The Bergen inlet, transgressive and regressive Holocene shoreline deposits in the Northwestern Netherlands in Special issue in the honour of J. D. De Jong.
Géographie de l'Europe ; Holocène ; Ligne de rivage ; Niveau marin ; Noord-Holland ; Palynologie ; Pays-Bas ; Quaternaire marin ; Stratigraphie ; Transgression marine
La comparaison des altitudes absolues des paléoniveaux des transgressions dans la basse vallée de la Pecora et des variations du niveau des océans sur l'échelle chronologique absolue permet de faire les conclusions suivantes: les transgressions
-Weichselian shore-level changes from one region to another. The highest marine levels recorded drop from 220 m in the Oslo area, in early Preboreal time, and from less than 10 m in Lista, during the post-Weichselian Tapes transgression maximum. Information
This book is not only an overview of the authors'major contribution to the subject, but also a sound documentary review of the work carried out during the last decades on sea-level changes in Tunisia. Five marine transgressions are recognized since
the Tyrrhenian: three of them (the Douiza, Rejiche and Chebba Formations) left clearly emerged marine deposits| Two further intra-würm transgressions have been inferred from eolian deposits. Indeed, neotectonics are significant and still active along the Tunisian
The Holocene transgression on the Arctic flank of Beringia: Chukchi Valley to Chukchi Estuary to Chukchi Sea in Quaternary coastlines and marine archaeology: Towards the prehistory of land bridges and continental shelves.
The history of the Holocene transgression is reconstructed in the area of the present straits between Siberia and Alaska using modern assemblages of benthonic foraminifera from 26 cores. The relative sequence of events progresses from a wind swept
invites joint consideration is the nature and scale of changes that will occur, both in coastline retreat and sea-level rise, if the modern global warming continues to such an extent that a major marine transgression occurs.
This paper reviews glacio-isostatic movements in Finland, using the shorelines left by the Baltic Ice Lake (10500-10200 B.P.), the brackish Yoldia stage (10000 B.P.), the Ancylus Lake (9000 B.P.), the transgressive brackish Littorina Sea (7500-7000
General characteristics of the coast. Regional descriptions. Coastal problems: Neotectonics along the coasts| submarine topography and Holocene transgression| late Holocene sea level fluctuations| pumice pebbles in the late Holocene beaches| coastal
Up till now it was thought that the alternation of clastic sediments and peat in the so-called perimarine area of the Netherlands was caused by an alternation of transgressions and regressions. Recently it was shown, however, that the alternation