Results 131 to 140 of about 491 (184)

Multiproxy climate reconstructions for the Eemian and Early Weichselian

Journal of Quaternary Science, 1998
Palaeobotanical, coleopteran and periglacial data from 106 sites across northwestern Europe have been analysed in order to reconstruct palaeoclimatic conditions during the Eemian and Early Weichselian. Three time slices in the Eemian and four in the Early Weichselian have been considered.
Aalbersberg, G., Litt, T.
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THE LATE WEICHSELIAN SEQUENCE IN THE VALE OF YORK

Proceedings of the Yorkshire Geological Society, 1970
Summary Three recent radiocarbon dates can be used to provide an outline chronology and correlation for a sequence of late Weichselian and early Flandrian environments in the Vale of York.
G. D. Gaunt, R. A. Jarvis, B. Matthews
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Sedimentary features of a Weichselian glaciolacustrine delta

Boreas, 1981
Inclined beds of sand, granules, pebbles and cobbles resembling a glacio‐tectonically tilted sequence were shown by sedimentological studies to constitute the 10–12 m thick foreset beds of a glaciolacustrine Gilbert‐type delta in Kyndby, North Sjælland, Denmark.
Clemmensen, Lars B, Houmark-Nielsen, Michael   +1 more
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Weichselian chronostratigraphy and correlations

Boreas, 1981
The glacial history of the Fennoscandian ice cap beyond some 20,000 years B.P. is fairly poorly known because of the absence of a reliable dating control. The Eemian Interglacial of Europe is not dated at all. The Weichselian Glaciation seems to be characterized by three main glaciation maxima separated by two main interstadial periods (of quite ...
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Weichselian palaeoenvironments at Kobbelgård, Møn, Denmark

Boreas, 1991
Lithostratigraphical and palynological investigations of a coastal cliff section at Kobbelgård, Møn (Denmark) reveal a sedimentary sequence of Weichselian age. Bedded clayey sediments are overlain by stratified silt, sand and occasional beds of clay and gravel.
Kolstrup, E., Houmark-Nielsen, M.
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Eemian and Weichselian stratigraphy in South Sweden

Boreas, 1981
The stratigraphy of Pleistocene sequences within three main areas of the province of Skane, South Sweden, is discussed. The traditional stratigraphy is revised. New lithostratigraphic units are deficned and named according to international stratigraphic terminology.
BJÖRN E. BERGLUND, ERIK LAGERLUND
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A Middle Weichselian deposit at Halling, Kent

Proceedings of the Geologists' Association, 1971
Abstract A periglacial deposit of loessic character at Halling, Kent, is described, and an analysis made of its molluscan fauna. The deposit is stratigraphically earlier than zone I of the Late Weichselian. The fauna suggests that an interstadial of the Middle Weichselian may be represented.
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Eemian and Weichselian correlation problems in Finland

Boreas, 1984
The Quaternary stratigraphy in Finland is discussed on the basis of an example from the Oulainen area of Ostrobothnia. Organogenic deposits found beneath till at this site are correlated with the Eemian Interglacial on biostratigraphical evidence. This is confirmed by TL dates of 97,000 ± 18,000 B.P.
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Weichselian in Sweden before 15,000 B.P.

Boreas, 1981
A brief summary is given of the present state of knowledge about the Weichselian glaciations and interstadials in sweden. The following stages are discussed: (1) The first Weichselian glaciation (W1). This glaciation has not been identified. Probably only northern Sweden was ice‐covered. (2) The Jämtland Interstadial, dated at > 50,000 B.P.
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Periglacial microjointing and faulting in Weichselian fluvio‐aeolian deposits

Journal of Quaternary Science, 1993
AbstractA Weichselian Late Pleniglacial fluvio‐aeolian deposit has been investigated in the southern Netherlands. Three main structural lineaments have been distinguished: (1) very small, vertical platy structures (microjoints), in a parallel and a columnar configuration; (2) large joints and normal faults with minor displacement (‘Grubbenvorst type’),
Mol, J., Vandenberghe, Jef, Kasse, C., Stel, H.   +3 more
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