenic sediments of the Eemian Interglacial and Early Weichselian.
J. Forysiak   +3 more
doaj   +1 more source

Geologic position of the Younger Dryas subfossil forest in the Warta River valley, central Poland [PDF]

open access: yesBulletin of the Geological Society of Finland, 2012
Numerous tree trunks are present in the Late Weichselian deposits on the low terrace of the Warta river valley, in central Poland. This study concerns the well preserved tree remnants as well as accompanying depositional series and their sedimentary ...
D. Dzieduszynska, J. Petera-Zganiacz
doaj   +1 more source

Glaciotectonic deformation of till-covered glaciofluvial deposits in Oulu region, Finland [PDF]

open access: yesBulletin of the Geological Society of Finland, 2008
Sedimentary sequences in Isoniemi and Hangaskangas in the Oulu area of Finland have been studied using conventional sedimentological techniques including structural and clast-fabric measurements on fold and fault structures and till units. Four different
A. Pasanen, J.P. Lunkka
doaj   +1 more source

Reworked Middle Pleistocene deposits preserved in the core region of the Fennoscandian Ice Sheet

open access: yesQuaternary 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
doaj   +1 more source

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